chains passing over a rod fitted with a lever for ``letting
go.'' The cat davit is hinged at its base, and can be laid flat
on the deck for right ahead fire or when at sea. Ground and
catting chains have been superseded in some ships by a wire
pendant and cat hook; the anchor is then hove close up to the
hawse-pipe. To avoid cutting away a portion of the forecastle,
in the ``Cressy,'' ``Terrible'' and ``Diadem'' classes of
the British navy, the anchors, secured by chains, are stowed
a-cock-bill, outside the ship, with their crowns resting on
iron shoes secured to the ship's side and the flukes fore and
aft. A difficulty is experienced in stowing the anchors when
the ship is pitching or rolling heavily. Fig. 4 illustrates
an anchor with cat davit or anchor crane used in the P.
and O. Company's steamers (``India'' class, 8000 tons);
for sea the anchor is stowed on board by the anchor crane.
Stockless anchors have been extensively used in the British
mercantile marine and in some foreign navies. In 1903 they
FIG. 5.--Hall's Improved FIG. 6.--W. L.
Byer's Stockless Anchor. Stockless Anchor.
were adopted generally for the British navy, after extensive
anchor trials, begun in 1885. Their advantages are:--handiness
combined with a saving of time and labour; absence of davits,
anchor-beds and other gear, with a resulting reduction in
weight; and a clear forecastle for ``right ahead'' gun fire
or for working ship. On the other hand a larger hawse-pipe is
required, and there appears to be a consensus of opinion that
a stockless anchor when ``let go'' does not hold so quickly
as a stocked one, is more uncertain in its action over uneven
ground, and is more liable to ``come home,' (drag). The
stockless anchors principally in use in the British navy are
Hall's improved, Byer's, and Wasteneys Smith's. In Hall's
improved (fig. 5) the arms and crown of cast steel are in one
piece, and the shank of forged steel passes up through an
aperture in the crown to which it is secured by two cross
bolts. Two trunnions or lugs are forged to the lower end of the
shank. In Byer's plan (fig. 6) the flukes and crown consist
of a steel-casting secured to a forged shank by a through bolt
of mild steel, the axis of which is parallel to the points
of the flukes; one end of the bolt has a head, but the other
is screwed and fitted with a phosphor bronze nut to allow the
bolt to be withdrawn for examination. A palm is cast on each
side of the crown to trip the flukes when the anchor is on the
ground, and for bringing them snug against the ship's side when
weighing. Wasteneys Smith's anchor (fig. 7) is composed of
Fig. 7.--Wasteneys Smith's Stockless anchor.
three main parts, the shank and crown which form one forging,
and the two flukes or arms which are separate castings. A bolt
passes through the crown of the anchor, connecting the flukes
to it; to prevent the flukes working off the connecting through
bolt, two smaller bolts pass through the flukes at right angles
to the through bolt and are recessed half their diameter into it.
Fig. 8 represents the starboard bow of H.M.S. ``New Zealand''
FIG. 8.--Starboard Bow of H.M.S. ``New Zealand.''
(16,350 tons) with lower and sheet (spare) anchors stowed.
To let go a stockless anchor (fig. 9) the cable or capstan
holder C is unscrewed, and in practice it is found desirable
to knock off the bottle screw-slip A, allowing the weight
of the anchor to be taken by the inner slip A' (Blake's
stopper). Stern, stream and kedge anchors are usually
stowed with special davits. A portable anchor suitable for
small yachts is the invention of Mr Louis Moore; the shank
passes through the crown of the anchor like the handle of
a pickaxe and the stock over the head of the shank. At
the end of the stock are loose pawls. There are no keys or
bolts, and the only fastening is for the cable. The anchor
takes to pieces readily and stows snugly. In 1890 Colonel
Bucknill also invented a portable anchor for small yachts.
Iron buoy-sinkers (fig. 10), as used by the London Trinity
House Corporation, weigh from 8 to 40 cwt.; the specified
weight is cast on them in large raised figures, and the
cast and wrought irons used are of special quality, of which
samples are previously submitted to the engineer-in-chief.
The anchors supplied to ships of the British navy are reqaired
FIG. 9.--Forecastle of H.M.S. ``New Zealand.,' A.
Bottle or screw-slip. B. Deck or navel pices. A'. Slip
or Blake's stopper. F. Fairleads for wire hawsers. D.
Bitts. H. Hawse-pipes. C. Cable or Capstan-holders. S.
Stopoer-bolts. C'. Centre line capstan. R. Rollers.
to withstand a certain tensile strain, expressed in tons,
proportionate to their weights in cwts. New anchors are
supplied by contractors, but repairs are made in H.M. dockyards,
a record of its repairs being stamped on each anchor. In
the Anchors and Cables Act 1899 a list is given of authorized
testing-establishments, with their distinctive marks and
charges, and testing- houses for foreign-owned vessels are
Fig. 10.--Iron Buoy- Sinker.
enumerated in Table 22 of Lloyd's Register of British and
Foreign Shipping. Cast-steel anchors, in addition to the
statutory tests, are subjected to percussive, hammering and
bending tests, and are stamped ``annealed steel.'' (J. W. D.)
ANCHOVY (Engraulis encrasicholus), a fish of the herring
family, easily distinguished by its deeply-cleft mouth,
the angle of the gape being behind the eyes. The pointed
snout extends beyond the lower jaw. The fish resembles a
sprat in having a forked tail and a single dorsal fin, but
the body is round and slender. The maximum length is 8 1/8
in. Anchovies are abundant in the Mediterranean, and are
regularly caught on the coasts of Sicily, Italy, France and
Spain. The range of the species also extends along the
Atlantic coast of Europe to the south of Norway. In winter
it is common off Devon and Cornwall, but has not hitherto been
caught in such numbers as to be of commercial importance. Off
the coast of Holland in summer it is more plentiful, entering
the Zuider Zee in such numbers as to give rise to a regular
and valuable fishery. It is also taken in the estuary of the
Scheldt. There is reason to believe that the anchovies found
at the western end of the English Channel in November and
December are those which annually migrate from the Zuider
Zee and Scheldt in autumn, returning thither in the following
spring; they must be held to form an isolated stock, for
none come up from the south in summer to occupy the English
Channel, though the species is resident on the coast of
Portugal. The explanation appears to be that the shallow
and landlocked waters of the Zuider Zee, as well as the sea
on the Dutch coast, become raised to a higher temperature
in summer than any part of the sea about the British coasts,
and that therefore anchovies are able to spawn and maintain
their numbers in these waters. Their reproduction and
development were first described by a Dutch naturalist from
observations made on the shores of the Zuider Zee. Spawning
takes place in June and July, and the eggs, like those of
the majority of marine fishes, are buoyant and transparent,
but they are peculiar in having an elongated, sausage-like
shape, instead of being globular. They resemble those of
the sprat and pilchard in having a segmented yolk and there
is no oil globule. The larva is batched two or three days
after the fertilization of the egg, and is very minute and
transparent. In August young specimens 1 1/2 to 3 1/2 in. in
length have been taken in the Zuider Zee, and these must be
held to have been derived from the spawning of the previous
summer. There is no evidence to decide the question whether
all the young anchovies as well as the adults leave the Zuider
Zee in autumn, but, considering the winter temperature there,
it is probable that they do. The eggs have also been obtained
from the Bay of Naples, and near Marseilles, also off the coast
of Holland, and once at least off the coast of Lancashire.
The occurrence of anchovies in the English Channel has been
carefully studied at the laboratory of the Marine Biological
Association at Plymouth. They were most abundant in 1889 and
1890. In the former year considerable numbers were taken
off Dover in drift nets of small mesh used for the capture of
sprats. In the following December large numbers were taken
together with sprats at Torquay. In November 1890 a thousand
of the fish were obtained in two days from the pilchard boats
fishing near Plymouth; these were caught near the Eddystone.
When taken in British waters anchovies are either thrown away
or sent to the market fresh with the sprats. If salted in
the proper way, they would doubtless be in all respects equal
to Dutch anchovies, if not to those imported from Italy. The
supply, however, is small and inconstant, and for this reason
English fish-curers have not learnt the proper way of preparing
them. The so-called ``Norwegian anchovies'' imported into
England in little wooden kegs are nothing but sprats pickled
in brine with bay-leaves and whole pepper. (J. T. C.)
ANCIEN REGIME, THE, a French phrase commonly used, even
by English writers, to denote the social and political system
established in France under the old monarchy, which was swept
away by the Revolution of 1789. The phrase is generally
applicable only to France, for in no other country, with perhaps
the exception of Japan, has there been in modern times so
clearly marked a division between ``the old order'' and the new.
ANCIENT (also spelt ANTIENT; derived, through the Fr.
ancien, old, from the late Lat. anitianum, from ante,
before), old or in olden times. ``Ancient history'' is
distinguished from medieval and modern, generally as meaning
before the fall of the western Roman empire. In English legal
history, ``ancient'' tenure or demesne refers to what was
crown property in the time of Edward the Confessor or William
the Conqueror. ``The Ancient of days'' is a Biblical phrase
for God. In the London Inns of Court the senior barristers
used to be called ``ancients.'' From the 16th to the 18th
century the word was also used, by confusion with ``ensign,''
i.e; flag or standard-bearer, for that military title, as
in the case of Shakespeare's ``ancient Pistol''; but this
use has nothing to do with ``ancient'' meaning ``old.''
ANCIENT LIGHTS, a phrase in English law for a negative
easement (q.v.) consisting in the right to prevent the
owner or occupier of an adjoining tenement from building
or placing on his own land anything which has the effect of
illegally obstructing or obscuring the light of the dominant
tenement. At common law a person, who opens a window in his
house, has a natural right to receive the flow of light
that passes through it. But his neighbour is not debarred
thereby from building on his own land even though the
effect of his action is to obstruct the flow of light thus
obtained. Where, however, a window had been opened for so
long a time as to constitute immemorial usage in law, the
light became an ``ancient light'' which the law protected from
disturbance. The Prescription Act 1832 created a statutory
prescription for light. It provided (s. 3) that ``when the
access and use of light to and for'' (any building) ``shall
have been actually enjoyed therewith for the full period of
20 years without interruption, the right thereto shall be
deemed absolute and indefeasible, any local usage or custom
to the contrary notwithstanding, unless it shall appear that
the same was enjoyed by some consent or agreement, expressly
made or given for that purpose by deed or writing.'' The
statute does not create an absolute or indefeasible right
immediately on the expiration of twenty years. Unless and
until the dominant owner's claim is brought into question
(s.4) no absolute or indefeasible title can arise under the
act. The dominant owner has only an inchoate right to avail
himself under the act of the twenty years' uninterrupted
enjoyment, if his claim is brought into question. But in the
meantime, however long the enjoyment may have been, his right
is just the same, and the origin of his right is just the
same as if the act had never been passed. These principles
were laid down in 1904 by the House of Lords in the leading
case of Colls v. Home & Colonial Stores Ltd. (1904 A.C.
179). They overrule an earlier view propounded by Lord
Westbury in 1865 (Tapling v. Jones, 11 H.L.C. 290) that the
Prescription Act 1832 had abrogated the common law prescription
as to light, that the right to ``ancient lights'' now depends
upon positive enactment alone, and does not require, and
ought not to be rested on, any fiction of a ``lost grant''
(see EASEMENT.) There has been much difference of judicial
opinion as to what constitutes an actionable interference
with ``ancient lights.'' On the one hand, the test has
been prescribed that if an angle of 45 deg. --uninterrupted sky
light--was left, the easement was not interfered with, and,
while this is not a rule of law, it is a good rough working
criterion. On the other hand, it was held in effect by the
Court of Appeal in the case of Colls v. Home & Colonial
Stores Ltd. (1902; 1 Ch. 302) that to constitute an actionable
obstruction of ancient lights it was sufficient if the light
was sensibly less than it was before. The House of Lords,
however, in the same case (1904 A. C. 179) overruled this
view, and held that there must be a substantial privation
of light enough to render the occupation of the house or
building uncomfortable according to the ordinary notions of
mankind and (in the case of business premises) to prevent the
plaintiff from carrying on his business as beneficially as
before. See also Kine v. Jolly (1905; 1 Ch. 480).
There is, in Scots law, no special doctrine as to ``ancient
lights.'' The servitude of light in Scotland is simply the
Roman servitude non officiendi luminibus vel prospectui (see
EASEMENT and ROMAN LAW). The same observation applies
to the Code Civil and other European Codes based on it. The
doctrine as to ancient lights does not prevail generally in
the United States (consult Rulinig Cases, under ``Air'').
ANCILLARY (from the Lat. anicilla, a handmaid), an
adjective meaning ``subordinate to'' or ``merely helping,''
as opposed to ``essential.'' By Thackeray and some other
writers it is also employed rather affectedly in its
primary meaning of ``pertaining to a maid-servant.''
ANCILLON, CHARLES (1659--1715), one of a distinguished family
of French Protestants, was born on the 28th of July 1659, at
Metz. His father, David Ancillon (1617-1692), was obliged
to leave France on the revocation of the edict of Nantes,
and became pastor of the French Protestant community in
Berlin. Charles Ancillon studied law at Marburg, Geneva, and
Paris, where he was called to the bar. At the request of the
Huguenots at Metz, he pleaded its cause at the court of Louis
XIV., urging that it should be excepted in the revocation of
the edict of Nantes, but his efforts were unsuccessful, and
he joined his father in Berlin. He was at once appointed
by the elector Frederick ``juge et directeur de colonic
de Berlin.'' He had before this published several works on
the revocation of the edict of Nantes and its consequences,
but his literary capacity was mediocre, his style stiff and
cold, and it was his personal character rather than his
reputation as a writer that earned him the confidence of the
elector. In 1687 he was appointed head of the so-called
Academie des nobles, the principal educational establishment
of the state; later on, as councillor of embassy, he took
part in the negotiations which led to the assumption of
the title of king by the elector. In 1699 he succeeded
Pufendorf as historiographer to the elector, and the same
year replaced his uncle Joseph Ancillon as judge of all the
French refugees in Brandenburg. He died on the 5th of July
1715. Ancillon's chief claim to remembrance is the work
that he did for education in Prussia, and the share he took,
in co-operation with Leibnitz, in founding the Academy of
Berlin. Of his fairly numerous works the only one still
of value is the Histoire de l'etablissement des Francais
refugies dans les etats de Brandebourg (Berlin, 1690).
ANCILLON, JOHANN PETER FRIEDRICH (1766-1837), Prussian
historian and statesman, great-grandson of Charles Ancillon,
was born at Berlin on the 30th of April 1766. He studied
theology at Geneva, and after finishing his course was
appointed minister to the French community at Berlin.
At the same time his reputation as a historical scholar
secured him the post of professor of history at the military
academy. In 1793 he visited Switzerland, and in 1796 France,
and published the impressions gathered during his travels
in a series of articles which he afterwards collected under
the title of Melanges de litterature et de philosophie
(1801). Ancillon took rank among the most famous historians
of his day by his next work, Tableau des revolutions
du systeme politique de l'Europe depuis le XVe siecle
(1803, 4 vols.; new ed., 1824), which gained him the eulogium
of the Institute of France, and admission to the Academy of
Berlin. It was the first attempt to recognize psychological
factors in historical movements, but otherwise its importance was
exaggerated. Its ``sugary optimism, unctuous phraseology and
pulpit logic'' appealed, however, to the reviving pietism of
the age succeeding the Revolution, and these qualities, as well
as his eloquence as a preacher, early brought Ancillon into
notice at court. In 1808 he was appointed tutor to the royal
princes, in 1809 councillor of state in the department of
religion, and in 1810 tutor of the crown prince (afterwards
Frederick William IV.), on whose sensitive and dreamy
nature he was to exercise a powerful but far from wholesome
influence. In October 1814, when his pupil came of age, Ancillon
was included by Prince Hardenberg in the ministry, as privy
councillor of legation in the department of foreign affairs,
with a view to utilizing his supposed gifts as a philosophical
historian in the preparation of the projected Prussian
constitution. But Ancillon's reputed liberalism was of too
invertebrate a type to survive the trial of actual contact with
affairs. The practical difficulty of the constitutional problem
gave the ``court parson''--as Gneisenau had contemptuously
called him--excuse enough for a change of front which,
incidentally, would please his exalted patrons. He covered
his defection from Hardenberg's liberal constitutionalism
by a series of ``philosophical'' treatises on the nature of
the state and of man, and became the soul of the reactionary
movement at the Berlin court, and the faithful henchman of
Metternich in the general politics of Germany and of Europe.
In 1817 Ancillon became a councillor of state, and in 1818
director of the political section of the ministry for foreign
affairs under Count Bernstorff. In his chief's most important
work, the establishment of the Prussian Zollverein, Ancillon
had no share, while the entirely subordinate role played
by Prussia in Europe during this period, together with the
personal part taken by the sovereign in the various congresses,
gave him little scope for the display of any diplomatic
talents he may have possessed. During this time he found
plentiful leisure to write a series of works on political
philosophy, such as the Nouveaux essais de politique et
de philosophie (Paris, 1824). In May 1831 he was made an
active privy councillor, was appointed chief of the department
for the principality of Neuchatel, in July became secretary
of state for foreign affairs, and in the spring of 1832, on
Bernstorff's retirement, succeeded him as head of the ministry.
By the German public, to whom Ancillon was known only through
his earlier writings and some isolated protests against the
``demagogue-hunting'' in fashion at Berlin, his advent to
power was hailed as a triumph of liberalism. They were soon
undeceived. Ancillon had convinced himself that the rigid class
distinctions of the Prussian system were the philosophically
ideal basis of the state, and that representation ``by estates''
was the only sound constitutional principle; his last and indeed
only act of importance as minister was his collaboration with
Metternich in the Vienna Final Act of the 12th of June 1834,
the object of which was to rivet this system upon Germany for
ever. He died on the 19th of April 1837, the last of his
family. His historical importance lies neither in his
writings nor in his political activity, but in his personal
influence at the Prussian court, and especially in its
lasting effect on the character of Frederick William IV.
See C. A. L. P. Varnhagen von Ense, Blatter aus der
preussischen Geschichte, 5 vols. (Leipzig, 1868-1869);
ib. Tagebucher, vol. i. (Leipzig, 1861); H. O. Treitschke,
Deutsche Geschichte (Leipzig, 1879-1894), and essay
on Ancillon in Preussiche Jahrbucher for April 1872;
Allgemeine Deutsche Biographie, s.v. (Leipzig, 1875).
ANCON, a small village and bathing-place on the coast
of Peru, 22 m. N. of Lima by rail. The bay is formed
by two projecting headlands and is one of the best on the
coast. It has a gently sloping beach of fine sand and has
been a popular bathing-place since the time of President
Balta, although the country behind it is arid and absolutely
barren. At some time previous to the discovery of America,
Ancon had a large aboriginal population. Traces of
terraces on the southern headland can still be seen, and the
sand-covered hills and slopes overlooking the bay contain
extensive burial-grounds which were systematically explored
in 1875 by Messrs W. Reiss and A. Stubel (see Reiss and
Stubel's The Necropolis of Anicon in Peru, translated by
A. H. Keane, 3 vols., Berlin, 1880-1887). In modern times
Ancon has been the scene of several important historical
events. Its anchorage was used by Lord Cochrane in 1820
during his attacks on Callao; it was the landing-place of
an invading Chilean army in 1838; it was bombarded by the
Chileans in 1880; and in 1883 it was the meeting-place
of the Chilean and Peruvian commissioners who drew up the
treaty of Ancon, which ended the war between Chile and Peru.
ANCON (from the Gr. agkon), the anatomical name for
``elbow''; ``ancones'' in architecture are the projecting
bosses left on stone blocks or on drums of columns, to allow
of their being either hoisted aloft or rubbed backwards and
forwards to obtain a fine joint; the term is also given by
Vitruvius to the trusses or console brackets on each side
of the doorway of a Greek or Roman building which support
the cornice over the same. A particular sort of sheep,
with short crooked forelegs, is called ``ancon'' sheep.
ANCONA, ALESSANDRO (1835- ), Italian critic and man of
letters, was born at Pisa on the 20th of February 1835, of
a wealthy Jewish family, and educated in Florence; at the
age of eighteen he published his essay on the life and work
of the philosopher Tommaso Campanella. In 1855 Ancona went
to Turin, nominally to study law, but in reality to act as
intermediary between the Tuscan Liberals and Cavour; he was an
intimate friend of Luigi Carlo Farini (q.v.) and represented
Tuscany in the Societa Nazionale. On the fall of the Austrian
dynasty in Tuscany (April 27, 1859) he returned to Florence,
where he edited the newly founded newspaper La Nazionie.
In 1861 he was appointed professor of Italian literature at
the university of Pisa. Among his works the following may
be mentioned: Operadi Tommaso Campanella, 2 vols. (Turin,
1854); Sacre Rappresentazioni dei secoli XIV., XV., e XVI.
(3 vols., Florence, 1872); Origini del Teatro in Italia (2
vols., Florence, 1877); La Poesia popolare italiana (Livorno,
1878), besides several volumes of literary essays, editions
of the works of Dante and other early Italian writers, &c.
ANCONA, a seaport and episcopal see of the Marches, Italy,
capital of the province of Ancona, situated on the N.E. coast of
Italy, 185 m. N.E. of Rome by rail and 132 m. direct, and 127
m. S.E. of Bologna. Pop. (1901) 56,835. The town is finely
situated on and between the slopes of the two extremities
of the promontory of Monte Conero, Monte Astagno to the S.,
occupied by the citadel, and Monte Guasco to the N., on which
the cathedral stands (300 ft.). The latter, dedicated to S.
Ciriaco, is said to occupy the site of a temple of Venus, who
is mentioned by Catullus and Juvenal as the tutelary deity
of the place. It was consecrated in 1128 and completed in
1189. Some writers suppose that the original church was in
the form of a Latin cross and belonged to the 8th century.
An early restoration was completed in 1234. It is a fine
Romanesque building in grey stone, built in the form of a Greek
cross, with a dodecagonal dome over the centre slightly altered
by Margaritone d' Arezzo in 1270. The facade has a Gothic
portal, ascribed to Giorgio da Como (1228), which was intended
to have a lateral arch on each side. The interior, which has
a crypt in each transept, in the main preserves its original
character. It has ten columns which are attributed to the
temple of Venus, and there are good screens of the 12th
century, and other sculptures. In the dilapidated episcopal
palace Pope Pius II. died in 1464. An interesting church
is S. Maria della Piazza, with an elaborate arcaded facade
(1210). The Palazzo del Comune, with its lofty arched
substructures at the back, was the work of Margaritone d'
Arezzo, but has been since twice restored. There are also
several fine late Gothic buildings, among them the churches
of S. Francesco and S. Agostino, the Palazzo Benincasa, and
the Loggia dei Mercanti, all by Giorgio Orsini, usually called
da Sebenico (who worked much at Sebenico, though he was not
a native of it), and the prefecture, which has Renaissance
additions. The portal of S. Maria della Misericordia is an
ornate example of early Renaissance work. The archaeological
museum contains interesting pre-Roman objects from tombs in
the district, and two Roman beds with fine decorations in
ivory (E. Brizio, in Notizie degli scavi, 1902, 437, 478).
To the east of the town is the harbour, now an oval basin of
990 by 880 yards, the finest harbour on the S. W. coast of the
Adriatic, and one of the best in Italy. It was originally
protected only by the promontory on the N., from the elbow-like
shape of which (Gk. agkon) the ancient town, founded by
Syracusan refugees about 390 B.C., took the name which it still
holds. Greek merchants established a purple factory here
(Sil. Ital. viii. 438). Even in Roman times it kept its
own coinage with the punning device of the bent arm holding
a palm branch, and the head of Aphrodite on the reverse, and
continued the use of the Greek language. When it became a
Roman colony is doubtful.1 It was occupied as a naval station
in the Illyrian war of 178 B.C. (Liv. xli. 1). Caesar took
possession of it immediately after crossing the Rubicon. Its
harbour was of considerable importance in imperial times, as
the nearest to Dalmatia,2 and was enlarged by Trajan, who
constructed the north quay, his architect being Apollodorus of
Damascus. At the beginning of it stands the marble triumphal
arch with a single opening, and without bas-reliefs, erected
in his honour in A.D. 115 by the senate and people. Pope
Clement II. prolonged the quay, and an inferior imitation of
Trajan's arch was set up; he also erected a lazaretto at the
south end of the harbour, now a sugar refinery, Vanvitelli
being the architect-in-chief. The southern quay was built
in 1880, and the harbour is now protected by forts on the
heights, while the place is the seat of the 7th army corps.
The port of Ancona was entered in 1904 by 869 steamships
and 600 sailing vessels, with a total tonnage of 961,612
tons. The main imports were coal, timber, metals,
jute. The main exports were asphalt and calcium
carbide. Sugar refining and shipbuilding are carried on.
Ancona is situated on the railway between Bologna and Brindisi,
and is also connected by rail with Rome, via Foligno and Orte.
After the fall of the Roman empire Ancona was successively
attacked by the Goths, Lombards and Saracens, but recovered
its strength and importance. It was one of the cities of
the Pentapolis under the exarchate of Ravenna, the other four
being Fano, Pesaro, Senigallia and Rimini, and eventually
became a semi-independent republic under the protection of
the popes, until Gonzaga took possession of it for Clement
VII. in 1532. From 1797 onwards, when the French took it,
it frequently appears in history as an important fortress,
until Lamoriciere capitulated here on the 29th of September
1860, eleven days after his defeat at Castelfidardo. (T. As.)
1 Scanty remains of the ancient town walls, of a gymnasium
near the harbour and of the amphitheatre are still extant.
2 It was connected by a road with the Via
Flaminia at Nuceria (Norcera), a distance of 70 m.
ANCREN RIWLE, a Middle English prose treatise written for
a small community of three religious women and their servants
at Tarent Kaines (Tarrant Crawford), at the junction of the
Stour and the Tarrant, Dorset. It was generally supposed to
date from the first quarter of the 13th century, but Professor
E. Kolbing is inclined to place the Corpus Christi MS.
about the middle of the 12th century. The house of Tarrant
was founded by Ralph de Kahaines, and greatly enriched about
1230 by Richard Poor, bishop successively of Chichester,
Salisbury and Durham, who was born at Tarrant and died there in
1237. At the time when the Ancren Riwle was addressed to
them the anchoresses did not belong to any of the monastic
orders, but the monastery was under the Cistercian rule before
1266.1 There are extant seven English MSS. of the work, and
one Latin, the Latin version being generally supposed to be a
translation. The Latin MS., Regula Anachoritarum sive de vita
solitaria ( Magdalen College, Oxford, No. 67, fol. 50) has
a prefatory note:-- Hic incipit prohemium venerabilis patris
magistri Simonis de Gandavo, episcopi Sarum, in librum de
vita solitaria, qaem scripsit sororibus suis anachoritis
apud Tarente. But Bishop Simon of Ghent, who died in 1315,
could not have written the book, if it dates, at latest, from
the early 13th century. It has been tentatively attributed
to Richard Poor, who was connected with Tarrant, and was
actually a benefactor of the monastery. But the adoption of
Prof. Kolbing's early date would almost destroy Poor's claim.
The Ancren Riwle is written in a simple, non-rhetorical
style. The severity of the doctrine of self-renunciation
is softened by the affectionate tone in which it is
inculcated. The book contains rules for the conduct of the
anchoresses, and gives liturgical directions for divine
service; but the greater part of it is taken up with the
purely spiritual side of religion. The rules for the
restraint of the senses, for Confession and penance, are
subordinated to the central idea of the supreme importance
of purity of heart and the love of Christ. The last chapter
deals with the domestic affairs and administration of the
monastery. Incidentally the writer gives a picture of the
manners and ideas of the time, and provides an account of
the doctrine then generally accepted in the English church.
Ancren Riwale was edited for the Camden Society by the Rev.
James Morton in 1843 from the Cotton MS. (Nero A xiv.). A
collation of this text with the MS. by E. Kolbing is printed
in the Jahrbuch fur romanische u. engl. Spr. und Lit.
xv. 180 seq. (1876). The Ancren Riwle (ed. Abbot F. A.
Gasquet, 1905) is available for the ordinary reader in The
King's Classics. There are three English MSS. of Ancren
Riwle in the Cottonian collection in the British Museum,
numbered Nero A xiv., Titus D xviii., and Cleopatra C vi. Nero
A xiv. is written in pure south-western dialect. Portions of
this text are printed in Henry Sweet's First Middle English
Primer (Oxford, 2nd ed., 1895), which contains a grammatical
introduction. MS. 402 in the library of Corpus Christi
College, Cambridge, contains the earliest version of Ancren
Riwle, entitled Ancren Wisse, and dating (according to E.
Kolbing in Englische Studien, 1886, vol. ix. 116) from about
1150. The language shows considerable traces of the Midland
dialect. MS. 234 in Caius College, Cambridge, contains a
considerable portion of the Ancren Riwle, but does not
follow the order of the other MSS. For its exact contents
see Kolbing, in Englische Studien, iii. 533 (1880).
A more recently discovered version in Magdalene College,
Cambridge, in MS. Pepys 2498, is entitled The Recluse, and
is abridged and differently arranged. It ir written in English
of the latter half of the 14th century (see A. C. Paues in
Englische Studien, xxx. 344-346, 1902). A Latin version
(Cotton MS. Vitellins E vii.), and a French copy (ibid.
F vii.) were seriously damaged in the fire at Ashburnham
House, but both MSS. have been recently restored. The Latin
MS. (Codex lxvii.) at Magdalen College, Oxford, is probably
a copy of another Latin text, for it contains obvious slips.
See also R. Wulker, ``Uber die Sprache der Ancren Riwle
und die der Homilie: Halli Meidenhad,'' in Beitrage zur
Geschichte der deutschen Sprache und Literatur (Halle,
1874, i. 209), giving an analysis of the differences in
dialect between the two works; and Edgar Elliott Bramlette,
``The Original Language of the Ancren Riwle,'' in
Anglia, xv. 478-498, arguing in favour of a Latin original.
1 For information on the subject of Tarent Kaines see Sir W.
Dugdale, Monasticon Anglicanum (new ed., 1846), vol. v. 619 et seq.
ANCRUM, a village on Ale or Alne Water (a tributary of the
Teviot), Roxburghshire, Scotland, 2 m. W. of Jedfoot Bridge
station on the Roxburgh-Jedburgh branch of the North British
railway. Pop. (1901) 973. The earlier forms of the name,
``Alnecrumba,'' ``Ankrom'' and ``Alnecrom,'' indicate its
Gaelic derivation from crom, ``crooked''--``the crook or
bend of the Alne.'' The village is of considerable antiquity,
and was formerly held by the see of Glasgow. Its cross,
said to date from the time of David I., is one of the best
preserved crosses in the Border counties. Ancrum Moor, 2
m. N.W., was the scene of the battle in which, on the 17th
of February 1545, the Scots under the earl of Angus, Sir
Walter Scott of Buccleuch, and Norman Leslie, defeated 5000
English, whose leaders, Sir Ralph Evers or Eure and Sir
Brian Latoun or Layton, were slain. A Roman road, 24 ft.
broad, forms the N.E. boundary of the parish of Ancrum.
ANCUS MARCIUS (640-616 B.C.), fourth legendary king of
Rome. Like Numa, his reputed grandfather, he was a friend of
peace and religion, but was obliged to make war to defend his
territories. He conquered the Latins, and a number of them he
settled on the Aventine formed the origin of the Plebeians. He
fortified the Janiculum, threw a wooden bridge across the Tiber,
founded the port of Ostia, established salt-works and built a prison.
Ancus Marcius is merely a duplicate of Numa, as is shown by
his second name, Numa Marcius, the confidant and pontifex of
Numa, being no other than Numa Pompilius himself, represented as
priest. The identification with Ancus is shown by the legend
which makes the latter a bridge-builder (pontifex), the
constructor of the first wooden bridge over the Tiber. It is
in the exercise of his priestly functions that the resemblance
is most clearly shown. Like Numa, Ancus died a natural death.
See Livy i. 32, 33; Dion Halic. iii. 36-45; Cicero, De
Republica, ii. 18. For a critical examination of the story
see Schwegler, Romische Geschichte, bk. xiii.; Sir G.
Cornewall kewis, Credibility of Early Roman History,
ch. xi.; W. Ihne, History of Rome, i.; R. Pais, Storia di
Roma, i. (1898), who considers that the name points to the
personification of the cult of Mars, and that the military
achievements of Ancus are anticipations of later events.
ANCYLOPODA, or ANCYLODACTYLA, an apparently primitive extinct
subordinal group of Ungulata showing certain resemblances to
the Perissodactyla, both as regards the cheek-teeth and the
skeleton, but broadly distinguished by the feet being of
an edentate type, carrying long curved and cleft terminal
claws. From this peculiar structure of the feet it would
seem that the weight of the body was mainly carried on their
outer sides, as in Edentates. The group is typified by
Chalicotherium, of which the original species was discovered
in the Lower Pliocene strata of Eppelsheim, Hesse-Darmstadt,
in 1825, and named on the evidence of the teeth, the limbs
being subsequently described as Macrotherium. The skull
is short, with a dental formula of i. 3/3, c. 0/1, p. 3/3,
m. 3/3, but in fully adult animals most of the front teeth were
shed. The molar teeth recall those of Palaeosyops (see
TITANOTHERIIDAE.) Remains referred to Chalicotherium
have been also obtained from the Lower Pliocene and Upper
Miocene strata of Greece, Hungary, India, China and North
America. A skull from Pikermi, near Mt. Pentelikon,
Attica, shows the absence in the adult state of upper and
lower incisors and upper canines, much the same condition
being indicated in an Indian skull. There were three toes
to each foot, and the femur lacked a third trochanter.
Macrotherium, which is typically from the Middle Miocene
of Sansan, in Gers, France, may indicate a distinct genus.
Limb-bones nearly resembling those of Macrotherium, but
relatively stouter, have been described from the Pliocene beds
of Attica and Samos as Ancylotherium. In America the names
Morothorium and Moropus have been applied to similar bones,
on the belief that they indicated edentates. Macrotherium
magnum must have been an animal of about 9 ft. in length.
The South American genus Homalodontotherium is often placed
in the Ancylopoda, but reasons against this view are given in
the article LITOPTERNA. Professor H. F. Osborn considers that
the Ancylopoda are directly descended from the Condylarthra.
See also H. F. Osborn, ``The Ancylopoda Chalicotherium and Artionyx,''
Amer. Nat. (1893), p. 118, and ``Artionyx, a New Genus of
Ancylopoda,'' Bull. Amer. Mus. vol. v. p. 1 (1893). (N.B.--
Artionyx was subsequently found to be an Artiodactyle.] (R. L.*)
ANCYRA (mod. Angora, q.v.), an ancient city of Galatia
in Asia Minor, situated on a tributary of the Sangarius.
Originally a large and prosperous Phrygian city on the Persian
Royal Road, Ancyra became the centre of the Tectosages,
one of the three Gaulish tribes that settled permanently in
Galatia about 232 B.C. The barbarian occupation dislocated
civilization, and the town sank to a mere village inhabited
chiefly by the old native population who carried on the
arts and crafts of peaceful life, while the Gauls devoted
themselves to war and pastoral life (see GALATIA.) In 189
B.C. Ancyra was occupied by Cn. Manlius Vulso, who made
it his headquarters in his operations against the tribe.
In 63 B.C. Pompey placed it (together with the Tectosagan
territory) under one chief, and it continued under native rule
till it became the capital of the Roman province of Galatia
in 25 B.C. By this time the population included Greeks,
Jews, Romans and Romanized Gauls, but the town was not yet
Hellenized, though Greek was spoken. Strabo (c. A.D. 19)
calls it not a city, but a fortress, implying that it had none
of the institutions of the Graeco-Roman city. Inscriptions
and coins show that its civilization consisted of a layer
of Roman ideas and customs superimposed on Celtic tribal
characteristics, and that it is not until c. A.D. 150 that
the true Hellenic spirit begins to appear. Christianity was
introduced (from the N. or N.W.) perhaps as early as the 1st
century, but there is no shred of evidence that the Ancyran
Church (first mentioned A.D. 192) was founded by St Paul
or that he ever visited northern Galatia. The real greatness
of the town dates from the time when Constantinople became
the metropolis of the Roman world: then its geographical
situation raised it to a position of importance which it
retained throughout the middle ages. See further ANGORA (1).
The modern town contains many remains of the Roman and Byzantine
periods. The most important monument is the Augusteum,
a temple of white marble erected to ``Rome and Augustus''
during the lifetime of that emperor by the common council
or diet of the three Galatian tribes. The temple was
afterwards converted into a church, and in the 16th century
a fine mosque was built against its S. face. On the walls
of the temple is engraved the famous Monumentum Ancyranum,
a long inscription in Latin and Greek describing the Res
gestae divi Augusti; the Latin portion being inscribed on
the inner left-hand wall of the pronaos, the Greek on the
outside wall of the naos (cella.) The inscription is a
grave and majestic narrative of the public life and work of
Augustus. The original was written by the emperor in
his 76th year (A.D. 13-14) to be engraved on two bronze
tablets placed in front of his mausoleum in Rome, and as a
mark of respect to his memory a copy was inscribed on the
temple walls by the council of the Galatians. Thus has been
preserved an absolutely unique historical document of great
importance, recounting (1) the numerous public offices
and honours conferred on him, (2) his various benefactions
to the state, to the plebs and to his soldiers, and (3)
his military and administrative services to the empire.
BIBLIOGRAPHY.--C. Ritter, Erdkunde von Asien, vol.
xviii. (1837- 1859); Hamilton, Researches in A. M. (1842);
Texier, Descrip. de l'Asie Min. (1839-1849); Perrot,
Explor. de la Galatie (1862): Humann and Puchstein,
Reisen in Kleinasien (1890). For Mon. Ancyr., Mommsen,
Res gestae divi Augusti (1883); and Inscr. graecae ad
res Romanas pertinentes, iii. (1902). For coins, Brit.
Museum Catal., Galatia (1899); Babelon-Reinach, Recueil
general d, A. M. See also under GALATIA. (J. G. C. A.)
SYNOD OF ANCYRA.--An important ecclesiastical synod was held at
Ancyra, the seat of the Roman administration for the province of
Galatia, in A.D. 314. The season was soon after Easter; the
year may be safely deduced from the fact that the first nine
canons are intended to repair havoc wrought in the church by
persecution, which ceased after the overthrow of Maximinus in
313. The tenth canon tolerates the marriages of deacons who
previous to ordination had reserved the right to take a wife;
the thirteenth forbids chorepiscopi to ordain presbyters or
deacons; the eighteenth safeguards the right of the people in
objecting to the appointment of a bishop whom they do not wish.
See Mansi, ii. 514 ff. The critical text of R. B. Rackham
(Oxford, 1891), Studia Biblica et ecclesiastica,
iii. 139 ff., is conveniently reprinted in Lauchert 29
ff. H. R. Percival translates and comments on an old
text in the Nicene and Post-Nicene Fathers (2nd series),
xiv. 61 ff. An elaborate discussion is found in Hefele,
Concilien- geschichte (2nd ed.), i. 219 ff. (English
translation, i. 199 ff.); more briefly in Herzog-Hauck (3rd
ed.), i. 497. For full titles see COUNCIL. (W. W. R.*)
ANDALUSIA, or ANDALUCIA, a captaincy-general, and
formerly a province, of southern Spain; bounded on the
N. by Estremadura and New Castile, E. by Murcia and the
Mediterranean Sea, S. by the Mediterranean and Atlantic,
and W. by Portugal. Pop. (1900) 3,563,606; area, 33,777 sq.
m. Andalusia was divided in 1833 into the eight provinces of
Almeria, Cadiz, Cordova, Granada, Jaen, Huelva, Malaga and
Seville, which are described in separate articles. Its
ancient name, though no longer used officially, except to
designate a military district, has not been superseded in
popular speech by the names of the eight modern divisions.
Andalusia consists of a great plain, the valley of the
Guadalquivir, shut in by mountain ranges on every side except
the S.W., where it descends to the Atlantic. This lowland,
which is known as Andalucia Baja, or Lower Andalusia,
resembles the valley of the Ebro in its slight elevation above
sea-level (300-400 ft.), and in the number of brackish lakes
or fens, and waste lands (despoblados) impregnated with
salt, which seem to indicate that the whole surface was covered
by the sea at no distant geological date. The barren tracts
are, however, exceptional and a far larger area is richly
fertile. Some districts, indeed, such as the Vega of Granada,
are famous for the luxuriance of their vegetation. The
Guadalquivir (q.v.) rises among the mountains of Jaen and
flows in a south-westerly direction to the Gulf of Cadiz,
receiving many considerable tributaries on its way. On the
north, its valley is bounded by the wild Sierra Morena; on the
south, by the mountains of the Mediterranean littoral, among
which the Sierra Nevada (q.v.), with its peaks of Mulhacen
(11,421 ft.)and Veleta(11,148 ft.), is the most conspicuous.
These highlands, with the mountains of Jaen and Almeria on
the east, constitute Anidalucia Alta or Upper Andalusia.
No part of Spain has greater natural riches. The sherry
produced near Jerez de la Frontera, the copper of the Rio
Tinto mines and the lead of Almeria are famous. But the
most noteworthy characteristics of the province are, perhaps,
the brilliancy of its climate, the beauty of its scenery
(which ranges in character from the alpine to the tropical),
and the interest of its art and antiquities. The climate
necessarily varies widely with the altitude. Some of the
higher mountains are covered with perpetual snow, a luxury
which is highly prized by the inhabitants of the valleys,
where the summer is usually extremely hot, and in winter the
snow falls only to melt when it reaches the ground. Here the
more common European plants and trees give place to the wild
olive, the caper bush, the aloe, the cactus, the evergreen
oak, the orange, the lemon, the palm and other productions
of a tropical climate. On the coasts of the Mediterranean
about Marbella and Malaga, the sugar-cane is successfully
cultivated. Silk is produced in the same region. Agriculture
is in a very backward state and the implements used are
most primitive. The chief towns are Seville (pop. 1900,
148,315), which may be regarded as the capital, Malaga
(130,109), Granada (75,900), Cadiz (69,382), Jerez de la
Frontera (63,473), Cordova (58,275) and Almeria (47,326).
Andalusia has never been, like Castile or Aragon, a separate
kingdom. Its history is largely a record of commercial and
artistic development. The Guadalquivir valley is often,
in part at least, identified with the biblical Tarshish
and the classical Tartessus, a famous Phoenician mart.
The port of Agadir or Gaddir, now Cadiz, was founded as
early as 1100 B.C. Later Carthaginian invaders came from
their advanced settlements in the Balearic Islands, about
516 B.C. Greek merchants also visited the coasts. The
products of the interior were conveved by the native Iberians
to the maritime colonies, such as Abdera (Adra), Calpe
(Gibraltar) or Malaca (Malaga), founded by the foreign
merchants. The Punic wars transferred the supreme power from
Carthage to Rome, and Latin civilization was established firmly
when, in 27 B.C., Andalusia became the Roman province of
Baetica--so called after its great waterway, the Baetis
(Guadalquivir). In the 5th century the province was overrun
by successive invaders--Vandals, Suevi and Visigoths-- from
the first of whom it may possibly derive its name. The forms
Vandalusia and Vandalitia are undoubtedly ancient; many
authorities, however, maintain that the name is derived from
the Moorish Andalus or Andalosh, ``Land of the West.''
The Moors first entered the province in 711, and only in 1492
was their power finally broken by the capture of Granada.
Their four Andalusian kingdoms, Seville, Jaen, Cordova and
Granada, developed a civilization unsurpassed at the time in
Europe. An extensive literature, scientific, philosophical and
historical, with four world-famous buildings--the Giralda and
Alcazar of Seville, the Mezquita or cathedral of Cordova and the
Alhambra at Granada--are its chief monuments. In the 16th and
17th centuries, painting replaced architecture as the distinctive
art of Andalusia; and many of the foremost Spanish painters,
including Velazquez and Murillo, were natives of this province.
Centuries of alien domination have left their mark upon the
character and appearance of the Andalusians, a mixed race,
who contrast strongly with the true Spaniards and possess
many oriental traits. It is impossible to estimate the
influence of the elder conquerors, Greek, Carthaginian and
Roman; but there are clear traces of Moorish blood, with
a less well-defined Jewish and gipsy strain. The men are
tall, handsome and well-made, and the women are among the most
beautiful in Spain; while the dark complexion and hair of both
sexes, and their peculiar dialect of Spanish, so distasteful
to pure Castilians, are indisputable evidence of Moorish
descent. Their music, dances and many customs, come from the
East. In general, the people are lively, good-humoured
and ready-witted, fond of pleasure, lazy and extremely
superstitious. In the literature and drama of his country,
the Andalusian is traditionally represented as the Gascon of
Spain, ever boastful and mercurial; or else as a picaresque
hero, bull-fighter, brigand or smuggler. Andalusia is
still famous for its bull-fighters; and every outlying
hamlet has its legends of highwaymen and contraband.
In addition to the numerous works cited under the heading
SPAIN, see Curiosidades historicas de Andalucia, by N.
Diaz de Escovar (Malaga, 1900): Histoire de la conquete de
l'Andalousie, by O. Houdas (Paris, 1889); Andalousie et Portugal
(Paris, 1886); El. Folk-Lore Andaluz (Seville, 1883); and
Nobleza de Andalucia, by G. Argote de Molina (Seville, 1588).
ANDALUSITE, a mineral with the same chemical composition
as cyanite and sillimanite, being a basic aluminium silicate,
Al2SiO5. As in sillimanite, its crystalline form is
referable to the orthorhombic system. Crystals of andalusite
have the form of almost square prisms, the prism-angle
being 89 deg. 12'; they are terminated by a basal plane and
sometimes by small dome-faces. As a rule the crystals are
roughly developed and rude columnar masses are common, these
being frequently altered partially to kaolin or mica. Such
FIG. 1.
crystals, opaque, and of a greyish or brownish colour, occur
abundantly in the mica-schist of the Lisens Alp near Innsbruck
in Tirol, while the first noted of the many localities of the
mineral is in Andalusia, from which place the mineral derives its
name. The unaltered mineral is found as transparent pebbles
with topaz in the gem-gravels of the Minas Novas district,
in Minas Geraes, Brazil. These pebbles are usually green
but sometimes reddish-brown in colour, and are remarkable for
their very strong dichroism, the same pebble appearing green
or reddish-brown according to the direction in which it is
viewed. Such specimens make very effective gem-stones,
the degree of hardness of the mineral (H.= 7 1/2) being quite
sufficient for this purpose. Its specific gravity is 3.18; it
is unattacked by acids and is infusible before the blowpipe.
FIG. 2.--Transverse sections of a crystal of Chiastolite.
Andalusite is typically a mineral of metamorphic origin,
occurring most frequently in altered clay-slates and crystalline
schists, near the junction of these with masses of intrusive
igneous rocks such as granite. It has been recognized
also, however, as a primary constituent of granite itself.
A curious variety of andalusite known as chiastolite is
specially characteristic of clay-slates near a contact with
granite. The elongated prismatic crystals enclose symmetrically
arranged wedges of carbonaceous material, and in cross-section
show a black cross on a greyish ground. Cross-sections of such
crystals are polished and worn as amulets or charms. Crystals
of a size suitable for this purpose are found in Brittany and
the Pyrenees, while still larger specimens have been found
recently in South Australia. The name chiastolite is derived
from the Greek chiastos, crossed or marked with the latter ch:
cross-stone and macle are earlier names, the latter having
been given on account of the resemblance the cross-section of
the stone bears to the heraldic macula or mascle. (L. J. S.)
ANDAMAN ISLANDS, a group of islands in the Bay of Bengal.
Large and small, they number 204, and lie 590 m. from the mouth
of the Hugli, 120 m. from Cape Negrais in Burma, the nearest
point of the mainland, and 340 m. from the northern extremity of
Sumatra. Between the Andamans and Cape Negrais intervene two
small groups, Preparis and Cocos; between the Andamans and
Sumatra lie the Nicobar Islands, the whole group stretching
in a curve, to which the meridian forms a tangent between Cape
Negrais and Sumatra; and though this curved line measures 700
m., the widest sea space is about 91 m. The extreme length
of the Andaman group is 219 m. with an extreme width of 32
m. The main part of it consists of a band of five chief islands,
so closely adjoining and overlapping each other that they have
long been known collectively as ``the great Andaman.'' The
axis of this band, almost a meadian line, is 156 statute miles
long. The five islands are in order from north to south: North
Andaman (51 m. long); Middle Andaman (59 m.); South Andaman
(49 m.); Baratang, running parallel to the east of the South
Andaman for 17 m. from the Middle Andaman; and Rutland Island (11
m.). Four narrow straits part these islands: Austin Strait,
between North and Middle Andaman; Homfray's Strait between
Middle Andaman and Baratang, and the north extremity of South
Andaman; Middle (or Andaman) Strait between Baratang and South
Andaman; and Macpherson Strait between South Andaman and Rutland
Island. Of these only the last is navigable by ocean-going
vessels. Attached to the chief islands are, on the extreme
N., Landfall Islands, separated by the navigable Cleugh
Passage; Interview Island, separated by the very narrow but
navigable Interview Passage, off the W. coast of the Middle
Andaman; the Labyrinth Island off the S.W. coast of the South
Andaman, through which is the safe navigable Elphinstone
Passage; Ritchie's (or the Andaman) Archipelago off the E.
coast of the South Andaman and Baratang, separated by the wide
and safe Diligent Strait and intersected by Kwangtung Strait
and the Tadma Juru (Strait). Little Andaman, roughly 26 m. by
16, forms the southern extremity of the whole group and lies 31
m. S. of Rutland Island across Duncan Passage, in which lie
the Cinque and other islands, forming Manners Strait, the
main commercial highway between the Andamans and the Madras
coast. Besides these are a great number of islets lying off
the shores of the main islands. The principal outlying islands
are the North Sentinel, a dangerous island of about 28 sq. m.,
lying about 18 m. off the W. coast of the South Andaman; the
remarkable marine volcano, Barren Idand (1150 ft.), quiescent
for more than a century, 71 m. N.E. of Port Blair; and the
equally curious isolated mountain, the extinct volcano of
Narcondam, rising 2330 ft. out of the sea, 71 m. E. of the North
Andaman. The land area of the Andaman Idands is 2508 sq.
m. About 18 m. to the W. of the Andamans are the dangerous
Western Banks and Dalrymple Bank, rising to within a few fathoms
of the surface of the sea and forming, with the two Sentinel
Islands, the tops of a line of submarine hills parallel to the
Andamans. Some 40 m. distant to the E. is the Invisible Bank,
with one rock just awash; and 34 m. S.E. of Narcondam is a
submarine hill rising to 377 fathoms below the surface of the
sea. Narcondam, Barren Island and the Invisible Bank, a
great danger of these seas, are in a line almost parallel
to the Andamans inclining towards them from north to south.
Topography.--The islands forming Great Andaman consist of a
mass of hills enclosing very narrow valleys, the whole covered
by an exceedingly dense tropical jungle. The hills rise,
especially on the east coast, to a considerable elevation:
the chief heights being in the North Andaman, Saddle Peak
(2400 ft.); in the Middle Andaman, Mount Diavolo behind
Cuthbert Bay (1678 ft.); in the South Andaman, Koiob (1505
ft.), Mount Harriet (1193 ft.) and the Cholunga range (1063
ft.); and in Rutland Island, Ford's Peak (1422 ft.). Little
Andaman, with the exception of the extreme north, is practically
flat. There are no rivers and few perennial streams in the
islands. The scenery is everywhere strikingly beautiful and
varied, and the coral beds of the more secluded bays in
its harbours are conspicuous for their exquisite colouring.
Harbours.--The coasts of the Andamans are deeply indented,
giving existence to a number of safe harbours and tidal creeks,
which are often surrounded by mangrove swamps. The chief
harbours, some of which are very capacious, are (starting
northwards from Port Blair, the great harbour of South
Andaman) on the E. coast: Port Meadows, Colebrooke Passage,
Elphinstone Harbour (Homfray's Strait), Stewart Sound and Port
Cornwallis. The last three are very large. On the W. coast:
Temple Sound, Interview Passage, Port Anson or Kwangtung Harbour
(large), Port Campbell (large), Port Mouat and Macpherson
Strait. There are besides many other safe anchorages about
the coast, notably Shoal Bay and Kotara Anchorage in the
South Andaman; Cadell Bay and the Turtle Islands in the
North Andaman; and Outram Harbour and Kwangtung Strait in the
archipelago. The whole of the Andamans and the outlying
islands were completely surveyed topographically by the Indian
Survey Department under Colonel Hobday in 1883-1886, and the
surrounding seas were charted by Commander Carpenter in 1888-1889.
Geology.--The Andaman Islands, in conjunction with the
other groups mentioned above, form part of a lofty range
of submarine mountains, 700 m. long, running from Cape
Negrais in the Arakan Yoma range of Burma, to Achin Head in
Sumatra. This range separates the Bay of Bengal from the
Andaman Sea; and it contains much that is geologically
characteristic of the Arakan Yoma, and formations common also
to the Nicobars and to Sumatra and the adjacent islands. The
older rocks are early Tertiary or late Cretaceous but there
are no fossils to indicate age. The newer rocks, common also
to the Nicobars and Sumatra, are in Ritchie's Archipelago
chiefly and contain radiolarians and foraminifera. There is
coral along the coasts everywhere, and the Sentinel Islands
are composed of the newer rocks with a superstructure of
coral. A theory of a still continuing subsidence of the
islanda was formed by Kurz in 1866 and confirmed by Oldham in
1884. Signs of its continuance are found on the east coast
in several places. Barren Island is a volcano of the general
Sunda group which includes also the Pegu group to which
Narcondam belongs. Barren Island was last in eruption in
1803, but there is still a thin column of steam from a
sulphur bed at the top and a variable hot spring at the
point where the last outburst of lava flowed into the sea.
Climate.--Rarely affected by a cyclone, though within
the influence of practically every one that blows in the
Bay of Bengal, the Andamans are of the greatest importance
because of the accurate information relating to the
direction and intensity of storms which can be communicated
from them better than from any other point in the bay,
to the vast amount of shipping in this part of the Indian
Ocean. Trustworthy information also regarding the weather
which may be expected in the north and east of India, is
obtained at the islands, and this proves of the utmost value
to the controllers of the great trades dependent upon the
rainfall. A well-appointed meteorological station has been
established at Port Blair since 1868. Speaking generally,
the climate of the Andamans themselves may be described as
normal for tropical islands of similar latitude. It is warm
always, but tempered by pleasant sea-breezes; very hot when
the sun is northing; irregular rainfall, but usually dry
during the north-east, and very wet during the south-west
monsoon. Not only does the rainfall at one place vary from
year to year, but there is an extraordinary difference in the
returns for places quite close to one another. The official
figures in inches for the station at Port Blair, which is
situated in by far the driest part of the settlement, were:--
_______________________________________________________________________
| 1895. | 1896. | 1897. | 1898. | 1899. | 1900. | 1901. |
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| 125.64 | 107.28 | 136.41 | 127.22 | 87.01 | 83.28 | 132.50 |
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A tidal observatory has also been maintained at Port Blair since 1880.
Flora.--A section of the Forest Department of India has
been established in the Andamans since 1883, and in the
neighbourhood of Port Blair 156 sq. m. have been set apart
for regular forest operations which are carried on by convict
labour. The chief timber of indigenous growth is padouk
(Pterocarpus dalbergioides) used for buildings, boats,
furniture, fine joinery and all purposes to which teak,
mahogany, hickory, oak and ash are applied. This tree
is widely spread and forms a valuable export to European
markets. Other first-class timbers are koko (Albizzia
lebbek), white chuglam (Terminalia bialata), black
chugiam (Myristica irya), marble or zebra wood (Diospyros
kurzii) and satin-wood (Murraya exotica), which differs
from the satin-wood of Ceylon (Chloroxylon swietenia.)
All of these timbers are used for furniture and similar
purposes. In addition there are a number of second-and
third-class timbers, which are used locally and for export to
Calcutta. Gangaw (Messua ferrea) the Assam iron-wood, is
suitable for sleepers; and didu (Bombax insigne) is used
for tea-boxes and packing-cases. Among the imported flora
are tea, Siberian coffee, cocoa, Ceara rubber (which has
not done well), Manila hemp, teak, cocoanut and a number
of ornamental trees, fruit-trees, vegetables and garden
plants. Tea is grown in considerable quantities and the
cultivation is under a department of the penal settlement.
The general character of the forests is Burmese with an
admixture of Malay types. Great mangrove swamps supply
unlimited fire-wood of the best quality. The great peculiarity
of Andaman flora is that, with the exception of the Cocos
islands, no cocoanut palms are found in the archipelago.
Fauna.--Animal life is generally deficient throughout the
Andamans, especially as regards mammalia, of which there
are only nineteen separate species in all, twelve of these
being peculiar to the islands. There is a small pig (Sus
andamanensis), important to the food of the people, and a wild
cat (Paradoxurus tytleri); but the bats (sixteen species) and
rats (thirteen species) constitute nearly three-fourths of the
known mammals. This paucity of animal life seems inconsistent
with the theory that the islands were once connected with the
mainland. Most of the birds also are derived from the distant
Indian region, while the Indo-Burmese and Indo-Malayan regions
are represented to a far less degree. Rasorial birds, such as
peafowl, junglefowl, pheasants and partridges, though well
represented in the Arakan hills, are rare in the islands; while
a third of the different species found are peculiar to the
Andamans. Moreover, the Andaman species differ from those
of the adjacent Nicobar Islands. Each group has its distinct
harrier-eagle, red-cheeked paroquet, oriole, sun- bird and
bulbul. Fish are very numerous and many species are peculiar to
the Andaman seas. Turtles are abundant and supply the Calcutta
market. Of imported animals, cattle, goats, asses and dogs
thrive well, ponies and horses indifferently, and sheep
badly, though some success has been achieved in breeding them.
Population.--The Andaman Islands, so near countries that
have for ages attained considerable civilization and have
been the seat of great empires, and close to the track of a
great commerce which has gone on at least 2000 years, are the
abode of savages as low in civilization as almost any known on
earth. Our earliest notice of them is in a remarkable
collection of early Arab notes on India and China (A.D.
851) which accurately represents the view entertained of this
people by mariners down to modern times. ``The inhabitants
of these islands eat men alive. They are black, with
woolly hair, and in their eyes and countenances there is
something quite frightful. . . . They go naked and have no
boats. If they had, they would devour all who passed near
them. Sometimes ships that are windbound and have exhausted
their provision of water, touch here and apply to the natives
for it; in such cases the crews sometimes fall into the
hands of the latter and most of them are massacred.'' The
traditional charge of cannibalism has been very persistent;
but it is entirely denied by the islanders themselves, and is
now and probably always has been untrue. Of their massacres
of shipwrecked crews, even in quite modern times, there is no
doubt, but the policy of conciliation unremittingly pursued
for the last forty years has now secured a friendly reception
for shipwrecked crews at any port of the islands except the
south and west of Little Andaman and North Sentinel Island.
The Andamanese are probably the relics of a negro race that
once inhabited the S.E. portion of Asia and its outlying
islands, representatives of which are also still to be found
in the Malay Peninsula and the Philippines. Their antiquity
and their stagnation are attested by the remains found in their
kitchen-middens. These are of great age, and rise sometimes to
a height exceeding 15 ft. The fossil shells, pottery and rude
stone implements, found alike at the base and at the surface
of these middens, prove that the habits of the islanders have
not varied since a remote past, and lead to the belief that
the Andamans were settled by their present inhabitants some
time during the Pleistocene period, and certainly no later
than the Neolithic age. The population is not susceptible
of accurate computation, but probably it has always been
small. The estimated total at a census taken in 1901 was
only 2000. Though all descended from one stock, there are
twelve distinct tribes of the Andamanese, each with its own
clearly-defined locality, its own distinct variety of the one
fundamental language and to a certain extent its own separate
habits. Every tribe is divided into septs fairly well
defined. The tribal feeling may be expressed as friendly within
the tribe, courteous to other Andamanese if known, hostile
to every stranger, Andamanese or other. Another division
of the natives is into Aryauto or long-shore-men, and the
Eremtaga or jungle-dwellers. The habits and capacities of
these two differ, owing to surroundings, irrespectively of
tribe. Yet again the Andamanese can be grouped according to
certain salient characteristics: the forms of the bows and
arrows, of the canoes, of ornaments and utensils, of tattooing
and of language. The average height of males is 4 ft. 10 1/2
in.; of females, 4 ft. 6 in. Being accustomed to gratify
every sensation as it arises, they endure thirst, hunger,
want of food and bodily discomfort badly. The skin varies in
colour from an intense sheeny black to a reddish-blown on the
collar-bones, cheeks and other parts of the body. The hair
varies from a sooty black to dark and light brown and red. It
grows in small rings, which give it the appearance of growing
in tufts, though it is really closely and evenly distributed
over the whole scalp. The figures of the men are muscular and
well-formed and generally pleasing; a straight, well-formed
nose and jaw are by no means rare, and the young men are often
distinctly good-looking. The only artificial deformity is
a depression of the skull, chiefly among one of the southern
tribes, caused by the pressure of a strap used for carrying
loads. The pleasing appearance natural to the men is not
a characteristic of the women, who early have a tendency to
stoutness and ungainliness of figure, and sometimes to pronounced
prognathism. They are, however, always bright and merry, are
under no special social restrictions and have considerable
influence. The women's heads are shaved entirely and the
men's into fantastic patterns. Yellow and red ochre mixed
with grease are coarsely smeared over the bodies, grey in
coarse patterns and white in fine patterns resembling tattoo
marks. Tattooing is of two distinct varieties. In the south
the body is slightly cut by women with small flakes of glass
or quartz in zigzag or lineal patterns downwards. In the north
it is deeply cut by men with pig-arrows in lines across the
body. The male matures when about fifteen years of age,
marries when about twenty-six, begins to age when about
forty, and lives onto sixty or sixty-five if he reaches old
age. Except as to the marrying age, these figures fairly
apply to women. Before marriage free intercourse between the
sexes is the rule, though certain conventional precautions
are taken to prevent it. Marriages rarely produce more
than three children and often none at all. Divorce is rare,
unfaithfulness after marriage not common and incest unknown.
By preference the Andamanese are exogamous as regards sept
and endogamous as regards tribe. The children are possessed
of a bright intelligence, which, however, soon reaches its
climax, and the adult may be compared in this respect with
the civilized child of ten or twelve. The Andamanese are,
indeed, bright and merry companions, busy in their own pursuits,
keen sportsmen, naturally independent and not lustful, but
when angered, cruel, jealous, treacherous and vindictive,
and always unstable--in fact, a people to like but not to
trust. There is no idea of government, but in each sept
there is a head, who has attained that position by degrees on
account of some tacitly admitted superiority and commands a
limited respect and some obedience. The young are deferential
to their elders. Offences are punished by the aggrieved
party. Property is communal and theft is only recognized as to
things of absolute necessity, such as arrows, pigs' flesh and
fire. Fire is the one thing they are really careful about,
not knowing how to renew it. A very rude barter exists between
tribes of the same group in regard to articles not locally
obtainable. The religion consists of fear of the spirits of the
wood, the sea, disease and ancestors, and of avoidance of acts
traditionally displeasing to them. There is neither worship
nor propitiation. An anthropomorphic deity, Puluga, is the
cause of all things, but it is not necessary to propitiate
him. There is a vague idea that the ``soul'' will go somewhere
after death, but there is no heaven nor hell, nor idea of
a corporeal resurrection. There is much faith in dreams,
and in the utterances of certain ``wise men,'' who practise
an embryonic magic and witchcraft. The great amusement of
the Andamanese is a formal night dance, but they are also
fond of simple games. The bows differ altogether with each
group, but the same two kinds of arrows are in general use:
(1) long and ordinary for fishing and other purposes; (2)
short with a detachable head fastened to the shaft by a thong,
which quickly brings pigs up short when shot in the thick
jungle. Bark provides material for string, while baskets and
mats are neatly and stoutly made from canes and buckets out
of bamboo and wood. None of the tribes ever ventures out of
sight of land, and they have no idea of steering by sun or
stars. Their canoes are simply hollowed out of trunks with the
adze and in no other way, and it is the smaller ones which are
outrigged; they do not last long and are not good sea-boats,
and the story of raids on Car Nicobar, out of sight across a
stormy and sea-rippled channel, must be discredited. Honour
is shown to an adult when he dies, by wrapping him in a cloth
and placing him on a platform in a tree instead of burying
him. At such a time the encampment is deserted for three
months. The Andaman languages are extremely interesting
from the philological standpoint. They are agglutinative in
nature, show hardly any signs of syntactical growth though
every indication of long etymological growth, give expression
to only the most direct and the simplest thought, and are purely
colloquial and wanting in the modifications always necessary
for communication by writing. The sense is largely eked out by
manner and action. Mincopie is the first word in Colebrooke's
vocabulary for ``Andaman Island, or native country,'' and
the term--though probably a mishearing on Colebrooke's part
for Mongebe (``I am an Onge,'' i.e. a member of the
Onge tribe)--has thus become a persistent book-name for the
people. Attempts to civilize the Andamanese have met with
little success either among adults or children. The home
established near Port Blair is used as a sort of free asylum
which the native visits according to his pleasure. The
policy of the government is to leave the Andamanese alone,
while doing what is possible to ameliorate their condition.
Penal Setllement.--The point of enduring interest as regards
the Andamans is the penal system, the object of which is to turn
the life-sentence and few long-sentence convicts, who alone are
sent to the settlement, into honest, self-respecting men and
women, by leading them along a continuous course of practice
in self-help and self-restraint, and by offering them every
inducement to take advantage of that practice. After ten years'
graduated labour the convict is given a ticket-of-leave and
becomes self-supporting. He can farm, keep cattle, and marry
or send for his family, but he cannot leave the settlement or be
idle. With approved conduct, however, he may be absolutely
released after twenty to twenty-five years in the settlement;
and throughout that time, though possessing no civil rights,
a quasi-judicial procedure controls all punishments inflicted
upon him, and he is as secure of obtaining justice as if
free. There is an unlimited variety of work for the labouring
convicts, and some of the establishments are on a large
scale. Very few experts are employed in supervision;
practically everything is directed by the officials, who
themselves have first to learn each trade. Under the chief
commissioner, who is the supreme head of the settlement,
are a deputy and a staff of assistant superintendents and
overseers, almost all Europeans, and sub-overseers, who are
natives of India. All the petty supervising establishments
are composed of convicts. The garrison consists of 140
British and 300 Indian troops, with a few local European
volunteers. The police are organized as a military battalion
643 strong. The number of convicts has somewhat diminished
of late years and in 1901 stood at 11,947. The total
population of the settlement, consisting of convicts, their
guards, the supervising, clerical and departmental staff,
with the families of the latter, also a certain number of
ex-convicts and trading settlers and their families, numbered
16,106. The labouring convicts are distributed among four
jails and nineteen stations; the self-supporters in thirty-eight
villages. The elementary education of the convicts' children
is compulsory. There are four hospitals, each under a
resident medical officer, under the general supervision of
a senior officer of the Indian medical service, and medical
aid is given free to the whole population. The net annual
cost of the settlement to the government is about L. 6 per
convict. The harbour of Port Blair is well supplied with
buoys and harbour lights, and is crossed by ferries at fixed
intervals, while there are several launches for hauling local
traffic. On Ross Island there is a lighthouse visible for 19
m. A complete system of signalling by night and day on
the Morse system is worked by the police. Local posts are
frequent, but there is no telegraph and the mails are irregular.
History.--It is uncertain whether any of the names of the
islands given by Ptolemy ought to be attached to the Andamans;
yet it is probable that his name itself is traceable in the
Alexandrian geographer. Andaman first appears distinctly
in the Arab notices of the 9th century, already quoted. But
it seems possible that the tradition of marine nomenclature
had never perished; that the 'Agathou daimonos nesos
was really a misunderstanding of some form like Agdaman,
while Nesoi Baroussai survived as Lanka Balus, the
name applied by the Arabs to the Nicobars. The islands
are briefly noticed by Marco Polo, who probably saw without
visiting them, under the name Angamanain, seemingly an
Arabic dual, ``The two Angamans,'' with the exaggerated
but not unnatural picture of the natives, long current,
as dog-faced Anthropophagi. Another notice occurs in the
story of Nicolo Conti (c. 1440), who explains the name to
mean ``Island of Gold,'' and speaks of a lake with peculiar
virtues as existing in it. The name is probably derived
from the Malay Handuman, coming from the ancient Hanuman
(monkey). Later travellers repeat the stories, too well
founded, of the ferocious hostility of the people; of whom we
may instance Cesare Federici (1569), whose narrative is given
in Ramusio, vol. iii. (only in the later editions), and in
Purchas. A good deal is also told of them in the vulgar and
gossiping but useful work of Captain A. Hamilton (1727).
In 1788-1789 the government of Bengal sought to establish
in the Andamans a penal colony, associated with a harbour of
refuge. Two able officers, Colebrooke of the Bengal Engineers,
and Blair of the sea service, were sent to survey and
report. In the sequel the settlement was established by Captain
Blair, in September 1789, on Chatham Island, in the S.E. bay
of the Great Andaman, now called Port Blair, but then Port
Cornwallis. There was much sickness, and after two years,
urged by Admiral Cornwallis, the government transferred
the colony to the N.E. part of Great Andaman, where a naval
arsenal was to be established. With the colony the name also
of Port Cornwallis was transferred to this new locality.
The scheme did ill; and in 1796 the government put an end to
it, owing to the great mortality and the embarrassments of
maintenance. The settlers were finally removed in May
1796. In 1824 Port Cornwallis was the rendezvous of the fleet
carrying the army to the first Burmese war. In 1839, Dr Helfer,
a German savant employed by the Indian government, having
landed in the islands, was attacked and killed. In 1844 the
troop-ships ``Briton'' and ``Runnymede'' were driven ashore
here, almost close together. The natives showed their usual
hostility, killing all stragglers. Outrages on shipwrecked
crews continued so rife that the question of occupation had
to be taken up again; and in 1855 a project was formed for
such a settlement, embracing a convict establishment. This
was interrupted by the Indian Mutiny of 1857, but as soon
as the neck of that revolt was broken, it became more urgent
than ever to provide such a resource, on account of the great
number of prisoners falling into British hands. Lord Canning,
therefore, in November 1857, sent a commission, headed by
Dr F. Mouat, to examine and report. The commission reported
favourably, selecting as a site Blair's original Port
Cornwallis, but pointing out and avoiding the vicinity of a
salt swamp which seemed to have been pernicious to the old
colony. To avoid confusion, the name of Port Blair was given
to the new settlement, which was established in the beginning of
1858. For some time sickness and mortality were excessively
large, but the reclamation of swamp and clearance of jungle
on an extensive scale by Colonel Henry Man when in charge
(1868-1870), had a most beneficial effect, and the health of
the settlement has since been notable. The Andaman colony
obtained a tragical notoriety from the murder of the viceroy,
the earl of Mayo, by a Mahommedan convict, when on a visit
to the settlement on the 8th of February 1872. In the same
year the two groups, Andaman and Nicobar, the occupation of
the latter also having been forced on the British government
(in 1869) by the continuance of outrage upon vessels, were
united under a chief commissioner residing at Port Blair.
See Sir Richard Temple, The Andaman and Nicobar Islands
(Indian Census, 1901); C. B. Kloss, In the Andamans and
Nicobars (1903); E. H. Man, Aboriginal Inhabitants of
the Andaman Islands (1883); M. V. Portman, Record of the
Andamanese (11 volumes MS. in India Office, London, and
Home Department, Calcutta), 1893- 1898, Andamanese Monual
(1887), Notes on the Languages of the South Andaman Group
of Tribes (1898), and History of our Relations with
the Andamanese (1899); S. Kurz, Vegetation of the Andamans
(1867); G. S. Miller, Mammals of the Andaman and Nicobar
Islands (vol. xxiv. of the Proceedings of the National
Museum, U.S.A.); A. L. Butler, ``Birds of the Andamans and
Nicobars'' (Proc. Bombay Nat. Hist. Soc., vols. xii. and
xiii.); and A. Alcock, A Naturalist in Indian Seas (1902).
ANDANTE (Ital. for ``moving slowly,'' from andare, to
go), a musical term to indicate pace, coming between adagio
and allegro; it is also used of an independent piece of
music or of the slow movement in a sonata, symphony, &c.
ANDERIDA, an ancient Roman fort at Pevensey, near Eastbourne
in Sussex (England), built about A.D. 300 as part of a scheme
of land-defence against the Saxon pirates; repaired, probably
by the great Stilicho, about A.D. 400; and after the Norman
Conquest utilized by William the Conqueror for a Norman castle.
Its massive Roman enceinte still stands but little damaged.
ANDERNACH, a town of Germany, in the Prussian Rhine province,
on the left bank of the Rhine, 10 m. N.W. of Coblenz by
the main line to Cologne. Pop. (1900) 7889. Viewed from
the river it makes a somewhat gloomy, though picturesque,
impression, with its parish church (a basilica dating from
the 12th century, with four towers), the round watch-tower
on the Rhine, old walls in places 15 ft. thick, and a famous
crane (erected 1554) for lading merchandise. Among other
buildings are a Gothic Minorite church (now Protestant), a town
hall, and a prison, formerly the castle of the archbishops of
Cologne. Andernach has considerable industries, brewing and
manufactures of chemicals and perfumes, and has also a trade
in corn and wine. But its most notable article of commerce
is that of mill-stones, made of lava and tufa-stone, a product
much used by the Dutch in the construction of their dykes.
Andernach (Antunnacum) is the old Roman Castellum ante
Nacum, founded by Drusus and fortified in the 3rd century
A.D. In 1109 Andernach received civic rights, passed in 1167
to the electors of Cologne, in 1253 joined the confederation
of the Rhine cities and was the most southern member of the
Hanseatic league. Here in 1474 a treaty was signed between
the emperor Frederick III., the four electors of the Rhine and
France. In 1794 Andernach passed to France, but in 1815 was
ceded, together with the left bank of the Rhine, to Prussia.
ANDERSEN, HANS CHRISTIAN (1805-1875), Danish poet and
fabulist, was born at Odense, in Funen, on the 2nd of April
1805. He was the son of a sickly young shoemaker of
twenty-two, and his still younger wife: the whole family lived
and slept in one little room. Andersen very early showed
signs of imaginative temperament, which was fostered by the
indulgence and superstition of his parents. In 1816 the
shoe-maker died and the child was left entirely to his own
devices. He ceased to go to school; he built himself a little
toy-theatre and sat at home making clothes for his puppets,
and reading all the plays that he could borrow; among them
were those of Holberg and Shakespeare. At Easter 1819 he
was confirmed at the church of St Kund, Odense, and began to
turn his thoughts to the future. It was thought that he was
best fitted to be a tailor; but as nothing was settled, and
as Andersen wished to be an opera-singer, he took matters
into his own hand and started for Copenhagen in September
1819. There he was taken for a lunatic, snubbed at the theatres,
and nearly reduced to starvation, but he was befriended by
the musicians Christoph Weyse and Siboni, and afterwards by
the poet Frederik Hoegh Guldberg (1771-1852). His voice
failed, but he was admitted as a dancing pupil at the Royal
Theatre. He grew idle, and lost the favour of Guldberg,
but a new patron appeared in the person of Jonas Collin, the
director of the Royal Theatre, who became Andersen's life-long
friend. King Frederick VI. was interested in the strange
boy and sent him for some years, free of charge, to the great
grammar-school at Slagelse. Before he started for school he
published his first volume, The Ghost at Palnatoke's Grave
(1822). Andersen, a very backward and unwilling pupil, actually
remained at Slagelse and at another school in Elsinore until
1827; these years, he says, were the darkest and bitterest in his
life. Collin at length consented to consider him educated, and
Andersen came to Copenhagen. In 1829 he made a considerable
success with a fantastic volume entitled A Journey on Foot
from Holman's Canal to the East Point of Amager, and he
published in the same season a farce and a book of poems. He
thus suddenly came into request at the moment when his friends
had decided that no good thing would ever come out of his early
eccentricity and vivacity. He made little further progress,
however, until 1833, when he received a small travelling
stipend from the king, and made the first of his long European
journeys. At Le Locle, in the Jura, he wrote Agnate and
the Merman; and in October 1834 he arrived in Rome. Early
in 1835 Andersen's novel, The Improvisatore, appeared, and
achieved a real success; the poet's troubles were at an end at
last. In the same year, 1835, the earliest instalment of
Andersen's immortal Fairy Tales (Eventyr) was published in
Copenhagen. Other parts, completing the first volume, appeared
in 1836 and 1837. The value of these stories was not at first
perceived, and they sold slowly. Andersen was more successful
for the time being with a novel, O.T., and a volume of
sketches, In Sweden; in 1837 he produced the best of his
romances, Only a Fiddler. He now turned his attention,
with but ephemeral success, to the theatre, but was recalled
to his true genius in the charming miscellanies of 1840 and
1842, the Picture-Book without Pictures, and A Poet's
Bazaar. Meanwhile the fame of his Fairy Tales had been
steadily rising; a second series began in 1838, a third in
1845. Andersen was now celebrated throughout Europe, although
in Denmark itself there was still some resistance to his
pretensions. In June 1847 he paid his first visit to
England, and enjoyed a triumphal social success; when he
left, Charles Dickens saw him off from Ramsgate pier. After
this Andersen continued to publish much; he still desired to
excel as a novelist and a dramatist, which he could not do,
and he still disdained the enchanting Fairy Tales, in the
composition of which his unique genius lay. Nevertheless he
continued to write them, and in 1847 and 1848 two fresh volumes
appeared. After a long silence Andersen published in 1857
another romance, To be or not to be. In 1863, after a
very interesting journey, he issued one of the best of his
travel-books, In Spain. His Fairy Tales continued to
appear, in instalments, until 1872, when, at Christmas, the
last stories were published. In the spring of that year
Andersen had an awkward accident, falling out of bed and
severely hurting himself. He was never again quite well,
but he lived till the 4th of August 1875, when he died very
peacefully in the house called Rolighed, near Copenhagen. (E. G.)
ANDERSON, ADAM (1692--1765), Scottish economist, was born in
1692, and died in London on the 10th of January 1765. He was a
clerk for forty years in the South Sea House, where he published
a work entitled Historical and Chronological Deduction
of the Origin of Commerce from the Earliest Accounts to the
Present Time, containing a History of the Great Commercial
Interests of the British Empire (1762, 2 vols. fol.).
ANDERSON, ALEXANDER (c. 1582-1620?), Scottish mathematician,
was born at Aberdeen. In his youth he went to the continent
and taught mathematics at Paris, where he published or
edited, between the years 1612 and 1619, various geometrical
and algebraical tracts, which are conspicuous for their
ingenuity and elegance. He was selected by the executors of
Franciscus Vieta to revise and edit his manuscript works, a
task which he discharged with great ability. The works of
Anderson amount to six thin 4to volumes, and as the last of
them was published in 1619, it is probable that the author
died soon after that year, but the precise date is unknown.
ANDERSON, SIR EDMUND (1530-1605), English lawyer, descended
from a Scottish family settled in Lincolnshire, was born
in 1530 at Flixborough or Broughton in that county. After
studying for a short time at Lincoln College, Oxford, he
became in 1550 a student of the Inner Temple. In 1579 he
was appointed serjeant-at-law to Queen Elizabeth, and also
an assistant judge on circuit. As a reward for his services
in the trial of Edmund Campian and his followers (1581), he
was, on the death of Sir James Dyer, appointed lord chief
justice of the Common Pleas (1582), and was knighted. He
took part in all the leading state trials which agitated
England during the latter years of Elizabeth's reign. Though
a great lawyer and thoroughly impartial in civil cases, he
became notorious by his excessive severity and harshness when
presiding over the trials of catholics and nonconformists; more
markedly so in those of Sir John Perrot, Sir Walter Raleigh,
and John Udall the puritan minister. Anderson was also one
of the commissioners appointed to try Mary queen of Scots in
1586. He died on the 1st of August 1605 at Eyworth in
Bedfordshire. In addition to Reports of Many Principal
Cases Argued and Adjudged in the Time of Queen Elizabeth
in the Common Bench, published after his death, he drew
up several expositions of statutes enacted in Elizabeth's
reign which remain in manuscript in the British Museum.
ANDERSON, ELIZABETH GARRETT (1836- ), English medical
practitioner, daughter of Newson Garrett, of Aldeburgh,
Suffolk, was born in 1836, and educated at home and at a private
school. In 1860 she resolved to study medicine, an unheard-of
thing for a woman in those days, and one which was regarded
by old-fashioned people as almost indecent. Miss Garrett
managed to obtain some more or less irregular instruction at
the Middlesex hospital, London, but was refused admission as a
full student both there and at many other schools to which she
applied. Finally she studied anatomy privately at the London
hospital, and with some of the professors at St Andrews
University, and at the Edinburgh Extra-Mural school. She
had no less difficulty in gaining a qualifying diploma to
practise medicine. London University, the Royal Colleges
of Physicians and Surgeons, and many other examining bodies
refused to admit her to their examinations; but in the end
the Society of Apothecaries, London, allowed her to enter
for the License of Apothecaries' Hall, which she obtained in
1865. In 1866 she was appointed general medical attendant to
St Mary's dispensary, a London institution started to enable
poor women to obtain medical help from qualified practitioners
of their own sex. The dispensary soon developed into the
New hospital for women, and there she worked for over twenty
years. In 1870 she obtained the Paris degree of M.D. The
same year she was elected to the first London School Board,
at the head of the poll for Marylebone, and was also made one
of the visiting physicians of the East London hospital for
children; but the duties of these two positions she found to
be incompatible with her principal work, and she soon resigned
them. In 1871 she married Mr J. G. S. Anderson (d. 1907), a
London shipowner, but did not give up practice. She worked
steadily at the development of the New hospital, and (from
1874) at the creation of a complete school of medicine in
London for women. Both institutions have since been handsomely
and suitably housed and equipped, the New hospital (in the
Euston Road) being worked entirely by medical women, and the
schools (in Hunter Street, W.C.) having over 200 students,
most of them preparing for the medical degree of London
University, which was opened to women in 1877. In 1897 Mrs
Garrett Anderson was elected president of the East Anglian
branch of the British Medical Association. In 1908 she was
elected (the first lady) mayor of Aldeburgh. The movement
for the admission of women to the medical profession, of
which she was the indefatigable pioneer in England, has
extended to every civilized country except Spain and Turkey.
ANDERSON, JAMES (1662-1728), Scottish genealogist, antiquary
and historian, was born at Edinburgh on the 5th of August
1662. He was educated for the law, and became a writer to
the signet in 1691. His profession gave him the opportunity
of gratifying his taste for the study of ancient documents;
and just before the union the Scottish parliament commissioned
him to prepare for publication what remained of the public
records of the kingdom, and in their last session voted a sum
of L. 1940 sterling to defray his expenses. At this work he
laboured for several years with great judgment and perseverance;
but it was not completed at his death in 1728. The book was
published posthumously in 1739, edited by Thomas Ruddiman,
under the title Selectus Diplomatum et Numismatum Scotiae
Thesaurus. The preparation of this great national work involved
the author in considerable pecuniary loss; and soon after his
death, the numerous plates, engraved by Sturt, were sold for
L. 530. These plates are now lost, and the book has become
exceedingly scarce. After the union of the crowns, Anderson
was appointed in 1715 postmaster-general for Scotland, as
some compensation for his labours; but in the political
struggles of 1717 he was deprived of this office, and never
again obtained any reward for his services. He died on the
3rd of April 1728. He published, during the controversy
about the union, An Historical Essay showing that the Crown
and Kingdom of Scotland is Imperial and Independent (Edin.,
1705,), and later Collections relating to the History of
Mary Queen of Scotland (in 4 vols., Edin., 1727-1728).
ANDERSON, JAMES (1739-1808), Scottish agriculturist and
economist, was born at Hermiston, near Edinburgh, in
1739. While still a boy he undertook the working of a farm
in Mid- Lothian which his family had occupied for several
generations, and later he rented in Aberdeenshire a farm
of 1300 acres of unimproved land. In 1783 he settled in
Edinburgh, where in 1791 he projected a weekly publication
called The Bee, which was largely written by himself, and
of which eighteen volumes were published. In 1797 he began
to reside at Isleworth, and from 1799 to 1802 he produced
a monthly publication, Recreations in Agriculture,
Natural History, Arts and Miscellaneous Literature. He
was also the author of many pamphlets on agricultural and
economical topics. He died on the 15th of October 1808.
ANDERSON, JOHN (1726-1796), Scottish natural philosopher,
was born at Roseneath, Dumbartonshire, in 1726. In 1756 he
became professor of oriental languages in the university of
Glasgow, where he had finished his education; and in 1760
he was appointed to the more congenial post of professor of
natural philosophy. He devoted himself particularly to the
application of science to industry, instituting courses of
lectures intended especially for artisans, and he bequeathed
his property for the foundation of an institution for
the furtherance of technical and scientific education in
Glasgow, Anderson's College, now merged in the Glasgow and
West of Scotland Technical College. He died in Glasgow on
the 13th of January 1796. His Institutes of Physics,
published in 1786, went through five editions in ten years.
ANDERSON, MARY (1859- ), American actress, was born at
Sacramento, California, on the 28th of July 1859. Her father,
an officer in the Confederate service in the Civil War, died in
1863. She was educated in various Roman Catholic institutions,
and at the age of thirteen, with the advice of Charlotte
Cushman, began to study for the stage, making her first
appearance at Louisville, Kentucky, as Juliet in 1875. Her
remarkable beauty created an immediate success, and she played
in all the large cities of the United States with increasing
popularity. Between 1883 and 1889 she had several seasons in
London, and was the Rosalind in the performance of As You
Like It which opened the Shakespeare Memorial theatre at
Stratford-on-Avon. Among her chief parts were Galatea (in W.
S. Gilbert's Pygmalion and Galatea), Clarice (in his Comedy
and Tragedy, written for her), Hermione, Perdita, and Julia
(in The Hunchback.) In 1889 she retired from the stage and
in 1890 married Antonio de Navarro, and settled in England.
See William Winter's Stage Life of Mary Anderson (New
York, 1886), and her own A Few Momories (New York, 1896).
ANDERSON, RICHARD HENRY (1821-1879), American soldier, was
born in South Carolina on the 7th of October 1821. Graduating
at West Point in 1842, he served in the Mexican War (in which
he won the brevet of first lieutenant) and in the Kansas
troubles of 1856-1857, becoming first lieutenant in 1848 and
captain in 1855. At the outbreak of the Civil War in 1861
he resigned his commission in the U.S. army, and entered the
Confederate service as a brigadier-general, being promoted
major-general in August 1862 and lieutenant-general in May
1864. With the exception of a few months spent with the army
under Bragg in 1862, Anderson's service was wholly in the Army
of Northern Virginia. Under Lee and Longstreet he served as
a divisional commander in nearly every battle from 1862 to
1864, winning especial distinction at Chancellorsville and
Gettysburg. When Longstreet was wounded at the battle of
the Wilderness, Anderson succeeded him in command of the
1st corps, which he led in the subsequent battles. His
services at the battle of Spottsylvania (q.v.) were most
important. He remained with the army, as a corps commander,
to the close of the war, after which he retired into private
life. He died at Beaufort S.C. on the 26th of June 1879.
ANDERSON, ROBERT (1750-1830), Scottish author and critic,
was born at Carnwath, Lanarkshire, on the 7th of January
1750. He studied first divinity and then medicine at the
university of Edinburgh, and subsequently, after some experience
as a surgeon, took the degree of M.D. at St Andrews in 1778.
He began to practise as a physician at Alnwick, but he became
financially independent by his marriage with the daughter of Mr
John Gray, and abandoned his profession for a literary life in
Edinburgh. For several years his attention was occupied
with his edition of The Works of the British Poets, with
Prefaces Biographical and Critical (14 vols. 8vo, Edin.,
1792-1807). His other publications were, The Miscellaneous
Works of Tobias Smollett, M.D., with Memoirs of his Life
and Writings (Edin., 1796); Life of Samuel Johnson, LL.D.,
with Critical Observations on his Works (Edin., 1815);
The Works of John Moore, M.D., with Memoirs of his Life
and Writings (Edin., 7 vols., 1820); and The Grave and other
Poems, by Robert Blair; to which are prefixed some Account
of his Life and Observations on his Writings (Edin., 1826).
Dr Anderson died at Edinburgh on the 20th of February 1830.
ANDERSON, a city and the county-seat of Madison county, Indiana,
U.S.A., situated on the west fork of the White river, about 35
m. N.E. of Indianapolis. Pop. (1880) 4126; (1890) 10,741;
(1900) 20,178, of whom 1081 were foreign-born; (1910, census)
22,476. It is served by the Central Indiana, the Cleveland,
Cincinnati, Chicago & St Louis, and the Pittsburg, Chicago & St
Louis railways, and also by the Indiana Union Traction System
(electric), the general offices and central power plant of
which are situated there. Its importance as a manufacturing
centre is due to its location in the natural gas region. In
1905 Anderson ranked first among the cities of the state in
the manufacture of carriage and wagon material, and iron and
steel. Among its many other manufactures are glass and
glassware, paper, strawboards, crockery and tiles. In 1905
the total factory product was valued at $8,314,760. There is a
good public library; much attention has been devoted to public
improvements; and the water works and the electric lighting
plants are owned and operated by the city. In connexion
with the water works there is a good filtration plant.
First settled about 1822, Anderson was incorporated in 1865.
ANDERSONVILLE, a village of Sumter county, Georgia, U.S.A.,
in the S.W. part of the state, about 60 m. S.W. of Macon,
on the Central of Georgia railway. Pop. (1910) 174. From
November 1863 until the close of the Civil War it was the seat
of a Confederate military prison. A tract of 16 1/2 acres of
land near the village was cleared of trees and enclosed with a
stockade. Prisoners began to arrive in February 1864, before
the prison was completed and before adequate supplies had
been received, and in May their number amounted to about
12,000. In June the stockade was enlarged so as to include
26 1/2 acres, but the congestion was only temporarily relieved,
and in August the number of prisoners exceeded 32,000. No
shelter had been provided for the inmates: the first arrivals
made rude sheds from the debris of the stockade; the others
made tents of blankets and other available pieces of cloth,
or dug pits in the ground. Owing to the slender resources
of the Confederacy, the prison was frequently short of
food, and even when this was sufficient in quantity it was
of a poor quality and poorly prepared on account of the lack
of cooking utensils. The water supply, deemed ample when
the prison was planned, became polluted under the congested
conditions. During the summer of 1864 the prisoners
suffered greatly from hunger, exposure and disease, and in
seven months about a third of them died. In the autumn,
after the capture of Atlanta, all the prisoners who could
be moved were sent to Millen, Georgia and Florence, South
Carolina. At Millen better arrangements prevailed, and when,
after Sherman began his march to the sea, the prisoners were
returned to Andersonville, the conditions there were somewhat
improved. During the war 49,485 prisoners were received at
the Andersonville prison, and of these about 13,000 died.
The terrible conditions obtaining there were due to the lack
of food supplies in the Confederate States, the incompetence
of the prison officials, and the refusal of the Federal
authorities in 1864 to make exchanges of prisoners, thus filling
the stockade with unlooked-for numbers. After the war Henry
Wirz, the superintendent, was tried by a court-martial, and
on the 10th of November 1865 was hanged, and the revelation
of the sufferings of the prisoners was one of the factors
that shaped public opinion regarding the South in the Northern
states, after the close of the Civil War. The prisoners' burial
ground at Andersonville has been made a national cemetery, and
contains 13,714 graves of which 921 are marked ``unknown.''
There is an impartial account of the Andersonville prison
in James F. Rhodes, History of the United States (vol.
v., New York, 1904). The partisan accounts are numerous;
see, for instance, A. C. Hamlin, Martyria; or, Andersonville
Prison (Boston, 1866); and R. R. Stevenson, The Southern
Side; or, Andersonville Prison (Baltimore, 1876).
ANDES, a vast mountain system forming a continuous chain
of highland along the western coast of South America. It is
roughly 4400 m. long, 100 m. wide in some parts, and of an
average height of 13,000 ft.1 The connexion of this system
with that of the Rocky Mountains, which has been pointed out
by many writers, has received much support from the discovery
of the extensive eruptions of granite during Tertiary times,
extending from the southern extremity of South America to
Alaska. The Andean range is composed of two great principal
chains with a deep intermediate depression, in which, and at
the sides of the great chains, arise other chains of minor
importance, the chief of which is that called the Cordillera
de la Costa of Chile. This starts from the southern extremity
of the continent, and runs in a northerly direction, parallel
with the coast, being broken up at its beginning into a number
of islands, and afterwards forming the western boundary of
the great central valley of Chile. To the north this coastal
chain continues in small ridges or isolated hills along the
Pacific as far as Colombia, always leaving the same valley
more or less visible to the west of the western great chain.
Tierra del Fuego.
Of the two principal chains the eastern is generally called Los
Andes, and the western La Cordillera, in Colombia, Peru and
Bolivia, where the eastern is likewise known as Cordillera Real
de los Andes, while to the south of parallel 23 deg. S. lat. in
Chile and Argentina, the western is called Cordillera de los
Andes. The eastern disappears in the centre of Argentina,
and it is therefore only the Cordillera de los Andes that
is prolonged as far as the south-eastern extremity of the
continent. The Cordillera de la Costa begins near Cape
Horn, which is composed principally of crystalline rocks,
and its heights are inconsiderable when compared with
those of the true Cordillera of the Andes. The latter,
as regards its main chain, is on the northern coast of the
Beagle Channel, in Tierra del Fuego, bounded on the north
by the deep depression of Lake Fagnano and of Admiralty
Sound. Staten Island appears to be the termination to the
east. The Cordillera of the Andes in Tierra del Fuego is
formed of crystalline schists, and culminates in the snow-capped
peaks of Mount Darwin and Mount Sarmiento (7200 ft.), which
contains glaciers of greater extent than those of Mont
Blanc. The extent of the glaciers is considerable in this
region, which, geographically, is more complex than was formerly
supposed. Although, in the explored portion of the Fuegian
chain, the volcanoes which have been mentioned from time to
time have not been met with, there seem to have existed to the
south, on the islands, many neo-volcanic rocks, some of which
appear to be contemporaneous with the basaltic sheet that covers
a part of eastern Patagonia. The insular region between Mount
Sarmiento and the Cordillera de los Andes, properly so called,
i.e. that which extends from Magellan Strait northwards, is
not fully explored, and all that is known of it is that it is
principally composed of the same rocks as the Fuegian section,
and that the greater part of its upper valleys is occupied
by glaciers that reach down to the sea amid dense forest.
Chile-Argentina, 52 deg. -38 deg. S.
As Admiralty Sound and Lake Fagnano bound the Cordillera to
the north in Tierra del Fuego, so at the eastern side of the
Cordillera in the southernmost part of the continent there is
a longitudinal depression which separates the Andes from some
independent ridges pertaining to a secondary parallel broken
chain called the pre-Cordillera. This depression is occupied
in great part by a series of lakes, some of these filling
transversal breaches in the range, whilst others are remains
of glacial reservoirs, bordered by morainic dams, extending
as far as the eastern tableland and corresponding in these
cases with transversal depressions which reach the Atlantic
Ocean. Between the larger lakes, fed by the Andine glaciers
of the eastern slope of the Southern Andes, are Lakes
Maravilla, 100 sq. m., and Sarmiento, 26 sq. m., 51 deg. S.
lat., which overflow into Last Hope Inlet; Argentino, 570 sq.
m., 50 deg. S. lat.; and Viedma, 450 sq; m., 49 deg. 30' S. lat.,
which empty into the river Santa Cruz; the fjordian Lake San
Martin, 49 deg. S. lat;, and Lakes Nansen, 18 sq. m.; Azara,
8 sq. m.; and Belgrano, 18 sq. m., which are dependents of
Lake San Martin (380sq. m.), and Lakes Pueyrredon (98 sq. m.)
and Buenos Aires (700 sq. m.), which now overflow into the
Pacific, through one of the remarkable inlets that are found
throughout the Cordillera, the Calen Inlet, which is the
largest western fjord of Patagonia. To the north of Lake
Buenos Aires there is Lake Elizalde, which, while situated
on the eastern slope, sends its waters to the Pacific Ocean,
and Lakes Fontana (30 sq. m.) and La Plata (34 sq. m.), 45 deg.
S. lat., which feed the river Senguerr, which flows to the
Atlantic. Lake General Paz (66 sq. m.) on the eastern slope
of the Andes, at 44 deg. S. lat., is the principal source of
the Palena river, which cuts all the Cordillera, while Lakes
Fetalauquen (20 sq. m.) Menendez (28 sq. m.), Rivadavia (10
sq. m.), and other smaller lakes, also situated between 43 deg.
30', and 42 deg. 30' S. lat. on the eastern slope send their
waters to the Pacific by the river Fetaleufu which cuts
through the Andes by a narrow gorge. The waters of Lake
Puelo (18 sq. m.) likewise flow into the same ocean through
the river of that name, which also cuts the Cordillera, and
of which the principal affluent likewise drains the waters
of a system of small lakes, the largest of which, Lake
Mascardi, measures 17 sq. m., which in comparatively recent
times formed part of the basin of Lake Nahuel Huapi (207 sq.
m.), 41 deg. S. lat. An extensive area of glacial deposits
shows that a sheet of ice formerly covered the whole eastern
slope to a great distance from the mountains. To the west
another sheet reached at the same time the Pacific Ocean.
From the Strait of Magellan up to 52 deg. S. lat., the western
slope of the Cordillera does not, properly speaking, exist.
Abrupt walls overlook the Pacific, and great longitudinal and
transversal channels and fjords run right through the heart of the
range, cutting it generally in a direction more or less oblique
to its axis, the result of movements of the earth's crust.
The mountains forming the Cordillera between Magellan Strait
and 41 deg. S. lat. are higher than those previously mentioned
in Tierra del Fuego. Generally composed of granite, gneiss
and Palaeozoic rocks, covered in many parts by rugged masses
of volcanic origin, their general height is not less than
6500 ft., while Mount Geikie is 7500 ft. and Mount Stokes
7100ft. To the north are Mounts Mayo (7600 ft.), Agassiz
(10,600 ft.), and Fitzroy, in 49 deg. S. lat. (11,120 ft.). The
section from 52 deg. to 48 deg. S. lat. is a continuous ice-capped
mountain range, and some of the glaciers extend from the
eastern lakes to the western channels, where they reach the
sea-level. The level of the lakes begins at 130 ft. at Lake
Maravilla and gradually ascends to nearly 700 ft. at Lake San
Martin. Passing the breach through which Lake San Martin
empties itself into Calen Inlet, in 48 deg. S. lat., is found a wide
oblique opening in the range, through which flows the river Las
Heras, fed by Lake Pueyrredon, which is only 410 ft. above the
sea-level to the east of the Andes, while Lake Buenos Aires,
immediately to the north, is 710 ft. The Andes continue to be
to the west an enormous rugged mass of ice and snow of an average
height of 9000 ft., sending glaciers to all the eastern fjords.
Mount San Lorenzo, detached from the main chain in the
Pre-Cordillera, is 11,800 ft. high. Mount San Valentin
(12,700 ft.) is the culminating point of the Andes in the
region extending from 49 deg. to 46 deg. S. lat., a little north of
which is the river Huemules which is followed by the breach
of the river Aisen. These two rivers have emptied a large
system of lakes, which in pre-Glacial times occupied the
eastern zone, thus forming a region suitable for colonization
in the broad valleys and hollows, where the rivers, as in
the case with those in the north, cut through the Andes by
narrow gaps, forming cataracts and rapids between the snowy
peaks. Volcanic action is still going on in these latitudes,
as the glaciers are at times covered by ashes, but the
predominant rocks to the east are the Tertiary granite,
while to the west gneiss, older granite and Palaeozoic rocks
prevail. The highest peaks, however, seem to be of volcanic
origin. Farther north, up to 41 deg. S. lat., the water gaps are
situated at a lesser distance one from the other, owing mainly
to more continuous erosion, this section of the continent
being the region of the maximum rainfall on the western
coast to the south of the equator. Between the gaps of the
river Aisen and river Cisnes or Frias, which also pierces the
chain, is found a huge mountain mass, in which is situated
Mount la Torre (7150 ft.). These form the continental
watershed, but in this region erosion is taking place so
rapidly that the day is not far distant when Lakes La Plata and
Fontana, situated to the east at a height of 3000 ft. and now
tributaries of the Atlantic, may become tributaries of the
Pacific. Already filtrations from the former go to feed
western affluents through the granitic masses. To the north
of Mount la Torre flows in the river Cisnes, 44 deg. 48' S. lat.,
across another water gap, continuing the range to the north
with high peaks, as Alto Nevado (7350 ft.) and Cacique (7000
ft.). The glaciers reach almost the western channels, as is
the case at the river Quelal. The northern glaciers, descending
nearly to sea- level, are situated at 43 deg. 40' S. lat. To
the north 45 deg. S. lat. a well-defined western longitudinal
valley, at some recent time occupied by lakes and rivers,
divides the Cordillera into two chains, the eastern being
the main chain, to which belong Mounts Alto Nevado, Cacique,
Dentista, Maldonado, Serrano, each over 7000 ft. high; and
Torrecillas (7400 ft.), Ventisquero (7500 ft.), and Tronador
(11,180 ft.); while the western chain, broken into imposing
blocks, contains several high volcanic peaks such as Mounts
Tanteles, Corcovado, Minchimahuida, Hornopiren and Yates. The
rivers Palena, with its two branches, Pico and Carrenleufu,
Fetaleufu, Puelo and Manso cut the two chains, while the rivers
Renihue, Bodadahue and Cochamo have their sources in the main
eastern ridge. Mention has been made of active volcanoes in
51 deg. , 49 deg. and 47 deg. S. lat., but these have not been properly
located. The active volcanoes south of 41 deg. , concerning
which no doubt exists, are the Huequen, in 43 deg. lat., and the
Calbuco, both of which have been in eruption in modern times.
The surroundings of Mount Tronador, consisting of Tertiary
granite and basalt, form one of the most interesting regions
in the Pataronian Andes for the mountaineers of the future. To
the east extends the large and picturesque lake of Nahuel-Huapi,
to the west is Lake Todos Los Santos (50 sq. m.), to which
the access is easy and of which the scenery is of surpassing
beauty. Between 41 deg. and 38 deg. S. lat., among other smaller
lakes, are Lakes Traful (45 sq. m.), Lacar (32 sq. m.),
which, properly belonging to the system of Atlantic lakes,
empties itself by the only water gap that occurs in this zone
of the Cordillera into the river Valdivia, a tributary of
the Pacific, Lake Lolog (15 sq. m.), Huechu-lafquen (45 sq.
m.), and Lake Alumine (21 sq. m.). The volcanoes of Lanin
(12,140 ft.), Quetropillan (9180 ft.), Villarica (10,400 ft.),
Yaimas and Tolhuaca are all more or less active; the first
is in the main chain, while the others are on the western
slope. The scenery in the neighbourhood is magnificent, the
snowy cones rising from amidst woods of araucaria, and being
surrounded by blue lakes. While the scenery of the western
slope of the Andes is exceedingly grand, with its deep fjords,
glaciers and woods, yet the severity of its climate detracts
considerably from its charm. The climate of the eastern
slope, however, is milder, the landscapes are magnificent, with
wooded valleys and beautiful lakes. The valleys are already
partly settled by colonists. Between 52 deg. and 40 deg. S. lat.
erosion has carried the watershed of the continent from the
summit of the Cordillera to the eastern plains of Patagonia.
From 40 deg. S. southward the Chile-Argentine Boundary Commission
under Sir T. H. Holdich carried out important investigations in
1902; and between 38 deg. and 33 deg. S. lat. the Andes were somewhat
extensively explored about the close of the 19th century by
Argentine and Chilean Commissions. The highest peaks in the
latter section are volcanic and their eruptions have sensibly
modified the character of the primitive ridges. Outflows
of lava and tufa cover the mountain sides and fill up the
valleys. The Jurassic and Cretaceous formations, which in
the Southern Cordillera are situated outside of the range
to the east, form to a considerable extent the mass of the
great range, together with quartz porphyry, the Tertiary,
granite and other eruptive rocks, which have been observed
along all the chain in South America up to Alaska in the
north. Gneiss is seldom met with, but there are crystalline
rocks, belonging chiefly to the pre-Cordillera of the eastern
and to the Cordillera de la Costa on the western side.
Chile-Argentina from 38 deg. S. northward.
About 38 deg. S. the Andes take a great transversal extension;
there are no wide intermediate valleys between the different
ridges but the main ridge is perfectly defined. Volcanic
cones continue to predominate, the old crystalline rocks
almost disappear, while the Mesozoic rocks are most
common. The higher peaks are in the main chain, while
the Domuyo (15,317 ft.) belongs to a lateral eastern
ridge. The principal peaks between this and Mount Tupungato
at 33 deg. S. lat. are: Mount Cochico (8255 ft.), Campanario,
(13,140 ft.), Peteroa (13,297 ft.), Tinguiririca, Castillo
(16,535 ft.), Volcano Maipu (17,576 ft.), Alvarado (14,600
ft.), Amarillo (15,321 ft.), Volcano San Jose (19,849 ft.),
Piuquenes (17,815 ft.), and Volcano Bravard (19,619 ft.).
North of Maipu volcano, ascended by R. P. Gussfeldt in
1883, the Cordillera is composed of two huge principal ridges
which unite and terminate in the neighbourhood of Mount
Tupungato. The valley between them is 9000 ft. high; and in
that part of the Cordillera are situated the highest passes
south of 33 deg. S. lat., one of which, the Piuquenes Pass,
reaches 13,333 ft., whilst the easiest of transit and almost
the lowest is that of Pichachen (6505 ft.), which is the most
frequented during winter. Mount Tupungato reaches 22,329
ft., according to Argentine measurement. To the north of this
mountain, situated at the watershed of the Andes, extends
a lofty region comprising peaks such as Chimbote (18,645
ft.) and Mount Polleras (20,266 ft.). The Pircas Pass is
situated at a height of 16,962 ft. The gaps of Bermejo and
Iglesia, in the Uspallata road, the best known of all the
passes between Argentina and Chile, are at 13,025 ft. and
13,412 ft. altitude respectively, while the nearest peaks,
those of Juncal and Tolorsa, are 19,358 and 20,140 ft. high.
Mounts Tupungato, Aconcagua (23,393 ft.) and Mercedario
A. Alluvium G. Upper Jurassic Gypsum
C. Cretaceous (including upper & lower) YV. Younger Volcanic Rocks
M. Upper Jurassic (Malm) } OV. Older Volcanic Rocks
D. Middle Jurassic (Dogger) }mostly porphyrite Di. Dioritic Rocks
L. Liassic }porphyritic X. Change of bearing in the
conglomerate Sections