FOOTNOTES:

[1] See the article ARTHROPODA for the use of the term "prosthomere."

[2] See fig. 12 in the article ARTHROPODA.

[3] Though ten is the prevailing number of retinula cells and

rhabdomeres in the lateral eye of Limulus, Watase states that they

may be as few as nine and as many as eighteen.

[4] A great deal of superfluous hypothesis has lately been put

forward in the name of "the principle of convergence of characters"

by a certain school of palaeontologists. The horse is supposed by

these writers to have originated by separate lines of descent in the

Old World and the New, from five-toed ancestors! And the important

consequences following from the demonstration of the identity in

structure of Limulus and Scorpio are evaded by arbitrary and even

phantastic invocations of a mysterious transcendental force which

brings about "convergence" irrespective of heredity and selection.

Morphology becomes a farce when such assumptions are made. (E. R. L.)

[5] A pair of round tubercles on the labram (camerostome or

hypostoma) of several species of Trilobites has been described and

held to be a pair of eyes (22). Sense-organs in a similar position

were discovered in Limulus by Patten (42) in 1894.

[6] The writer is indebted to R.I. Pocock, assistant in the Natural

History departments of the British Museum, for valuable assistance in

the preparation of this article and for the classification and

definition of the groups of Eu-arachnida here given. The general

scheme and some of the details have been brought by the writer into

agreement with the views maintained in this article. Pocock accepts

those views in all essential points and has, as a special student of

the Arachnida, given to them valuable expansion and confirmation. The

writer also desires to express his thanks to Messrs. Macmillan & Co.

for permission to use figs. 22, 43, 44 and 45, which are taken from

Parker and Haswell's _Text-book of Zoology_; and to Messrs. Swan

Sonnenschein & Co. for the loan of several figures from the

translations published by them of the admirable treatise on

_Embryology_ by Professors Korschelt and Heider; also to the

publishers of the treatise on _Palaeontology_ by Professor Zittel,

Herr Oldenbourg and The Macmillan Co., New York, for several cuts of

extinct forms.

[7] Pocock suggests that the area marked vii. in the outline figure

of the dorsal view of _Limulus_ (fig. 7) may be the tergum of the

suppressed prae-genital somite. Embryological evidence must settle

whether this is so or not.

ARAD, or O-ARAD, a town of Hungary, capital of the county of the same

name, 159 m. S.E. of Budapest by rail. Pop. (1900) 53,903. It is

situated on the right bank of the river Maros, and consists of the inner

town and five suburbs. Arad is a modern-built town, and contains many

handsome private and public buildings, including a cathedral. It is the

seat of a Greek-Orthodox bishop, and possesses a Greek-Orthodox

theological seminary, two training schools for teachers--one Hungarian,

and the other Rumanian--and a conservatoire for music. The town played

an important part in the Hungarian revolution of 1848-49, and possesses

a museum containing relics of this war of independence. One of the

public squares contains a martyrs' monument, erected in memory of the

thirteen Hungarian generals shot here on the 6th of October 1849, by

order of the Austrian general Haynau. It consists of a colossal figure

of Hungary, with four allegorical groups, and medallions of the

executed generals. Arad is an important railway junction, and has become

the largest industrial and commercial centre of south-eastern Hungary.

Its principal industries are: distilling, milling, machinery-making,

leather-working and saw-milling. A large trade is carried on in grain,

flour, alcohol, cattle and wood. Arad was a fortified place, and was

captured by the Turks during the wars of the 17th century, and kept by

them till the end of that century. The new fortress, built in 1763,

although small, was formidable, and played a great role during the

Hungarian struggle for independence in 1849. Bravely defended by the

Austrian general Berger until the 1st of July 1849, it was then captured

by the Hungarian rebels, who made it their headquarters during the

latter part of the insurrection. It was from it that Kossuth issued his

famous proclamation (11th August 1849), and it was here that he handed

over the supreme military and civil power to Gorgei. The fortress was

recaptured shortly after the surrender of Gorgei to the Russians at

Vilagos. The fortress is now used as an ammunition depot.

The town of Uj-Arad, i.e. New Arad (pop. 6124), situated on the opposite

bank of the Maros, is practically a suburb of Arad, with which it is

connected by a bridge. The town was founded during the Turkish wars of

the 17th century. The works erected by the Turks for the capture of the

fortress of Arad formed the nucleus of the new town.

Vilagos, the town where the famous capitulation of Gorgei to the

Russians took place on the 13th of August 1849, lies 21 m. by rail

north-east of Arad.

ARAEOSTYLE (Gr. [Greek: araios], weak or widely spaced, and [Greek:

stylos], column), an architectural term for the intercolumniation (q.v.)

given to those temples where the columns had only timber architraves to

carry.

ARAEOSYSTYLE (Gr. [Greek: araios], widely spaced, and [Greek: systylos],

with columns set close together), an architectural term applied to a

colonnade, in which the intercolumniation (q.v.) is alternately wide and

narrow, as in the case of the western porch of St Paul's cathedral and

the east front of the Louvre by Perrault.

ARAGO, DOMINIQUE FRANCOIS JEAN (1786-1853), French physicist, was born

on the 26th of February 1786, at Estagel, a small village near

Perpignan, in the department of the eastern Pyrenees. He was the eldest

of four brothers. Jean (1788-1836) emigrated to America and became a

general in the Mexican army. Jacques Etienne Victor (1799-1855) took

part in L.C. de S. de Freycinet's exploring voyage in the "Uranie" from

1817 to 1821, and on his return to France devoted himself to journalism

and the drama. The fourth brother, Etienne Vincent (1802-1892), is said

to have collaborated with H. de Balzac in the _Heritiere de Birague_,

and from 1822 to 1847 wrote a great number of light dramatic pieces,

mostly in collaboration. A strong republican, he was obliged to leave

France in 1849, but returned after the amnesty of 1859. In 1879 he was

nominated director of the Luxembourg museum.

Showing decided military tastes Francois Arago was sent to the municipal

college of Perpignan, where he began to study mathematics in preparation

for the entrance examination of the polytechnic school. Within two years

and a half he had mastered all the subjects prescribed for examination,

and a great deal more, and, on going up for examination at Toulouse, he

astounded his examiner by his knowledge of Lagrange. Towards the close

of 1803 he entered the polytechnic school, with the artillery service as

the aim of his ambition, and in 1804, through the advice and

recommendation of S.D. Poisson, he received the appointment of secretary

to the Observatory of Paris. He now became acquainted with Laplace, and

through his influence was commissioned, with J.B. Biot, to complete the

meridional measurements which had been begun by J.B.J. Delambre, and

interrupted since the death of P.F.A. Mechain (1744-1804). The two left

Paris in 1806 and began operations among the mountains of Spain, but

Biot returned to Paris after they had determined the latitude of

Formentera, the southernmost point to which they were to carry the

survey, leaving Arago to make the geodetical connexion of Majorca with

Ivica and with Formentera.

The adventures and difficulties of the latter were now only beginning.

The political ferment caused by the entrance of the French into Spain

extended to these islands, and the ignorant populace began to suspect

that Arago's movements and his blazing fires on the top of Mount Galatzo

were telegraphic signals to the invading army. Ultimately they became so

infuriated that he was obliged to cause himself to be incarcerated in

the fortress of Belver in June 1808. On the 28th of July he managed to

escape from the island in a fishing-boat, and after an adventurous

voyage he reached Algiers on the 3rd of August. Thence he procured a

passage in a vessel bound for Marseilles, but on the 16th of August,

just as the vessel was nearing Marseilles, it fell into the hands of a

Spanish corsair. With the rest of the crew, Arago was taken to Rosas,

and imprisoned first in a windmill, and afterwards in the fortress of

that seaport, until the town fell into the hands of the French, when the

prisoners were transferred to Palamos. After fully three months'

imprisonment they were released on the demand of the dey of Algiers, and

again set sail for Marseilles on the 28th of November, but when within

sight of their port they were driven back by a northerly wind to Bougie

on the coast of Africa. Transport to Algiers by sea from this place

would have occasioned a weary stay of three months; Arago, therefore,

set out for it by land under conduct of a Mahommedan priest, and reached

it on Christmas day. After six months' stay in Algiers he once again, on

the 21st of June 1809, set sail for Marseilles, where he had to undergo

a monotonous and inhospitable quarantine in the lazaretto, before his

difficulties were over. The first letter he received, while in the

lazaretto, was from A. von Humboldt; and this was the origin of a

connexion which, in Arago's words, "lasted over forty years without a

single cloud ever having troubled it."

Through all these vicissitudes Arago had succeeded in preserving the

records of his survey; and his first act on his return home was to

deposit them in the Bureau des Longitudes at Paris. As a reward for his

adventurous conduct in the cause of science, he was in September 1809

elected a member of the Academy of Sciences, in room of J.B.L. Lalande,

at the remarkably early age of twenty-three, and before the close of the

same year he was chosen by the council of the polytechnic school to

succeed G. Monge in the chair of analytical geometry. About the same

time he was named by the emperor one of the astronomers of the Royal

Observatory, which was accordingly his residence till his death, and it

was in this capacity that he delivered his remarkably successful series

of popular lectures on astronomy, which were continued from 1812 to

1845.

In 1816, along with Gay-Lussac, he started the _Annales de chimie et de

physique_, and in 1818 or 1819 he proceeded along with Biot to execute

geodetic operations on the coasts of France, England and Scotland. They

measured the length of the seconds-pendulum at Leith, and in Unst, one

of the Shetland isles, the results of the observations being published

in 1821, along with those made in Spain. Arago was elected a member of

the Board of Longitude immediately afterwards, and contributed to each

of its _Annuals_, for about twenty-two years, important scientific

notices on astronomy and meteorology and occasionally on civil

engineering, as well as interesting memoirs of members of the Academy.

In 1830, Arago, who always professed liberal opinions of the extreme

republican type, was elected a member of the chamber of deputies for the

Lower Seine, and he employed his splendid gifts of eloquence and

scientific knowledge in all questions connected with public education,

the rewards of inventors, and the encouragement of the mechanical and

practical sciences. Many of the most creditable national enterprises,

dating from this period, are due to his advocacy--such as the reward to

L.J.M. Daguerre for the invention of photography, the grant for the

publication of the works of P. Fermat and Laplace, the acquisition of

the museum of Cluny, the development of railways and electric

telegraphs, the improvement of the navigation of the Seine, and the

boring of the artesian wells at Grenelle.

In the year 1830 also he was appointed director of the Observatory, and

as a member of the chamber of deputies he was able to obtain grants of

money for rebuilding it in part, and for the addition of magnificent

instruments. In the same year, too, he was chosen perpetual secretary of

the Academy of Sciences, in room of J.B.J. Fourier. Arago threw his

whole soul into its service, and by his faculty of making friends he

gained at once for it and for himself a world-wide reputation. As

perpetual secretary it fell to him to pronounce historical _eloges_ on

deceased members; and for this duty his rapidity and facility of

thought, his happy piquancy of style, and his extensive knowledge

peculiarly adapted him.

In 1834 he again visited England, to attend the meeting of the British

Association at Edinburgh. From this time till 1848 he led a life of

comparative quiet--not the quiet of inactivity, however, for his

incessant labours within the Academy and the Observatory produced a

multitude of contributions to all departments of physical science,--but

on the fall of Louis Philippe he left his laboratory to join in forming

the provisional government. He was entrusted with the discharge of two

important functions, that had never before been united in one person,

viz. the ministry of war and of marine; and in the latter capacity he

effected some salutary reforms, such as the improvement of rations in

the navy and the abolition of flogging. He also abolished political

oaths of all kinds, and, against an array of moneyed interests,

succeeded in procuring the abolition of negro slavery in the French

colonies.

In the beginning of May 1852, when the government of Louis Napoleon

required an oath of allegiance from all its functionaries, Arago

peremptorily refused, and sent in his resignation of his post as

astronomer at the Bureau des Longitudes. This, however, the prince

president, to his credit, declined to accept, and made "an exception in

favour of a _savant_ whose works had thrown lustre on France, and whose

existence his government would regret to embitter." But the tenure of

office thus granted did not prove of long duration. Arago was now on his

death-bed, under a complication of diseases, induced, no doubt, by the

hardships and labours of his earlier years. In the summer of 1853 he was

advised by his physicians to try the effect of his native air, and he

accordingly set out for the eastern Pyrenees. But the change was

unavailing, and after a lingering illness, in which he suffered first

from diabetes, then from Bright's disease, complicated by dropsy, he

died in Paris on the 2nd of October 1853.

Arago's fame as an experimenter and discoverer rests mainly on his

contributions to magnetism and still more to optics. He found that a

magnetic needle, made to oscillate over nonferruginous surfaces, such as

water, glass, copper, &c., falls more rapidly in the extent of its

oscillations according as it is more or less approached to the surface.

This discovery, which gained him the Copley medal of the Royal Society

in 1825, was followed by another, that a rotating plate of copper tends

to communicate its motion to a magnetic needle suspended over it

("magnetism of rotation"). Arago is also fairly entitled to be regarded

as having proved the long-suspected connexion between the aurora

borealis and the variations of the magnetic elements.

In optics we owe to him not only important optical discoveries of his

own, but the credit of stimulating the genius of A.J. Fresnel, with

whose history, as well as with that of E.L. Malus and of Thomas Young,

this part of his life is closely interwoven. Shortly after the beginning

of the 19th century the labours of these three philosophers were shaping

the modern doctrine of the undulatory theory of light. Fresnel's

arguments in favour of that theory found little favour with Laplace,

Poisson and Biot, the champions of the emission theory; but they were

ardently espoused by Humboldt and by Arago, who had been appointed by

the Academy to report on the paper. This was the foundation of an

intimate friendship between Arago and Fresnel, and of a determination to

carry on together further researches in this subject, which led to the

enunciation of the fundamental laws of the polarization of light known

by their names (see POLARIZATION). As a result of this work Arago

constructed a _polariscope_, which he used for some interesting

observations on the polarization of the light of the sky. To him is also

due the discovery of the power of _rotatory polarization_ exhibited by

quartz, and last of all, among his many contributions to the support of

the undulatory hypothesis, comes the _experimentum crucis_ which he

proposed to carry out for comparing directly the velocity of light in

air and in water or glass. On the emission theory the velocity should be

accelerated by an increase of density in the medium; on the wave theory,

it should be retarded. In 1838 he communicated to the Academy the

details of his apparatus, which utilized the revolving mirrors employed

by Sir C. Wheatstone in 1835 for measuring the velocity of the electric

discharge; but owing to the great care required in the carrying out of

the project, and to the interruption to his labours caused by the

revolution of 1848, it was the spring of 1850 before he was ready to put

his idea to the test; and then his eyesight suddenly gave way. Before

his death, however, the retardation of light in denser media was

demonstrated by the experiments of H.L. Fizeau and J.B.L. Foucault,

which, with improvements in detail, were based on the plan proposed by

him.

Arago's _OEuvres_ were published after his death under the direction

of J.A. Barral, in 17 vols., 8vo, 1854-1862; also separately his

_Astronomie populaire_, in 4 vols.; _Notices biographiques_, in 3

vols.; _Notices scientifiques_, in 5 vols.; _Voyages scientifiques_,

in 1 vol.; _Memoires scientifiques_, in 2 vols.; _Melanges_, in 1

vol.; and _Tables analytiques et documents importants_ (with

portrait), in 1 vol. English translations of the following portions of

his works have appeared:--_Treatise on Comets_, by C. Gold, C.B.

(London, 1833); also translated by Smyth and Grant (London, 1861);

_Hist. eloge of James Watt_, by James Muirhead (London, 1839); also

translated, with notes, by Lord Brougham; _Popular Lectures on

Astronomy_, by Walter Kelly and Rev. L. Tomlinson (London, 1854); also

translated by Dr W.H. Smyth and Prof. R. Grant, 2 vols. (London,

1855); _Arago's Autobiography_, translated by the Rev. Baden Powell

(London, 1855, 1858); _Arago's Meteorological Essays_, with

introduction by Humboldt, translated under the superintendence of

Colonel Sabine (London, 1855), and _Arago's Biographies of Scientific

Men_, translated by Smyth, Powell and Grant, 8vo (London, 1857).

ARAGON, or ARRAGON (in Span. _Aragon_), a captaincy-general, and

formerly a kingdom of Spain; bounded on the N. by the Pyrenees, which

separate it from France, on the E. by Catalonia and Valencia, S. by

Valencia, and W. by the two Castiles and Navarre. Pop. (1900) 912,711;

area, 18,294 sq. m. Aragon was divided in 1833 into the provinces of

Huesca, Teruel and Saragossa; an account of its modern condition is

therefore given under these names, which have not, however, superseded

the older designation in popular usage.

Aragon consists of a central plain, edged by mountain ranges. On the

south, east and west, these ranges, though wild and rugged, are of no

great elevation, but on the north the Pyrenees attain their greatest

altitude in the peaks of Aneto (11,168 ft.) and Monte Perdido (10,998

ft.)--also known as Las Tres Sorores, and, in French, as Mont Perdu. The

central pass over the Pyrenees is the Port de Canfranc, on the line

between Saragossa and Pau. Aragon is divided by the river Ebro (q.v.),

which flows through it in a south-easterly direction, into two nearly

equal parts, known as Trans-ibero and Cis-ibero. The Ebro is the

principal river, and receives from the north, in its passage through the

province, the Arba, the Gallego and the united waters of the Cinca,

Esera, Noguera Ribagorzana, Noguera Pallaresa and Segre--the last three

belonging to Catalonia. From the south it receives the Jalon and Jiloca

(or _Xalon_ and _Xiloca_) and the Guadalope. The Imperial Canal of

Aragon, which was begun by the emperor Charles V. in 1529, but remained

unfinished for nearly two hundred years, extends from Tudela to El Burgo

de Ebro, a distance of 80 m.; it has a depth of 9 ft., and an average

breadth of 69, and is navigable for vessels of about 80 tons. The Royal

Canal of Tauste, which lies along the north side of the Ebro, was cut

for purposes of irrigation, and gives fertility to the district. Two

leagues north-north-east of Albarracin is the remarkable fountain called

Cella, 3700 ft. above the sea, which forms the source of the Jiloca; and

between this river and the Sierra Molina is an extensive lake called

Gallocanta, covering about 6000 acres. The climate is characterized by

extreme heat in the summer and cold in the winter; among the mountains

the snowfall is heavy, and thunderstorms are frequent, but there is

comparatively little rain.

Within a recent geological period, central Aragon was undoubtedly

submerged by the sea, and the parched chalky soil remains saturated with

salt, while many of the smaller streams run brackish. As the mountains

of Valencia and Catalonia effectually bar out the fertilizing moisture

of the sea-winds, much of the province is a sheer wilderness, stony,

ash-coloured, scarred with dry watercourses, and destitute of any

vegetation except thin grass and heaths. In contrast with the splendid

fertility of Valencia or the south of France, the landscape of this

region, like the rest of central Spain, seems almost a continuation of

the north African desert area. There are, however, extensive oak, pine

and beech forests in the highlands, and many beautiful oases in the

deeply sunk valleys, and along the rivers, especially beside the Ebro,

which is, therefore, often called the "Nile of Aragon." In such oases

the flora is exceedingly rich. Wheat, maize, rice, oil, flax and hemp,

of fine quality, are grown in considerable quantities; as well as

saffron, madder, liquorice, sumach, and a variety of fruits. Merino wool

is one of the chief products.

In purity of race the Aragonese are probably equal to the Castilians, to

whom, rather than to the Catalans or Valencians, they are also allied in

character. The dress of the women is less distinctive than that of the

men, who wear a picturesque black and white costume, with knee-breeches,

a brilliantly coloured sash, black hempen sandals, and a handkerchief

wound round the head.

Three counties--Sobrarbe, situated near the headwaters of the Cinca,

Aragon, to the west, and Ribagorza or Ribagorca, to the east--are

indicated by tradition and the earliest chronicles as the cradle of the

Aragonese monarchy. These districts were never wholly subdued when the

Moors overran the country (711-713). Sobrarbe especially was for a time

the headquarters of the Christian defence in eastern Spain. About 1035,

Sancho III. the Great, ruler of the newly established kingdom of

Navarre, which included the three counties above mentioned, bequeathed

them to Gonzalez and Ramiro, his sons. Ramiro soon rid himself of his

rival, and welded Sobrarbe, Ribagorza and Aragon into a single kingdom,

which thenceforward grew rapidly in size and power and shared with

Castile the chief part in the struggle against the Moors. The history of

this period, which was terminated by the union of Castile and Aragon

under Ferdinand and Isabella in 1479, is given, along with a full

account of the very interesting constitution of Aragon, under SPAIN

(q.v.). At the height of its power under James I. (1213-1276), the

kingdom included Valencia, Catalonia, the Balearic Islands and the

considerable territory of Montpellier in France; while Peter III.

(1276-1285) added Sicily to his dominions.

The literature relating to Aragon is very extensive. See, in addition

to the works cited in the article SPAIN (section _History_), "Les

Archives d'Aragon et de Navarre," by L. Cadier, in _Bibliotheque de

l'Ecole des Chartes_, 49 (Paris, 1888). Among the more important

original authorities, the following may be selected:--for general

history, _Anales de la corona de Aragon_, by G. Curita, 3rd ed. in 7

folio volumes (Saragossa, 1668-1671; 1st ed. 1562-1580);--for

ecclesiastical history, _Teatro historico de las iglesias de Aragon_

(Pamplona, 1770-1807); for economic history, _Historia de la economia

politica de Aragon_, by I.J. de Asso y del Rio (Saragossa, 1798). For

the constitution and laws of Aragon, see _Origines del Justicia de

Aragon_, &c., by J. Ribera Tarrago (Saragossa, 1897), and

_Instituciones y reyes de Aragon_, by V. Balaguer (Madrid, 1896). The

topography, inhabitants, art, products, &c., of the kingdom are

described in a volume of the series _Espana_ entitled _Aragon_, by

J.M. Quadrado (Barcelona, 1886).

ARAGONITE, one of the mineral forms of calcium carbonate (CaCO3), the

other form being the more common mineral calcite. It crystallizes in the

orthorhombic system, and the crystals are either prismatic or acicular

in habit. Simple crystals are, however, rare; twinning on the prism

planes (_M_ in the figures) being a characteristic feature of the

mineral (fig. 1). This twinning is usually often repeated on the same

plane (fig. 2), and gives rise to striations on the terminal faces (k)

of the crystals; often, also, three crystals are twinned together on two

of the prism planes of one of them, producing an apparently hexagonal

prism. The mineral is colourless, white or yellowish, transparent or

translucent, has a vitreous lustre, and, in fact, is not unlike calcite

in general appearance. It may, however, always be readily distinguished

from calcite by the absence of any marked cleavage, and by its greater

hardness (H. = 3-1/2-4) and specific gravity (2.93); further, it is

optically biaxial, whilst calcite is uniaxial. It is brittle and has a

subconchoidal fracture; on a fractured surface the lustre is decidedly

resinous in character.

[Illustration: FIG. 1.]

[Illustration: FIG. 2.]

The mineral was first found, as reddish twinned crystals with the form

of six-sided prisms, at Molina in Aragon, Spain, where it occurs with

gypsum and small crystals of ferruginous quartz in a red clay. It is

from this locality that the mineral takes its name, which was originally

spelt arragonite. Fine groups of crystals of the same habit are found in

the sulphur deposits of Girgenti in Sicily; also at Herrengrund near

Neusohl in Hungary. At many other localities the mineral takes the form

of radiating groups of acicular crystals, such as those from the

haematite mines of west Cumberland: beautiful feathery forms have been

found in a limestone cave in the Transvaal. Fibrous forms are also

common. A peculiar coralloidal variety known as _flosferri_ ("flower of

iron") consists of radially arranged fibres: magnificent snow-white

specimens of this variety have long been known from the iron mines of

Eisenetz in Styria. The calcareous secretions of many groups of

invertebrate animals consist of aragonite (calcite is also common);

pearls may be specially cited as an example.

Aragonite is a member of the isomorphous group of minerals comprising

witherite (BaCO3), strontianite (SrCO3), cerussite (PbCO3) and bromlite

((Ba, Ca)CO3); and crystals of aragonite sometimes contain small amounts

of strontium or lead. A variety known as tarnowitzite, from Tarnowitz in

Silesia, contains about 5% of lead carbonate.

Aragonite is the more unstable of the two modifications of calcium

carbonate. A crystal of aragonite when heated becomes converted into a

granular aggregate of calcite individuals: altered crystals of this kind

(paramorphs) are not infrequently met with in nature, whilst in fossil

shells the original nacreous layer of aragonite has invariably been

altered to calcite. From a solution of calcium carbonate in water

containing carbon dioxide crystals of calcite are deposited at the

ordinary temperature, but from a warm solution aragonite crystallizes

out. The thermal springs of Carlsbad deposit spherical concretions of

aragonite, forming masses known as pisolite or _Sprudelstein_.

(L. J. S.)

ARAGUA, one of the smaller states of Venezuela under the redivision of

1904, lying principally within the parallel ranges of the Venezuelan

Cordillera, and comprising some of the most fertile and healthful

valleys of the republic. It is bounded E. by the Federal District and

Maturin, S. by Guarico and W. by Zamora and Carabobo. Pop. (1905, est.)

152,364. Aragua has a short coast-line on the Caribbean west of the

Federal District, but has no port of consequence. Cattle, swine and

goats are raised, and the state produces coffee, sugar, cacao, beans,

cereals and cheese. The climate of the higher valleys is subtropical,

the mean annual temperature ranging from 74 deg. to 80 deg. F. The

capital, La Victoria (pop. 7800), is situated in the fertile Aragua

valley, 1558 ft. above sea-level and 36 m. south-west of Caracas. Other

important towns are Barbacoas (pop. 13,109) on the left bank of the

Guarico in a highly fertile region, Ciudad de Cura and Maracay (pop.

7500), 56 m. west-south-west of Caracas near the north-east shore of

Lake Valencia. The last two towns are on the railway between Caracas and

Valencia.

ARAGUAYA, ARAGUAY or ARAGUIA, a river of Brazil and principal affluent

of the Tocantins, rising in the Serra do Cayapo, where it is known as

the Rio Grande, and flowing in a north by east direction to a junction

with the Tocantins at Sao Joao do Araguaya, or Sao Joao das Duas Barras.

Its upper course forms the boundary line between Goyaz and Matto Grosso.

The river divides into two branches at about 13 deg. 20' S. lat., and

unites again at 10 deg. 30', forming the large island of Santa Anna or

Bananal. The eastern branch, called the Furo, is the one used by boats,

as the main channel is obstructed by rapids. Its principal affluent is

the Rio das Mortes, which rises in the Serra de Sao Jeronymo, near

Cuyaba, Matto Grosso, and is utilized by boatmen going to Para. Of other

affluents, the Bonito, Garcas, Cristallino and Tapirape on the west, and

the Pitombas, Claro, Vermelho, Tucupa and Chavante on the east, nothing

definite is known as the country is still largely unexplored. The

Araguaya has a course of 1080 m., considerable stretches of which are

navigable for small river steamers, but as the river below Santa Anna

Island is interrupted by reefs and rapids in two places--one having a

fall of 85 ft. in 18 m., and the other a fall of 50 ft. in 12 m.--it

affords no practicable outlet for the products of the state. It was

explored in part by Henri Coudreau in 1897.

See Coudreau's _Voyage au Tocantins-Araguaya_ (Paris, 1897).

ARAKAN, a division of Lower Burma. It consists of a strip of country

running along the eastern seaboard of the Bay of Bengal, from the Naaf

estuary, on the borders of Chittagong, to Cape Negrais. Length from

northern extremity to Cape Negrais, about 400 m.; greatest breadth in

the northern part, 90 m., gradually diminishing towards the south, as it

is hemmed in by the Arakan Yoma mountains, until, in the extreme south,

it tapers away to a narrow strip not more than 15 m. across. The coast

is studded with islands, the most important of which are Cheduba, Ramree

and Shahpura. The division has its headquarters at Akyab and consists of

four districts--namely, Akyab, Northern Arakan Hill Tracts, Sandoway and

Kyaukpyu, formerly called Ramree. Its area is 18,540 sq. m. The

population at the time of the British occupation in 1826 did not exceed

100,000. In 1831 it amounted to 173,000; in 1839 to 248,000, and in 1901

to 762,102.

The principal rivers of Arakan are--(1) the Naaf estuary, in the north,

which forms the boundary between the division and Chittagong; (2) the

Myu river, an arm of the sea, running a course almost parallel with the

coast for about 50 m.; (3) the Koladaing river, rising near the Blue

mountain, in the extreme north-east, and falling into the Bay of Bengal

a few miles south of the Myu river, navigable by vessels of from 300 to

400 tons burden for a distance of 40 m. inland; and (4) the Lemyu river,

a considerable stream falling into the bay a few miles south of the

Koladaing. Farther to the south, owing to the nearness of the range

which bounds Arakan on the east, the rivers are of but little

importance. These are the Talak and the Aeng, navigable by boats; and

the Sandoway, the Taungup and the Gwa streams, the latter of which alone

has any importance, owing to its mouth forming a good port of call or

haven for vessels of from 9 to 10 ft. draught. There are several passes

over the Yoma mountains, the easiest being that called the Aeng route,

leading from the village of that name into Upper Burma. The staple crop

of the province is rice, along with cotton, tobacco, sugar, hemp and

indigo. The forests produce abundance of excellent oak and teak timber.

The natives of Arakan trace their history as far back as 2666 B.C., and

give a lineal succession of 227 native princes down to modern times.

According to them, their empire had at one period far wider limits, and

extended over Ava, part of China, and a portion of Bengal. This

extension of their empire is not, however, corroborated by known facts

in history. At different times the Moguls and Pegus carried their arms

into the heart of the country. The Portuguese, during the era of their

greatness in Asia, gained a temporary establishment in Arakan; but in

1782 the province was finally conquered by the Burmese, from which

period until its cession to the British in 1826, under the treaty of

Yandaboo, its history forms part of that of Burma. The old city of

Arakan, formerly the capital of the province, is situated on an inferior

branch of the Koladaing river. Its remoteness from the ports and

harbours of the country, combined with the extreme unhealthiness of its

situation, have led to its gradual decay subsequently to the formation

of the comparatively recent settlement of Akyab, which place is now the

chief town of the province. The old city (now Myohaung) lies 50 m.

north-east of Akyab. The Maghs, who form nearly the whole population of

the province, follow the Buddhist doctrines, which are universally

professed throughout Burma. The priests are selected from all classes of

men, and one of their chief employments is the education of children.

Instruction is consequently widely diffused, and few persons, it is

said, can be found in the province who are unable to read. The

qualifications for entering into the priestly order are good conduct and

a fair measure of learning--such conduct at least as is good according

to Buddhist tenets, and such learning as is esteemed among their

votaries.

The Arakanese are of Burmese origin, but separated from the parent stock

by the Arakan Yoma mountains, and they have a dialect and customs of

their own. Though conquered by the Burmese, they have remained distinct

from their conquerors.

The Northern Arakan Hill Tracts district is under a superintendent, who

is usually a police officer, with headquarters at Paletwa. The area of

the Hill Tracts is 5233 sq. m.; pop. (1901) 20,682. (J. G. Sc.)

ARAKCHEEV, ALEKSYEI ANDREEVICH, COUNT (1769-1834), Russian soldier and

statesman, was descended from an ancient family of Great Novgorod. From

his mother, Elizabeth Vitlitsaya, he inherited most of his

characteristics, an insatiable love of work, an almost pedantic love of

order and the most rigorous sense of duty. In 1788 he entered the corps

of noble cadets in the artillery and engineering department, where his

ability, especially in mathematics, soon attracted attention. In July

1791 he was made an adjutant on the staff of Count N.I. Saltuikov, who

(September 1792) recommended him to the cesarevich Paul Petrovich as the

artillery officer most capable of reorganizing the army corps maintained

by the prince at Gatchina. Arakcheev speedily won the entire confidence

of Paul by his scrupulous zeal and undeniable technical ability. His

inexorable discipline (magnified into cruelty by later legends) soon

made the Gatchina corps a model for the rest of the Russian army. On the

accession of Paul to the throne Arakcheev was promptly summoned to St

Petersburg, appointed military commandant in the capital, and

major-general in the grenadier battalion of the Preobrazhenskoe Guard.

On the 12th of December 1796, he received the ribbon of St Anne and a

rich estate at Gruzina in the government of Novgorod, the only

substantial gift ever accepted by him during the whole of his career. At

the coronation (5th of April 1797) Paul created him a baron, and he was

subsequently made quartermaster-general and colonel of the whole

Preobrazhenskoe Guard. It was to Arakcheev that Paul entrusted the

reorganization of the army, which during the latter days of Catherine

had fallen into a state of disorder and demoralization. Arakcheev

remorselessly applied the iron Gatchina discipline to the whole of the

imperial forces, beginning with the Guards. He soon became generally

detested by the army, but pursued his course unflinchingly and

introduced many indispensable hygienic reforms. "Clean barracks are

healthy barracks," was his motto. Nevertheless, the opposition of the

officers proved too strong for him, and on the 18th of March 1798 he was

dismissed from all his appointments. Arakcheev's first disgrace only

lasted six months. On the 11th of August he was received back into

favour, speedily reinstated in all his former offices, and on the 5th of

May 1799 was created a count, the emperor himself selecting the motto:

"Devoted, not servile." Five months later he was again in disgrace, the

emperor dismissing him on the strength of a denunciation subsequently

proved to be false. It was a fatal step on Paul's part, for everything

goes to prove that he would never have been assassinated had Arakcheev

continued by his side. During the earlier years of Alexander, Arakcheev

was completely overlooked. Only on the 27th of April 1803, was the count

recalled to St Petersburg, and employed as inspector-general of the

artillery. His wise and thorough reorganization of the whole department

contributed essentially to the victories of the Russians during the

Napoleonic wars. All critics agree, indeed, that the Arakcheev

administration was the golden era of the Russian artillery. The activity

of the inexhaustible inspector knew no bounds, and he neglected nothing

which could possibly improve this arm. His principal reforms were the

subdivision of the artillery divisions into separate independent units,

the formation of artillery brigades, the establishment of a committee of

instruction (1808), and the publishing of an _Artillery Journal_. At

Austerlitz he had the satisfaction of witnessing the actual results of

his artillery reforms. The commissariat scandals which came to light

after the peace of Tilsit convinced the emperor that nothing short of

the stern and incorruptible energy of Arakcheev could reach the sources

of the evil, and in January 1808 he was appointed inspector-general and

war minister. When, on the outbreak of the Swedish war of 1809, the

emperor ordered the army to take advantage of an unusually severe frost

and cross the ice of the Gulf of Finland, it was only the presence of

Arakcheev that compelled an unwilling general and a semi-mutinous army

to begin a campaign which ended in the conquest of Finland. On the

institution of the "Imperial Council" (1st of January 1810), Arakcheev

was made a member of the council of ministers and a senator, while still

retaining the war office. Subsequently Alexander was alienated from him

owing to the intrigues of the count's enemies, who hated him for his

severity and regarded him as a dangerous reactionary. The alienation was

not, however, for long. It is true, Arakcheev took no active part in the

war of 1812, but all the correspondence and despatches relating to it

passed through his hands, and he was the emperor's inseparable companion

during the whole course of it. At Paris (31st of March 1814) Alexander,

with his own hand, wrote the _ukaz_ appointing him a field-marshal, but

he refused the dignity, accepting, instead, a miniature portrait of his

master. From this time Alexander's confidence in Arakcheev steadily

increased, and the emperor imparted to him, first of all, his many

projects of reform, especially his project of military colonies, the

carrying out of the details of which was committed to Arakcheev (1824).

The failure of the scheme was due not to any fault of the count, but to

the inefficiency and insubordination of the district officers. In

Alexander's last years Arakcheev was not merely his chief counsellor,

but his dearest friend, to whom he submitted all his projects for

consideration and revision. The most interesting of these projects was

the plan for the emancipation of the peasantry (1818). On the accession

of Nicholas I., Arakcheev, thoroughly broken in health, gradually

restricted his immense sphere of activity, and on the 26th of April

1826, resigned all his offices and retired to Carlsbad. The 50,000

roubles presented to him by the emperor as a parting gift he at once

handed to the Pavlovsk Institute for the education of the daughters of

poor gentlemen. His last days he spent on his estate at Gruzina,

carefully collecting all his memorials of Alexander, whose memory he

most piously cherished. He also set aside 25,000 roubles for the author

of the best biography of his imperial friend. Arakcheev died on the 21st

of April 1834, with his eyes fixed to the last on the late emperor's

portrait. "I have now done everything," he said, "so I can go and make

my report to the emperor Alexander." In 1806 he had married Natalia

Khomutova, but they lived apart, and he had no children by her.

See Vasily Ratch, _Memorials of Count Arakcheev_ (Rus.) (St

Petersburg, 1864); Mikhail Ivanovich Semevsky, _Count Arakcheev and

the Military Colonies_ (Rus.) (St Petersburg, 1871); Theodor

Schiemann, _Gesch. Russland's unter Kaiser Nikolaus I._, vol. i.,

_Alexander I._, &c. (Berlin, 1904). (R. N. B.)

ARAL, a lake or inland sea in the west of Asia, situated between lat. 43

deg. 30' and 46 deg. 51' N., and long. 58 deg. 13' and 61 deg. 56' E. It

was known to the ancient Arab and Persian geographers as the Sea of

Khwarizm or Kharezm, from the neighbouring district of the Chorasmians,

and derives its present name from the Kirghiz designation of

Aral-denghiz, or Sea of Islands. In virtue of its area (26,233 sq. m.)

it is the fourth largest inland sea of the world. It has nearly the same

length as width, namely about 170 m., if its northern gulf

(Kichkineh-denghiz) is left out of account. Its depth is insignificant,

the maximum being 220 ft. in a depression in the north-west, and the

mean depth only 50 ft., so that notwithstanding its area it contains

only eleven times as much water as the Lake of Geneva. Its altitude is

242-1/2 ft. above the Caspian, i.e. about 155 ft. above the ocean. The

lake is surrounded on the north by steppes; on the west by the rocky

plateau of Ust-Urt, which separates it from the Caspian; on the south by

the alluvial district of Khiva; and on the east by the Kyzyl-kum, or Red

Sand Desert. On the north the shores are comparatively low, and the

coast-line is broken by a number of irregular bays, of which the most

important are those of Sary-chaganak and Paskevich. On the west an

almost unbroken wall of rock extends from Chernychev Bay southwards,

rising towards the middle to 500 ft. The southern coast is occupied by

the delta of the Oxus (Jihun, Amu-darya), one of the arms of which, the

Laudan, forms a swamp, 80 m. long and 20 broad, before it discharges

into the sea. The only other tributary of any size that the sea receives

is the Jaxartes (Sihun, Syr-darya) which enters towards the northern

extremity of the east coast, and is suspected to be shifting its

embouchure more and more to the north. This river, as well as the Amu,

conveys vast quantities of sediment into the lake; the delta of the

Syr-darya increased by 13-3/4 sq. m. between 1847 and 1900. The eastern

coast is fringed with multitudes of small islands, and other islands,

some of considerable size, are situated in the open towards the north

and west. Kug-Aral, the largest, lies opposite the mouth of the

Syr-darya, cutting off the Kichkineh-denghiz or Little Sea. The next

largest island is the Nikolai, nearly in the middle. Navigation is

dangerous owing to the frequency and violence of the storms, and the

almost total absence of shelter. The north-east wind is the most

prevalent, and sometimes blows for months together. The only other

craft, except the steamships of the Russians, that venture on the

waters, are the flat-bottomed boats of the Kirghiz.

In regard to the period of the formation of the Aral there were formerly

two theories. According to Sir H.C. Rawlinson (_Proc. Roy. Geog. Soc._,

March 1867) the disturbances which produced the present lake took place

in the course of the middle ages; while Sir Roderick Murchison contended

(_Journ. of Roy. Geog. Soc._, 1867, p. cxliv. &c.) that the Caspian and

Aral existed as separate seas before and during all the historic period,

and that the main course of the rivers Jaxartes and Oxus was determined

in a prehistoric era. The former based his opinion largely on historical

evidence, and the latter trusted principally to geological data. There

is no doubt that in recent historical times Lake Aral had a much greater

extension than it has at the present time, and that its area is now

diminishing. This is, of course, due to the excess of evaporation over

the amount of water supplied by its two feeders, the Amu-darya and the

Syr-darya, both of which are seriously drawn upon for irrigation in all

the oases they flow through. Old shore lines and other indications point

to the level of the lake having once been 50 ft. above the existing

level. Nevertheless the general desiccation is subject to temporary

fluctuations, which appear to correspond to the periods recently

suggested by Eduard Bruckner (b. 1862); for, whereas the lake diminished

and shrank during 1850-1880, since the latter year it has been rising

again. Islands which were formerly connected with the shore are now some

distance away from it and entirely surrounded by water. Moreover, on a

graduated level, put down in 1874, there was a permanent rise of nearly

4 ft. by 1901. The temperature at the bottom was found (1900-1902) by

Emil Berg to be 33.8 deg. Fahr., while that of the surface varied from

44.5 deg. to 80.5 deg. between May and September; the mean surface

temperature for July was 75 deg. The salinity of the water is much less

than that of the ocean, containing only 1.05% of salt, and the lake

freezes every year for a great distance from its shores. The opinion

that Lake Aral periodically disappeared, which was for a long time

countenanced by Western geographers, loses more and more probability now

that it is evident that at a relatively recent period the Caspian Sea

extended much farther eastward than it does now, and that Lake Aral

communicated with it through the Sary-kamysh depression. The present

writer is even inclined to think that, besides this southern

communication with the Caspian, Lake Aral may have been, even in

historical times, connected with the Mortvyi Kultuk (Tsarevich) Gulf of

the Caspian, discharging part of its water into that sea through a

depression of the Ust-Urt plateau, which is marked by a chain of lakes

(Chumyshty, Asmantai). In this case it might have been easily confounded

with a gulf of the Caspian (as by Jenkinson). That the level of Lake

Aral was much higher in post-Pliocene times is proved by the discovery

of shells of its characteristic species of _Pecten_ and _Mytilus_ in the

Kara-kum Desert, 33 m. south of the lake and at an altitude of 70 ft.

above its present level, and perhaps even up to 200 ft. (by Syevertsov).

The fish of Lake Aral belong to fresh-water species, and in some of its

rapid tributaries the interesting _Scaphirhynchus_, which represents a

survival from the Tertiary epoch, is found. The fishing is very

productive, the fish being exported to Turkestan, Merv and Russia. The

shores of the lake are uninhabited; the nearest settlements are Kazala,

55 m. east, on the Syr, and Chimbai and Kungrad in the delta of the Amu.

AUTHORITIES.--Maksheev's "Description of Lake Aral," and Kaulbars'

"Delta of the Amu," in _Zapiski of Russ. Geogr. Soc._, 1st series, v.,

and new series, ix.; _Grimm's Studies of the Aral-Caspian Expedition_;

Nikolsky's "Fishing in Lake Aral," in _Izvestia, Russ. Geogr. Soc._,

1887; Prof. Mushketov, _Turkestan_, vol. i. (1886), which contains

bibliographical references; Rosler, _Die Aralseefrage_ (1873); Wood,

_The Shores of the Aral Lake_ (1876); and Berg in _Izvestia, Turkestan

Branch of Russian Geog. Soc._ (vol. iii., Tashkent, 1902).

(P. A. K.)

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