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CAUCASIA, or CAUCASUS

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Originally appearing in Volume V05, Page 550 of the 1911 Encyclopedia Britannica.
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See also:

CAUCASIA, or See also:CAUCASUS  , a See also:governor-generalship of See also:Russia, occupying the See also:isthmus between the See also:Black See also:Sea and the Sea of See also:Azov on the See also:west and the See also:Caspian Sea on the See also:east, as well as portions of the Armenian See also:highlands . Its See also:northern boundary is the Kuma-See also:Manych depression, a See also:succession of narrow, See also:half-desiccated lakes and See also:river-beds, only temporarily filled with See also:water and connecting the Manych, a tributary of the See also:Don, with the Kuma, which flows into the Caspian . This depression is supposed to be a relic of the former See also:post-See also:Pliocene connexion between the Black Sea and the Caspian, and is accepted by most geographers as the natural frontier between See also:Europe and See also:Asia, while others make the dividing-See also:line coincide with the See also:principal water-parting of the See also:Caucasus See also:mountain See also:system . The See also:southern boundary of See also:Caucasia is in See also:part coincident with the river See also:Aras (Araxes), in part purely conventional and See also:political . It was shifted several times during the 19th See also:century, but now runs from a point on the Black Sea, some 20 M. See also:south of See also:Batum, in a south-easterly and easterly direction to Mt . See also:Ararat, and thence along the Aras to within 30 M. of its confluence with the Kura, where it once more turns south-east, and eventually strikes the Caspian at See also:Astara (300 35' N.) . This large territory, covering an See also:area of 180,843 sq. m., and having in 1897 9,248,695 inhabitants (51 per sq. m.) , maybe divided into four natural zones or sections: —(i.) the plains See also:north of the Caucasus mountains, comprising the administrative See also:division of Northern Caucasia; (ii.) the Caucasus range and the highlands of See also:Daghestan; (iii.) the valleys of the Rion and the Kura, between the Caucasus range and the highlands of See also:Armenia; and (iv.) the highlands of Armenia . (i.) The plains of Northern Caucasia, which include most of the provinces of See also:Kuban and See also:Terek and of the See also:government of See also:Stavropol, slope gently downwards from the See also:foot of the Caucasus range towards the Kuma-Manych depression . It is only in their centre that they reach altitudes of as much as 2000-2500 ft. e.g. in the Stavropol " See also:plateau," which stretches northwards, separating the tributaries of the Kuban from those of the Terek and the Kuma . Towards the foothills of the Caucasus they are clothed' with thick forests, while in the west they See also:merge into the See also:steppes of south Russia or end in marshy ground, choked with reeds and rushes, in the See also:delta of the Kuban . In the north and east they give See also:place, as the Manych and the coasts of the Caspian are approached, to arid, sandy, stony steppes . The See also:soil of these plains is generally very fertile and they support a See also:population of nearly 2,800,000 Russians, composed of See also:Cossacks and See also:peasant immigrants, settled chiefly along the See also:rivers and grouped in large, wealthy villages .

They carry on agriculturewheat-growing on a large See also:

scale—with the aid of See also:modern agricultural See also:machines, and breed See also:cattle and horses . Vines are extensively cultivated on the See also:low levels, and a variety of domestic trades are prosecuted in the villages . The higher parts of the plains, which are deeply trenched by the upper tributaries of the rivers, are inhabited by various Caucasian races—Kabardians and Cherkesses (Circassians) in the west, Ossetes in the See also:middle, and several tribal elements from Daghestan, described under the See also:general name of Chechens, in the east; while nomadic Nogai See also:Tatars and Turkomans occupy the steppes . (ii.) The Caucasus range runs from north-west to south-east from the Strait of See also:Kerch to the Caspian Sea for a length of 900 M., with a varying breadth of 30 to 140 m., and covers a See also:surface of 12,000 sq. m . The orographical characteristics of the Caucasus are described in detail under that heading . (iii.) The combined valleys of the Rion and the Kura, which intervene between the Caucasus and the Armenian highlands, and stretch their axes north-west and south-east respectively, embrace the most populous and most fertile parts of Caucasia . They correspond roughly with the governments of See also:Kutais, See also:Tiflis, See also:Elisavetpol and See also:Baku, and have a population of nearly 3,650,000 . The two valleys are separated by the low See also:ridge of the Suram or Meskes mountains . Spurs from the Caucasus and from the Armenian highlands fill up the broad latitudinal depression between them . Above (i.e. west of) Tiflis those spurs so far intrude into the valley that it is reduced to a narrow 'See also:strip in breadth . But below that See also:city it suddenly widens out, and the width gradually increases through the stretch of 350 M. to the Caspian, until in the Mugan See also:steppe along that sea it See also:measures See also:loo m. in width . The See also:snow-clad peaks of the See also:main Caucasus, descending by See also:short, steep slopes, fringe the valley on the north, while an abrupt escarpment, having the characteristics of a border ridge of the Armenian highlands, fronts it on the south .

The See also:

floor of the valley slopes gently eastwards, from 1200 ft. at Tiflis to 500 ft. in the middle, and to 85 ft. below normal sea-level beside the Caspian . But the uniformity of the slope is interrupted by a plateau (2000-3000 ft. in See also:altitude) along the southern foothills of the east central Caucasus, in the region known as Kakhetia, drained by the Alazan, a See also:left-See also:hand tributary of the Kura . The deep, short See also:gorges and glens which seam the southern slopes of the Caucasus are inhabited by Ossetes, Tushes, Pshays and See also:Khevsurs in the west, and by various tribes of See also:Lesghians in the east . In these high and stony valleys every available patch of ground is utilized for the cultivation of See also:barley, even up to altitudes of 7000 and 8000 ft. above the level of the sea; but cattle-breeding is the principal resource of the mountaineers, whose little communities are often separated from one another by passes, few of which are See also:lower than mono ft . The steppes along the bottom of the principal valley are for the most part too dry to be cultivated without See also:irrigation . It is only in Kakhetia, where numerous mountain streams See also:supply the See also:fields and gardens of the plateau of Alazan, that See also:wheat, See also:millet and See also:maize are grown, and orchards, vineyards and mulberry plantations are possible . Lower down the valley cattle-breeding is the See also:chief source of See also:wealth, while in the small towns and villages of the former Georgian See also:kingdom various See also:petty trades, exhibiting a high development of See also:artistic See also:taste and technical skill, are widely diffused . The slopes of the Armenian highlands are clothed with See also:fine forests, and the See also:vine is grown at their See also:base, while on the wide-stretching steppes the Turko-Tatars pasture cattle, horses and See also:sheep, The lower part of the Kura valley assumes the See also:character of a dry steppe, the rainfall not reaching 14 in. annually at Baku, and it is still less in the Mugan steppe, though quite abundant in the adjacent region of See also:Lenkoran . The vegetation of the steppe is on the whole scanty . Trees are generally absent, except for thickets of poplars, See also:dwarf oaks and tamarisks along the course of the Kura, the delta of which is smothered under a See also:jungle of reeds and rushes . The Mugan steppe is, however, in spite of its dryness, a more fertile region in virtue of the irrigation practised ; but the Kura has excavated its See also:bed too deeply to admit of that being done along its course . The Lenkoran See also:district, sometimes called Talysh, on the western See also:side of the Kizil-Agach See also:bay, is blessed with a See also:rich vegetation, a fertile soil, and a moist See also:climate .

The inhabitants of the Kura valley consist principally of Iranian "fates and Talyshes, of Armenians and Lesghians, with Russians, See also:

Jews and See also:Arabs., This conjoint valley of the Rion-Kura was in remote antiquity the site of several See also:Greek colonial settlements, later the seat of successive kingdoms of the Georgians, and for centuries it has formed a See also:bulwark against hostile invasions from the south and east . It is still inhabited chiefly by Georgian tribes—Gurians, Imeretians, Mingrelians, Svanetians—in the See also:basin of the Rion, and by Georgians intermingled with Armenians in the valley of the Kura, while the steppes that stretch away from the lower course of the latter river are ranged over by Turko-Tatars . See also:Mingrelia and See also:Imeretia (valley of Rion) are the gardens of Caucasia, but the high valleys of See also:Svanetia, farther north on the south slopes of the Caucasus mountains, are See also:wild and difficult of See also:access . In the cultivated parts the See also:land is so exceedingly fertile and productive that it sells for almost fabulous prices, and its val,ue is still further enhanced by the See also:discovery of See also:manganese and See also:copper mines in the basin of the Rion, and of the almost inexhaustible supplies of See also:naphtha and See also:petroleum at Baku in the Apsheron See also:peninsula . The principal products of the soil are mentioned lower down, while the general character of the vegetation is indicated under CAUCASUS: Western Caucasus . In the basin of the Rion, in that of the Chorokh (which runs off the Pontic highlands into the Black Sea south of Batum), and on the Black Sea littoral from Batum northwards to Sukhum-kaleh, and beyond, the climate is extremely hot and the rainfall heavy (see under Climate below) . It is in this valley that the principal towns (except See also:Vladikavkaz at the north foot of the Caucasus) of Caucasia are situated, namely, Baku (179,133 inhabitants in 1900), Tiflis (160,649 in 1897), Kutais (32,492), and the two Black Sea ports of Batum (28,512) and See also:Poti (7666) . (iv.) The highlands of Armenia are sometimes designated the See also:Minor Caucasus, Little Caucasus and See also:Anti-Caucasus . But to use such terms for what is not only an See also:independent, but also an older, orographical formation than the Caucasus tends to perpetuate confusion in See also:geographical nomenclature . The Armenian highlands, which run generally parallel to the Caucasus, though at much lower elevations (5000-6000 ft.), are a plateau region, sometimes quite See also:flat, sometimes gently undulating, clothed with luxuriant meadows and mostly cultivable . From it rise See also:double or triple ranges connected by See also:cross-ridges and spined with See also:outer spurs . These double and triple ranges, which have a general See also:elevation of 8500-10,000 ft., stretch from the south-east See also:angle of the Black Sea, 400 M. south-eastwards to the Kara-dagh and Salavat mountains in north See also:Persia, and the latter See also:link them on to the See also:Elburz mountains that skirt the southern end of the Caspian Sea .

Various names are given to the different parts of the constituent ranges, or, perhaps more correctly, elongated See also:

groups of mountains . The Ajar, Akhalt-See also:sikh and Meskes or Trialety groups in the west are succeeded farther east by the Somkhet, Murguz, Ganji and Karabakh sections, forming the southern rim of the Kura basin, while parallel with them, but farther south, run the Mokry, Miskhan, Akmangan and Paltapin ranges, marking the northern edge of the Aras drainage area . These two sets of parallel ranges are linked together transversely by the cross-ridges of Bezobdal, Pambak, Shah-dagh and Gok-cha . From this last branches off the highest range in the entire See also:series, namely, the Zangezur, which soars up to 10,000 ft. above the left See also:bank of the Aras . From it again there shoot away at right angles, one on each side, the ranges of the See also:Dar-alagoz and Bergushet . These highlands exhibit very considerable evidences of volcanic activity both in remote See also:geological periods and also since the See also:Tertiary See also:epoch . Large areas are overlain with See also:trachyte, See also:basalt, See also:obsidian, See also:tuff and See also:pumice . The most conspicuous features of the entire region, See also:Mount Ararat (16,930 ft.) and Mount Alagoz (13,440 ft.), are both solid masses of trachyte; and both rise above the limits of perpetual snow . See also:Extinct volcanoes are numerous in several of the ranges, e.g . Akmangan, Mokry, Karabakh and Egri-dagh (see below) . It is in this region of the Armenian highlands that the largest lakes of Caucasia are situated, namely, the Gok-cha or Sevanga (540 sq. m. in area) at an altitude of 6340 ft., the Chaldir-gol (33 sq. m.) at 6520 ft., and several smaller ones, such as the gols of Khozapin, Khopchalu, Arpa, Toporavan and Tabiztskhur, all situated between 6500 and 7000 ft. above sea-level . The principal water-See also:divide in this highland region is, however, the range of Egri-dagh (Ararat), which just south of 4o° S. forms for too m. the boundary between See also:Russian and See also:Turkish Armenia, having Ararat at its eastern extremity and the extinct See also:volcano of Kessa-dagh (11,26o ft.) at its western .

Its importance lies in the fact that it divides the streams which flow into the Black Sea and Caspian from those which make their way into the See also:

Persian Gulf . The Egri-dagh possesses a sharply defined See also:crest, ranges at a general elevation of 8000 ft., is See also:bare of See also:timber, scantily supplied with water, and rugged and deeply fissured . The transverse water-parting between the Black Sea and the Caspian begins on the south side of the main range of the Caucasus, at Mount Zikara (12,56o ft.), a little south-west of See also:Kasbek, and runs south-west along the sinuous crests of the Racha, Suram or Meskes (3000-5000 ft.), Vakhan (1o,000-11,000 ft.), Arzyan (7000-10,000 ft.), and its continuation the Soganluk, thus linking the Caucasus ranges with those of the Armenian highlands . This line of heights separates the basins of the Chorokh and the Rion (Black Sea) from those of-the Aras and the Kura (Caspian Sea) . North of the Caucasus ranges the water-divide between these two seas descends from Mount Elbruz along the Sadyrlar Mountains (t 1,000 ft.), and finally sinks into the Stavropol " plateau " (1600 ft.) . But the main See also:axis of the transverse upheavals would appear to be continued in a north-eastern direction in the Andi and other parallel ranges of Daghestan, as stated under CAUCASUS . The population in this region consists principally of Armenians, Tatars, See also:Turks, Kurds, Ossetes, Greeks, with Persians, Tates and a few Russians (see particulars below) . Climate.—Owing in part to the See also:great See also:differences in altitude in different regions of Caucasia and in part to the directions in which the mountain ranges run, and consequently the quarters towards which their slopes See also:face, the climate varies very greatly according to locality . Generally speaking, it may be characterized as a climate of extremes on the Armenian highlands, in the Kura valley and in northern Caucasia, and as maritime and genial in Lenkoran, on the Black Sea coastlands, and in thevalley of the Rion . The greatest recorded range of temperature is at See also:Erivan (altitude 3230 ft.), namely, of 64° between a See also:January See also:average of 14.9° and an See also:August average of 78.8° F . At Sukhumkaleh, on the Black Sea, the corresponding range is only 27.3°, between a January average of 48.8° and an August average of 76.1° . The highest mean temperatures for the whole See also:year are those of Lenkoran (60.3°) and of Sukhum-kaleh and Poti (about 58°), and the lowest at Ardahan (5840 ft.), in the See also:province of See also:Kars, namely, 37'9°, and at Gudaur (7245 ft.), a few See also:miles south of Kasbek, namely, 38.6° .

The following table gives particulars of temperature averages at a few typical places: Place . Altitude . See also:

Annual January See also:July Mean . Mean . Mean . Stavropol 2030 47.00 24.00 70.0° Vladikavkaz 2345 47'3° 23'4° 68.o° Gudaur 7245 38.6° 20.3° 57.2° Baku on Caspian 58.o° 38.0° 80•o° Tiflis 1490 55 0° 32'0° 76'5° Batum on Black Sea 59.0° 42.0° 75.0° Sochi on Black Sea 56.3° 40.3° 76.1° Lenkoran on Caspian 60.3° 39.0° 8o•6° Erivan 3170 51•o° 15•o° 75.0° In respect of precipitation the entire region of Caucasia may be divided into two strikingly contrasted regions, a wet and a dry . To the former belong the Black Sea littoral, where the rainfall averages 59 to 93 in. annually, and the valleys that open upon it or are exposed to winds blowing off it, in which the rainfall varies, however, from 20 in . (Abbas-tuman, See also:Borzhom) to 6o (Kutais) . In Lenkoran also the rainfall averages 40 to 50 in. in the year . Between 16 and 4o in. fall as a See also:rule at the northern foot of the Caucasus (1blozdok, See also:Pyatigorsk) and in the Kura valley (Tiflis, Novo-bayazet) . On the Armenian highlands and on the steppes north of Pyatigorsk the rainfall is less than 12 in. annually, and even in some places less than 8 in., e.g. at the foot of Ararat . Most See also:rain falls at Batum and at Lenkoran in the autumn, in northern Caucasia and in See also:Transcaucasia in See also:spring and summer, but in the vicinity of the Sea of Azov in See also:winter .

See also:

Flora and See also:Fauna.—Plant-See also:life, in such a mountainous See also:country as Caucasia, being intimately dependent upon aspect and altitude, is treated under CAUCASUS . The wild animals of Caucasia are for the most part the same as those which frequent the mountainous parts of central Europe, though there is also an irruption of See also:Asiatic forms, e.g. the See also:tiger (in Lenkoran only), See also:panther, hyaena and See also:jackal . The more important of the carnivores which haunt the forests, valleys and mountain slopes are the See also:bear (Ursus arcios), See also:wolf, See also:lynx, wild See also:cat and See also:fox (Vulpes melanotus) . The wild See also:boar occurs around Borzhom . The See also:aurochs (See also:Bos urns) appears to exist still in the forests of the western Caucasus . Of See also:interest for sportsmen, as well as serving as See also:prey for the carnivores, are red See also:deer, goats (Capra pallasit and C. aegagrus), See also:chamois, See also:roebuck, moufflon (Ovis musimon), See also:argali or Asiatic wild sheep (O . See also:Ammon), another See also:species of sheep in O. gmelini, and See also:fallow deer (Capreolus pigargus) in northern Caucasus only . Rodents are numerous, the See also:mouse (See also:Mus sylvaticus) is very destructive, and beavers are met with in places . The birds of prey are the same as these of central Europe, and include the sea See also:eagle, alpine See also:vulture (Gyps fulvus), See also:buzzard, kites (Gypaelus barbalus and Milvus ater), See also:hawks (e.g . Astur See also:nisus) , goshawk (A. palumbarius), See also:fish-See also:hawk (Pandion haliaetus) and owls . Among the smaller birds may be enumerated finches, the See also:siskin, See also:bullfinch, See also:pipit, titmcuse, See also:wagtail, See also:lark, fine-crested See also:wren, hedge-See also:sparrow, See also:corn-wren, See also:nut-See also:hatch, See also:starling, See also:swallow, See also:martin, See also:swift, See also:thrush, See also:butcher See also:bird, See also:shrike, dipper, yellow-See also:hammer, See also:ortolan and a See also:warbler (Accentor alpinus) . The See also:game birds consist of See also:grouse, See also:blackcock, moorhen, See also:quail and See also:partridge .

The See also:

pheasant derives its name from the See also:ancient name (Phasis) of the Rion . In the seas and rivers about 190 species of fishes have been enumerated . Of these, 115 species are Mediterranean, 30 are See also:common to the Caspian Sea, and the remaining species are See also:peculiar to the Black Sea . The most useful economically are several species of See also:sturgeon and of See also:herring, See also:trout, See also:barbel, See also:chubb, See also:bream, See also:ray,sea-See also:dace, See also:carp, See also:anchovy . See also:Insects abound, especially See also:Coleoptera . Flies, lice, gadflies and mosquitoes are the worst of the See also:insect plagues . There are several See also:snakes, including the See also:viper (See also:Pelias berus) . See also:Ethnology.—The population of Caucasia is increasing rapidly . In 1897 it numbered 9,291,090, of whom 4,886,230 were See also:males and 4,404,867 were See also:females . The most densely-peopled provinces were Kutais and Tiflis, each with 8o inhabitants to the square mile; the thinnest the Black Sea government (2o2 per sq. m.), Terek (31), and Kars (39) . Of the See also:total population 3,725,543 lived in northern Caucasia and 5,564,547 m Transcaucasia (including Daghestan) . In the latter territorial division there exists a great disproportion between the sexes, namely, to every zoo males only 86 females; indeed in the Black Sea government there are only 65•.5 females to every loo males .

Phoenix-squares

Ethnologically the population belongs to a great variety of races . The older authorities asserted that these numbered as many as 'so, or even 300; the more See also:

recent researches of See also:Baron P . V . Uslar, F . Anton, von See also:Schiefner, Zagursky, and others have greatly reduced this number; but even then there are not less than fifty represented . According to the See also:languages spoken the populations of Caucasia admit of being classified as follows,1 according to Senator N . Trointsky, See also:president of the Russian See also:Census See also:Committee for 1897 . See also:ARYANS 4,901,412 Slays 3,183,870 Great Russians . 1,829,793 Little Russians . . 1,305,463 See also:White Russians 19,642 Poles . 25,117 Germans 47,391 Greeks _ 100,299 Rumanians 7,232 See also:French and Italians 1,435 See also:Lithuanians . 6,687 Lithuanians proper 5,121 Letts .

1,511 Iranians 315,695 Persians 13,929 Talyshes 34,994 Tates . 95,056 Ossetes 171,716 Kurds 99,836 Armenians 1,116,461 Gypsies . 3,041 SEMITES 46,739 Jews 40,498 Chaldaeans (Aisors) 5,353 URAL-ALTAIANS I,902,142 Finns . 7,432 Esthonians . 4,281 Turko-Tatars 1,879,908 Tatars • 1,509,785 Osmanli Turks . 139,419 Nogai Tatars 64,048 Turkomans 24,522 See also:

Bashkirs 953 See also:Chuvashes 411 See also:Kirghiz 98 Sarts 158 Karachais 27,222 See also:Kumyks 83,408 Kara-papaks 29,902 Kalmucks 14,409 CAUCASIANS 2,439,071 Georgians (including Imeretians, Gur- ians, Svanetians, Lazes, Mingrel- ians, &c.) 1,352,455 Circassians Cherkesses (Adigheh) and Kabardians . Abkhasians . . 72,103 Chechens 274,318 Chechens proper 226,496 Ingushes2 47,409 Kistines 413 1 Premier Recensement general de la population de l'See also:empire de Russie, ed . N . Trointsky (St See also:Petersburg, 1905, 2 vols.), in Russian and French . 2 Although the Ingushes speak a Chechen See also:dialect, they have recently been proved to be, anthropologically, quite a distinct See also:race . See also:Religion.—Most of the Russians and the Georgians belong to the Orthodox Greek See also:Church (over 4,000,000 in all); but considerable See also:numbers (estimated at nearly 122,000, though in reality probably a See also:good many more) are Nonconformists of different denominations .

The Georgian Lazes are, however, Mussulmans . The Armenians are Christians, mostly of the See also:

national Gregorian Church (979,566), though 34,000 are See also:Roman Catholics . The Caucasian races (except the Gregorians), together with the Turks and Tatars, are Mussulmans of the Sunnite See also:sect (2,021,300), and the Iranian races mostly Mussulmans of the Shiite sect (884,100) . The Kalmucks and other Mongolic tribes are Lamaists (20,300), and some of the Kurds profess the. peculiar tenets of the Yezids . See also:Industries.—The principal occupation of the settled inhabitants is See also:agriculture and of the nomadic the breeding of live stock, including camels . The cultivation of the soil is, however, attended in many parts with great difficulties owing to the scanty rainfall and the very See also:primitive implements still in use, and in the valley of the Kura heavy losses are frequently incurred from depredations by locusts . But where irrigation is employed the yield of crops is excellent . See also:Rye and wheat are the most important crops harvested in northern Caucasia, but oats, barley and maize are also cultivated, whereas in Transcaucasia the principal crops are maize, See also:rice See also:tobacco and See also:cotton . The rice is grown chiefly in the valley of the Kura and in Lenkoran; the tobacco in the Rion valley and on the Black Sea coastlands, also to some extent in Kuban; and the cotton in the eastern provinces . Various kinds of See also:fodder crops are grown in Transcaucasia, such as See also:hay, rye-grass and See also:lucerne . It is estimated that nearly 54,000 acres are under vineyards in northern Caucasia and some 278,000 acres in Transcaucasia, the aggregate yield of See also:wine being 30 million gallons annually . The best wine grows in Kakhetia, a district lying north-east and east of Tiflis; this district alone yields nearly 8 million gallons annually .

Large numbers of mulberry trees are planted for rearing silkworms, especially in Kutais, Erivan, Elisavetpol (See also:

Nukha) and Baku (See also:Shemakha); the groves occupy nearly 150,000 acres, and the winding of the See also:silk gives employment to large numbers of the population . Melons and water-melons are also important See also:objects of cultivation . Sunflowers are very extensively grown for oil in the government of Kuban and elsewhere, and also some See also:flax . See also:Liquorice is an See also:article of export . Many varieties of See also:fruit are grown, especially good being the apricots, peaches, walnuts and See also:hazel nuts . A limited area (not more than 115o acres) of the Black Sea See also:coast between Sukhum-kaleh and Batum is planted with the See also:tea-See also:shrub, which succeeds very well . In the same district bamboos, See also:ramie-fibre and See also:attar (See also:otto) of See also:roses are cultivated . The See also:mining See also:industry is growing rapidly in importance in spite of costly and deficient means of communication, want of See also:capital, and lack of general initiative . So far the principal developments of the industry have been in the governments of Kutais, Batum, Elisavetpol and Kuban . Copper ore is extracted above the Murgul river (some 30 M. south of Batum), at Akhtala south of Tiflis, and at Kedabek in Elisavetpol; manganese to a consider-ably greater extent (over 400,000 tons annually) at Chiaturi in the Kvirila valley in Kutais . See also:Steam See also:coal of good quality is reported to exist about 30 M. inland from the open roadstead of Ochemchiri in Kutais, but it is not See also:mined . About 50,000 tons of coal of very poor quality are, however, extracted annually, and the same quantity of See also:salt in the Armenian highlands and in Kuban .

Small quantities of quicksilver, See also:

sulphur and See also:iron are obtained . But all these are insignificant in comparison with the See also:mineral oil industry of Baku, which in normal times yields annually between ten and eleven million tons of crude oil (naphtha) . A good See also:deal of this is transported by See also:
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