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KARAKORUM (Turkish, " black stone deb...

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Originally appearing in Volume V15, Page 676 of the 1911 Encyclopedia Britannica.
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KARAKORUM (See also:Turkish, " See also:black See also:stone debris ")  , the name of two cities in See also:Mongolia . One of these, according to G . Potanin, was the See also:capital of the See also:Uighur See also:kingdom in the 8th See also:century, and the other was in the 13th century a capital of the See also:steppe See also:monarchy of Mongolia . The same name seems also to have been applied to the Khangai range at the headwaters of the Orkhon . (1) The Uighur See also:KARAKORUM, also named Mubalik (" See also:bad See also:town "), was situated on the See also:left See also:bank of the Orkhon, in the Talal-khain-dala steppe, to the See also:south-See also:east of Ughei-nor . It was deserted after the fall of the Uighur kingdom, and in the loth century Abaki, the founder of the Khitan kingdom, planted on its ruins a See also:stone bearing a description of his victories . (2) The Mongolian KARAKORUM was founded at the See also:birth of the Mongolian monarchy established by Jenghiz See also:Khan . A See also:palace for the khan was built in it by See also:Chinese architects in 1234, and its walls were erected in 1235 . Plano See also:Carpini visited it in 1246, See also:Rubruquis in 1253, and Marco See also:Polo in 1275 . Later, the See also:fourth Mongolian See also:king, Kublai, left Karakorum, in See also:order to reside at Kai-See also:pin-fu, near See also:Peking . When the khan Arik-See also:bog declared himself and Karakorum See also:independent of Kublai-Khan, the latter besieged Karakorum, took it by See also:famine, and probably laid it See also:waste so thoroughly that the town was afterwards forgotten . The exact sites of the two Mongolian capitals were only established in 1889-1891 .

See also:

Sir H . See also:Yule (The See also:Book of Marco Polo, 1871) was the first to distinguish two cities of this name . The See also:Russian traveller Paderin in 1871 visited the Uighur capital (see Tunics), named now by the See also:Mongols Kara Balghasun (" See also:black See also:city ") or Khara-kherem (" black See also:wall "), of which only the wall and a See also:tower are in existence, while the streets and ruins outside the wall are seen at a distance of 14 m . Paderin's belief that this was the old Mongol capital has been shown to be incorrect . As to the Mongolian Karakorum, it is identified by several authorities with a site on which towards the See also:close of the 16th century the Buddhist monastery of Erdeni Tsu was built . This monastery lies about 25 M. south by east of the Uighur capital . See also:North and north-east of the monastery are ruins of See also:ancient buildings . See also:Professor D . Pozdneev, who visited Erdeni Tsu for a second See also:time in 1892, stated that the earthen wall surrounding the monastery might well be See also:part of the wall of the old city . The proper position of the two Karakorums was determined by the expedition of N . Yadrintsev in 1889, and the two expeditions of the See also:Helsingfors Ugro-Finnish society (189o) and the Russian See also:academy of See also:science, under Dr W . Radlov (1891), which were sent out to study Yadrintsev's See also:discovery .

See See also:

Works (Trudy) of the Orkhon Expedition (St See also:Petersburg, 1892) ; Yule's Marco Polo, edition revised by See also:Henri Cordier (of See also:Paris), vol. i. ch. xlvi . (See also:London, 1903) . Cordier confines the use of Karakorum to the Mongol capital; Pozdneev, Mongolia and the Mongols, vol. i . (St Petersburg, 1896) ; C . W . See also:Campbell, " Journeys in Mongolia," Geog . Journ. vol. xx . (1903), with See also:map . Campbell's See also:report was printed as a See also:parliamentary See also:paper (See also:China No. z, z9o4) . KARA-KUL, the name of two lakes (" See also:Great " and " Little ") of Russian See also:Turkestan, in the See also:province of See also:Ferghana, and on the Pamir See also:plateau . Great) Kara-kul, 12 M. See also:long and 10 m. wide (formerly much larger), is under 39° N., to the south of the Trans-Alai range, and lies at an See also:altitude of 13,200 ft.; it is surrounded by high mountains, and is reached from the north over the Kyzyl-See also:art pass (14,015 ft.) . A See also:peninsula projecting from the south See also:shore and an See also:island off the north shore See also:divide it into two basins, a smaller eastern one which is shallow, 42 to 63 ft:, and a larger western one, which has depths of 726 to 756 ft: It has no drainage outlet .

Phoenix-squares

Little Kara-kul lies in the north-east Pamir, or Sarikol, north-See also:

west of the Mustagh-ata See also:peak (25,850 ft.), at an altitude of 12,700 ft . It varies in See also:depth from 79 ft. in the south to 50 to 70 ft. in the See also:middle, and loon ft, or more in the north . It is a See also:moraine See also:lake; and a stream of the same name flows through it, but is named Ghez in its farther course towards See also:Kashgar in East Turkestan . KARA-See also:KUM ("Black Sands "), a See also:flat See also:desert in Russian Central See also:Asia . It extends to nearly ' 1o,000 sq. m., and is bounded on the N.W. by the Ust-urt plateau, between the See also:Sea of See also:Aral and the See also:Caspian Sea, on the N.E. by the Amu-darya, on the S. by the See also:Turkoman oases, and on the W. it nearly reaches the Caspian Sea . Only part of this See also:surface is covered with See also:sand . There are broad expanses (takyrs) of See also:clay See also:soil upon which See also:water accumulates in the See also:spring; in the summer these are muddy, but later quite dry, and merely a few See also:Solanaceae and bushes grow on them . There is also shor, similar to the above but encrusted with See also:salt and See also:gypsum, and relieved only by Solanaceae along their See also:borders . The See also:remainder is occupied with sand, which, according to V . Mainov, assumes five different forms . (1) Barkhans, chiefly in the east, which are mounds of loose sand, 15 to 35 ft. high, hoof-shaped, having their gently sloping See also:convex sides turned towards the prevailing winds, and a See also:concave See also:side, 3o° to 4o° steep, on the opposite slope . They are disposed in See also:groups or chains, and the winds drive them at an See also:average See also:rate of 20 ft. annually towards the south and south-east .

Some grass (Stipa pennata) and bushes of saksaul (Haloxylon ammodendron) and other steppe bushes (e.g . Calligonium, Halimodendron and Atraphaxis) grow on them . (2) Mounds of sand, of about the same See also:

size, but irregular in shape and of a slightly firmer consistence, mostly bearing the same bushes, and also See also:Artemisia and Tamarix; they are chiefly met with in the east and south . (3) A sandy desert, slightly undulating, and covered in spring'with grass and See also:flowers (e.g. tulips, Rheum, various See also:Umbelliferae), which are soon burned by the See also:sun; they See also:cover very large spaces in the south-east . (4) Sands disposed in waves from 50 to 70 ft., and occasionally up to See also:loo ft. high, at a distance of from 200 to 400 ft. from each other; they cover the central portion, and their vegetation is practically the same as in the preceding See also:division . (5) See also:Dunes on the shores of the Caspian, composed of moving sands, 35 to 8o ft. high and devoid of vegetation . A typical feature of the Kara-kum is the number of " old See also:river beds," which may have been either channels of tributaries of the Amu and other See also:rivers or depressions which contained elongated salt lakes . Water is only found in See also:wells, to to 20 M. apart—sometimes as much as loo m.—which are dug in the takyrs and give saline water, occasionally unfit to drink, and in pools of See also:rain-water retained in the See also:lower parts of the takyrs . The See also:population of the Kara-kum, consisting of See also:nomad See also:Kirghiz and Turkomans, is very small . The region in the north of the province of Syr-darya, between Lake Aral and Lake Chalkarteniz, is also called Kara-kum . (P . A .

K . ; J . T .

End of Article: KARAKORUM (Turkish, " black stone debris ")
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