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KARAKORUM ( See also: Mongolia
.
One of these, according to G
.
Potanin, was the capital of the See also: Uighur See also: kingdom in the 8th century, and the other was in the 13th century a capital of the 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 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 Khan
.
A 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 Polo in 1275
.
Later, the See also: fourth Mongolian See also: king, Kublai, left Karakorum, in
See also: order to reside at Kai-pin-fu, near See also: Peking
.
When the khan Arik-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 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 (" black city ") or Khara-kherem (" black See also: wall "), of which only the wall and a 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 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
.
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 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 map
.
Campbell's report was printed as a
See also: parliamentary 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 province of See also: Ferghana, and on the Pamir See also: plateau
.
Great) Kara-kul, 12 M. long and 10 m. wide (formerly much larger), is under 39° N., to the south of the Trans-Alai range, and lies at an 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 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
.
Little Kara-kul lies in the north-east Pamir, or Sarikol, north- west of the Mustagh-ataSee 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 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 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 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 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 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 rain-water retained in the See also: lower parts of the takyrs
.
The population of the Kara-kum, consisting of 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
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A
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K . ; J . T . |
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