Online Encyclopedia

KARAKORUM (Turkish, " black stone deb...

Online Encyclopedia
Originally appearing in Volume V15, Page 676 of the 1911 Encyclopedia Britannica.
Spread the word: del.icio.us del.icio.us it!

KARAKORUM (
See also:
Turkish, " black stone debris ")
  , the name of two cities in
See also:
Mongolia . One of these, according to G . Potanin, was the capital of the Uighur
See also:
kingdom in the 8th century, and the other was in the 13th century a capital of the steppe 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 south-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 stone bearing a description of his victories . (2) The Mongolian KARAKORUM was founded at the birth of the Mongolian monarchy established by Jenghiz Khan . A palace for the khan was built in it by Chinese architects in 1234, and its walls were erected in 1235 . Plano Carpini visited it in 1246, Rubruquis in 1253, and Marco Polo in 1275 . Later, the
See also:
fourth Mongolian king, Kublai, left Karakorum, in order to reside at Kai-pin-fu, near Peking . When the khan Arik-bog declared himself and Karakorum
See also:
independent of Kublai-Khan, the latter besieged Karakorum, took it by 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 . 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 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 . North and north-east of the monastery are ruins of ancient buildings . Professor D . Pozdneev, who visited Erdeni Tsu for a second 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 Helsingfors Ugro-Finnish society (189o) and the Russian 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 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 . 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 Turkestan, in the province of Ferghana, and on the Pamir 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 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-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 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 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 sand . There are broad expanses (takyrs) of 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 salt and
See also:
gypsum, and relieved only by Solanaceae along their
See also:
borders . The 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 side, 3o° to 4o° steep, on the opposite slope . They are disposed in 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 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 flowers (e.g. tulips, Rheum, various
See also:
Umbelliferae), which are soon burned by the sun; they cover very large spaces in the south-east . (4) Sands disposed in waves from 50 to 70 ft., and occasionally up to 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 rivers or depressions which contained elongated salt lakes . Water is only found in 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 . A .

K . ; J . T .

End of Article: KARAKORUM (Turkish, " black stone debris ")
[back]
VUK STEFANOVICH KARAJICH (1787-1864)
[next]
KARAMAN (anc. Laranda, a name still used by the Chr...

Additional information and Comments

There are no comments yet for this article.
» Add information or comments to this article.
Please link directly to this article:
Highlight the code below, right click and select "copy." Paste it into a website, email, or other HTML document.