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See also:BALKASH, or BALKHASH (called by the See also:Kirghiz Ak-denghiz or See also:Ala-denghiz and by the See also:Chinese Si-See also:hai) , a See also:lake of See also:Asiatic See also:Russia, in the See also:Kirghiz See also:steppes, between the governments of See also:Semipalatinsk and See also:Semiryechensk, in 450 to 470 N. and 730 30' to 79° E., about 600 m. to the See also:east of Lake See also:Aral . It is See also:fourth in See also:size of the lakes in Eurasia, having an See also:area of 7115 sq. m., and lies at an See also:altitude of goo ft . It has the shape of a broad See also:crescent, about 430 M. See also:long from W.S.W. to E.N.E., having its See also:concave See also:side turned southwards; its width varies from 36 to 53 M . Its See also:north-western See also:shore is bordered by a dreary See also:plateau, known as the See also:Famine See also:Steppe (See also:Bek-pak-dala) . The See also:south-east shore, on the contrary, is See also:low, and bears traces of having extended formerly as far as the Sasyk-kul and the See also:Ala-kul . The Kirghiz in 1903 declared that its See also:surface had been rising steadily during the preceding ten years, though See also:prior to that it was dropping . The See also:chief feeder of the lake is the See also:Ili, which rises in the Khantengri See also:group of the Tian-shan Mountains . The Karatal, the See also:Aksu and the Lepsa also enter from the south-east, and the Ayaguz from the north-east . The first three See also:rivers make their way with difficulty through the sands and reeds, which at a quite See also:recent See also:time were covered by the lake . Although it has no outlet, its See also:waters are relatively fresh . It freezes generally from See also:November to See also:April . Its greatest See also:depth, 35 ft., is along the north-See also:west shore . The See also:fauna of the lake and of its tributaries —explored by Nikolsky—is more akin to the fauna of the rivers of the See also:Tarim See also:basin than to that of the Aral; it also does not contain the See also:common See also:frog . It seems, therefore, probable that Lake See also:Balkash stood formerly in communication through lakes Ebi-nor and Ayar (Telli-nor) with the lake that formerly filled the Lukchun depression (in 891° E. long. and 422° N. See also:lat.), but researches show that a connexion with Lake Aral—at least in recent times—was improbable . The lake has been investigated by L . S . See also:Berg (see Petermanns Mitteilungen, 1903) . |
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