, LakeA shallow lake of southeast Kazakhstan. It has saline water in the east and fresh water in the west.
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, Lake
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| Lake Balkhash Балқаш Көлі |
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|---|---|
| From space, April 1991 | |
| Location | Kazakhstan |
| Coordinates | 46°32′27″N 74°52′44″E / 46.54083°N 74.87889°ECoordinates: 46°32′27″N 74°52′44″E / 46.54083°N 74.87889°E |
| Lake type | Endorheic, Saline |
| Primary inflows | Ili, Karatal, Aksu, Lepsi, Byan, Kapal, Koksu rivers |
| Primary outflows | evaporation |
| Basin countries | Kazakhstan 85% China 15% |
| Max. length | 605 km (376 mi) |
| Max. width | East 74 km (46 mi) West 19 km (12 mi) |
| Average depth | 5.8 m (19 ft) |
| Max. depth | 26 m (85 ft) |
| Water volume | 106 cu mi (440 km3) |
| Surface elevation | 341.4 m (1,120 ft) |
| Frozen | November to March |
Lake Balkhash (Kazakh: Балқаш Көлі, Balqaş köli; Russian: Озеро Балхаш, Ozero Balkhash) is a lake in southeastern Kazakhstan,presently the largest in Central Asia (after the drying of most of Aral Sea).[1] It is a closed basin that is part of the endorheic basin that includes the Caspian and Aral seas.
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From as early as 103 BC up until the 8th century, the Balkhash polity was known to the Chinese as Pu-Ku/Bu-Ku. From the 8th century on, the land to the south of the lake, between it and the Tian Shan mountains, was known as "Seven Rivers" (Jetisu in Turkic, Semirechye in Russian). It was a land where the nomadic Turks and Mongols of the steppe mingled cultures with the settled peoples of Central Asia.[2] During China's Qing Dynasty (1644 - 1911), the lake formed the northwestern-most boundary of the Empire. In 1864, the lake and its neighbouring area was ceded to Imperial Russia through the Sino-Russian Treaty. With the dissolution of the Soviet Union in 1991, the lake became part of Kazakhstan.
The lake currently covers 16,996 km2 (6,562 sq mi), but, like the Aral Sea, it is shrinking because of the diversion of water from the rivers that feed it.[3] The lake has a mean depth of 5.8 metres (19 ft), and a maximum of 25.6 metres (84 ft). The western half of the lake is fresh water, while the eastern half is saline.[4] The mean depth of the eastern part is 1.7 times that of the western. Approximately 1,600 km (990 mi) to the northeast lies Lake Baikal, the largest lake on Earth by volume.
The Balkhash inland basin drains into Lake Balkhash via seven rivers; chief among these is the Ili River, which brings the majority of the riparian inflow, others such as the Karatal provide both surface and subsurface flow. The Ili is fed from precipitation (largely vernal snowmelt) from the mountains of China's Xinjiang region. The Balkhash basin is itself endorheic – there is no outflow – and Balkhash suffers from the same problems as other endorheic lakes.
The waters of the Ili River and of Lake Balkhash are of vital economic importance to Kazakhstan. The Ili is dammed for hydroelectric power at Kapchagay, and the river waters are heavily diverted for agricultural irrigation and for industrial purposes. Balkhash itself serves as a vital fishery.
As the population and degree of industrialisation in western China increase, it is likely that conflict between China and Kazakhstan over the fate of the limited waters of the Ili will intensify. Similar international disputes over water use in the arid region led to the desiccation of the Aral Sea, and Balkhash appears to be following a similar path.[5]
The water pollution of Balkhash is intensified as urbanisation and industrialisation in the area grow rapidly. Extinctions of species in the lake due to its decreasing area, as well as overfishing activities, are cause for alarm among conservationist organisations worldwide.[6]
| Wikisource has the text of the 1911 Encyclopædia Britannica article Balkash. |
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| Balqash, Lake | |
| Ili (river) | |
| Central Asia |
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