In the world of Kypshak, there is a wide range of perspectives, opinions and knowledge that fuel the constant debate and exchange of ideas. For decades, Kypshak has been the object of study, analysis and reflection by academics, experts, enthusiasts and the curious. Its impact on society, culture, science and technology has been undeniable, and its relevance continues to constantly evolve. In this article, we will explore the various facets of Kypshak, providing a detailed analysis and comprehensive view that allows us to better understand its importance and influence in our contemporary world.
Kypshak | |
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Қыпшақ / Әжібайсор | |
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Location | Kazakh Uplands |
Coordinates | 50°08′N 68°23′E / 50.133°N 68.383°E |
Type | endorheic |
Primary inflows | Kypshak, Akkoshkar |
Primary outflows | none |
Catchment area | 3,151 square kilometers (1,217 sq mi) |
Basin countries | Kazakhstan |
Max. length | 10.5 kilometers (6.5 mi) |
Max. width | 8.5 kilometers (5.3 mi) |
Surface area | 64.7 square kilometers (25.0 sq mi) |
Shore length1 | 37.2 kilometers (23.1 mi) |
Surface elevation | 318.9 meters (1,046 ft) |
Islands | none |
1 Shore length is not a well-defined measure. |
Kypshak (Kazakh: Қыпшақ), also known as Azhibeksor (Kazakh: Әжібайсор; Russian: Ажибексор),[1][2] is a salt lake in Nura District, Karaganda Region, Kazakhstan.[3][4]
In the 1930s Kypshak dried up and turned into a salt pan,[5] but in the following decades it filled up once more and on the USSR topographic map of 1989 it was marked again as a lake.[4]
Kypshak is a roughly triangular-shaped lake that lies at 318.9 meters (1,046 ft) above sea level. It is located 23 kilometers (14 mi) to the southwest of Lake Tengiz and 12 kilometers (7.5 mi) to the west of lake Kerey.[6] It is an endorheic lake, having no outflow. 111 kilometers (69 mi) long river Kypshak flows into the lake from the northwest, and smaller river Akkoshkar from the west.[3]