In today's world, Aralsor has become an increasingly relevant topic of interest. With a significant impact on various aspects of society, Aralsor has generated extensive debate and interest in different sectors. From its influence on the economy to its impact on health, Aralsor is a topic that has been the subject of study and analysis by experts and academics around the world. With the aim of clarifying and deepening the understanding of Aralsor, this article will address the different aspects related to this topic, in order to provide a broad and detailed vision of its importance and impact today.
Aralsor | |
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Аралсор | |
![]() Sentinel-2 image of Aralsor in 2024 | |
Location | Caspian Lowland |
Coordinates | 49°04′N 48°11′E / 49.067°N 48.183°E |
Type | endorheic |
Primary inflows | Ashchyozek |
Basin countries | Kazakhstan |
Max. length | 34.3 kilometers (21.3 mi) |
Max. width | 13 kilometers (8.1 mi) |
Surface area | 124 square kilometers (48 sq mi) to 200 square kilometers (77 sq mi) |
Surface elevation | 1.6 meters (5 ft 3 in) |
Aralsor (Kazakh: Аралсор; Russian: Аралсор) is a bittern salt lake group in Bokey Orda District, West Kazakhstan Region, Kazakhstan.[1]
The lake lies about 80 kilometers (50 mi) to the east of the Russian border, north of the R-97 Highway (Kazakhstan). The road connects Saykyn station of the Volga Railway near lake Botkul with the village of Taipak on the right bank of the Ural River.[2] Salt extraction on an industrial scale is carried out at the lake.[3]
Lying at the northern edge of the Ryn Desert, east of the Russian border, Aralsor is an endorheic lake group. The main water body is colored pink and is surrounded by a string of smaller lakes and salt pans.[4] The latter contain clay salt-mud deposits covered with a crust of halite reaching 0.3 meters (1 ft 0 in). The western and eastern banks of Aralsor are steep and cliff-like in places.[3]
Flowing from the north, the Ashchyozek is the main river in the area. A short channel connects the end of the river with Aralsor. This channel is periodically dry. The Kamys-Samar Lakes lie to the east.[2][3]
There is desert and steppe vegetation in the terraced flat areas of the Aralsor lakeside cliff-like formations. In the ravines of the shoreline cliffs there are plants such as tamarisk, anabasis, Halocnemum and winterfat, providing a habitat and breeding ground for the local fauna of small mammals, birds and reptiles.[5]