Karasor Basin Explained

Karasor Basin
Other Name:Қарасор ойысы
Type:Depression
Coordinates:49.88°N 75.38°W
Area:ca
Length:ca
Width:ca
Part Of:Kazakh Uplands
Elevation:ca
Map:Kazakhstan
Relief:Yes
Location:Karaganda Region, Kazakhstan

The Karasor Basin (Kazakh: Қарасор ойысы; Russian: Карасорская впадина) or Karasor Depression, is a depression in Karkaraly District, Karaganda Region, Kazakhstan.[1] [2]

The Karasor Basin includes a 37286ha Important Bird Area.[3]

Geography

The Karasor Depression is an endorheic basin in the Kazakh Uplands. It extends roughly from east to west for a length of approximately to the southeast of the Ayr and Zheltau ranges, and north of the Karkaraly Range and the Kyzyltas. Fourteen rivers flow into the basin, the largest of which are the 159km (99miles) long Taldy and the 156km (97miles) long Zharly. The Karasor Basin is covered in snow approximately between October and April every year. Most rivers and rivulets flow only following the melting of the snows, breaking up into disconnected pools or drying out completely during the summer.[4]

Karasor, the largest lake, lies in a central position at the bottom of the depression. There are three other major lakes in the basin, Saumalkol, Katynkol and Balyktykol, as well as numerous smaller lakes and sors. The water of all the lakes is saline; Saumalkol in the west is a dead lake, having the highest salt concentration, while Balyktykol has the lowest. The salinity of Karasor and Taldykol exceeds the values of average sea water. Parts of the depressions between the surrounding hills are occupied by salt pans.[3] [1]

Ancient lake

Karasor was a much larger lake in the past. There are traces of high water levels reaching in the banks of Karasor and adjacent Saumalkol and Katynkol lakes, indicating that the former extension of lake Karasor reached —about five times larger, with a depth between and —almost five times deeper. At that time the water of river Nura reached the ancient lake from the west.[2] [5] [4]

Flora and fauna

The landscape of the basin area is hilly steppe,. There are plowed agricultural fields with clayey and loamy soils. The vegetation in the basin includes spear grass, wormwood, Siberian peashrub, Neotrinia splendens and fescue.[6] [7] [3] [8]

See also

Notes and References

  1. [Google Earth]
  2. Jilili Abuduwaili, Gulnura Issanova, Galymzhan Saparov. Hydrology and Limnology of Central Asia, Springer, Berlin 2019,
  3. Web site: Karasor Lake - BirdLife Data Zone . 2024-03-29 . 2024-03-29 . https://web.archive.org/web/20240329045312/https://datazone.birdlife.org/site/factsheet/karasor-lake-iba-kazakhstan . live .
  4. Web site: L-42 Topographic Chart (in Russian) . 29 March 2024 . 8 October 2023 . https://web.archive.org/web/20231008005938/https://maps.vlasenko.net/smtm1000/n-41.jpg . live .
  5. Kazakhstan National Encyclopedia / Ch. ed. B.O. Jakyp. — Almaty: «Kazakh encyclopedia» ZhSS, 2011. (T.Z.),
  6. Jilili Abuduwaili, Gulnura Issanova, Galymzhan Saparov, Hydrology and Limnology of Central Asia. pp. 177-181
  7. Web site: News of the National Academy of Sciences of the Republic of Kazakhstan . 2024-03-31 . 2023-05-22 . https://web.archive.org/web/20230522052453/http://soc-human.kz/images/o20195/039_234-239.pdf . live .
  8. Gel dyyeva G.V. 1974: Landscapes of the Karasor Basin, central Kazakhstan. Voprosy Geografii Kazakhstana 16, Geografiya prirodnykh resursov Kazakhstana): 51