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Lake Manych-Gudilo

Saltwater lake in Kalmykia, Russia From Wikipedia, the free encyclopedia

Lake Manych-Gudilo (Russian: Ма́ныч-Гуди́ло) is a large saltwater reservoir lake in Kalmykia, Russia. Part of the lake lies also in Rostov Oblast and Stavropol Krai. It has an area of about 344 km2 and average depth of only about 0.6 m.[3]

LocationKalmykia
Coordinates46°20′09″N 42°47′58″E
Quick facts Location, Coordinates ...
Lake Manych-Gudilo
Lake Manych Gudilo coastline
Lake Manych-Gudilo is located in Kalmykia
Lake Manych-Gudilo
Lake Manych-Gudilo
Location within Kalmykia
Lake Manych-Gudilo is located in Rostov Oblast
Lake Manych-Gudilo
Lake Manych-Gudilo
Location within Rostov Oblast
Lake Manych-Gudilo is located in Stavropol Krai
Lake Manych-Gudilo
Lake Manych-Gudilo
Location within Stavropol Krai
Lake Manych-Gudilo is located in European Russia
Lake Manych-Gudilo
Lake Manych-Gudilo
Location within European Russia
LocationKalmykia
Coordinates46°20′09″N 42°47′58″E
Lake typeSaline
Sea of Azov (via the West Manych River)
Basin countriesRussia
344 km2 (133 sq mi)
Average depth
0.6 m (2 ft 0 in)
Max. depth2.2 m (7 ft 3 in)
Surface elevation
8 m (26 ft)[1]
Official name
Lake Manych-Gudilo
Designated13 September 1994
Reference no.673[2]
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Lake Manych-Gudilo is the source of the West Manych River, which flows north-west, through a number of reservoirs, falling into the lower Don a short distance upstream from Rostov-on-Don and the Don's fall into the Sea of Azov.[4]

Temperatures in the region through the year can range from −30 °C (−22 °F) in winter to 40 °C (104 °F) in summer. The area is also home to many species of birds and is the site of the Chernye Zemli Biosphere Reserve.[5][6][7]

Manych-Gudilo as seen from space

A global sea level rise of roughly 25 metres (80 ft) would cause the ocean surface to be higher than the highest point of an area between the ocean and the Caspian, forming a narrow channel straddling the lake in the area between the Sea of Azov and the Caspian Sea, potentially placing the Caspian Depression area underwater.[8][9]

See also

Further reading

  • Yanko-Hombach, Valentina (2006). Allan S. Gilbert, Nicolae Panin and Pavel M. Dolukhanov (ed.). The Black Sea Flood Question. Springer. p. 999. ISBN 978-1402047749.

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