Baksan (river)

The Baksan[lower-alpha 1] (/bɑːkˈsɑːn/) is a river in Kabardino-Balkaria in Russia. It flows east northeast and joins the Malka just before that river joins the northwest bend of the Terek. The Baksan is 169 kilometres (105 mi) long, with a drainage basin of 6,800 square kilometres (2,600 sq mi).[1]

Baksan
Baksan (river) is located in Kabardino-Balkaria
Baksan (river)
Baksan mouth location
Baksan (river) is located in Caucasus mountains
Baksan (river)
Baksan (river) (Caucasus mountains)
Location
CountryKabardino-Balkaria (Russia)
Physical characteristics
SourceLateral Range
Mount Elbrus
  locationGreater Caucasus
MouthMalka
  coordinates
43.7331°N 44.0633°E / 43.7331; 44.0633
Length169 km (105 mi)
Basin size6,800 km2 (2,600 sq mi)
Basin features
ProgressionMalkaTerekCaspian Sea

Course

The Baksan River is a 169 km long river with a catchment area of 6800 km². It originates from the glaciers Azau Bolshoi and Azau Maly in the Elbrus region and its food source is mainly glacial, snow and underground. The river experiences high water levels during July and August.

The Baksan River has several notable tributaries, the largest of which are the Cherek and Chegem rivers, which merge into the Baksan just upstream from its confluence with the Malka River. In the upper reaches of the Baksan and its tributaries, there are several climbing camps such as Baksan, Dzhan-Tuugan, and Elbrus, as well as the Elbrus National Park and the Terskol Observatory.

The cities of Tyrnyauz and Baksan are located along the Baksan River, while the city of Prokhladny lies opposite the point where it meets the Malka River. In the lower reaches, the Baksan is used for irrigation purposes and has a hydroelectric power station built on it, known as the Baksan Hydroelectric Power Station.

The Baksan River also has an increased level of contamination.

Notes

  1. Russian: Баксан, pronounced [bɐkˈsan]; Kabardian: Бэхъсэн, romanized: Bexsen, pronounced [bɜχˈsɜn]; Karachay-Balkar: Басхан, romanized: Bashan, pronounced [bɑsˈχɑn]

References


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