Katun (river)
The Katun (Russian: Катунь [kɐˈtunʲ]; Altay: Кадын [qɑˈdɯn]) is a river in the Altai Republic and the Altai Krai of Russia. It forms the Ob as it joins the Biya some 19 kilometres (12 mi) southwest of Biysk. The Katun is 688 kilometres (428 mi) long, and its drainage basin covers 60,900 square kilometres (23,500 sq mi). It originates in the Katun glaciers on the southwestern slope of Belukha Mountain. The river freezes up in late November or early December and breaks up in early or mid-April. The main tributaries of the Katun are, from source to mouth: Koksa (left), Kucherla (right), Argut (right), Chuya (right), Ursul (left), Sema (left) and Isha (right). The river is navigable.
In its upper reach of the Katun flows down the distant and sparsely populated area, but a few kilometers downstream near the village Kuyus, the coastal population density grows steadily and the area downstream of the village Ust-Sema is the most populated. There are numerous buildings, holiday camps and various guest houses in the pine forest near the village. The main settlements along the Katun are, from source to mouth: Ust-Koksa, Katanda, Inya, Chemal, Manzherok, Souzga, Aya, Mayma, Srostki and Verkh-Katunskoye.
See also
References
- ^ "Katun River discharge at Srostki". Soviet Union Hydro-Station archive. UNESCO. 1936–1990. Archived from the original on 25 November 2009. Retrieved 12 November 2010.
- ^ "Katun River discharge at Srostki". Soviet Union Hydro-Station archive. UNESCO. 1936–1990. Archived from the original on 25 November 2009. Retrieved 12 November 2010.
- ^ Катунь, Great Soviet Encyclopedia
- ^ "Река БИЯ in the State Water Register of Russia". textual.ru (in Russian)., erroneously named "БИЯ"