Kuznetsk Alatau (Russian: Кузнецкий Алатау) is a mountain range, South Siberia, Russia between Kuznetsk Depression and Minusinsk Depression. Length: about 300 km., elevation: up to 2,178 metres (7,146 ft). It is part of the mountain system of Central Asia. See Geography of South-Central Siberia.
These mountains have smooth outline, rather steep western and gentle eastern slopes. The fir overwhelmingly predominates in the forest belt except for its upper part where, at the tree line (1300–1900 m), the pine becomes a dominant. The highlands are occupied mostly by vast large-stoned screes, and also by patches of subalpine meadows and, on some southern mountain massifs, of bushy, lichen and moss tundras. The basin of the Kondoma River in Gornaya Shoriya is remarkable for the lime-tree woods which are thought to be the relics of a pre-Pleistocene nemoral vegetation of Siberia. All over the upland the forest openings are occupied by long forb forest meadows.
Siberia (//; Russian: Сиби́рь, tr. Sibir'; IPA: [sʲɪˈbʲirʲ] ( listen)) is an extensive geographical region constituting almost all of North Asia. Comprising the central and eastern portion of the Russian Federation, Siberia was part of the Soviet Union (USSR) from its beginning, as of its predecessor states, the Tsardom of Russia and the Russian Empire since the 16th century.