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The Sakmara rises in the southern Ural Mountains about 60 kilometres (37 mi) west-southwest of Magnitogorsk and flows south through a valley with some canyon development. At Kuvandyk it swings west, leaves the mountains, and flows west parallel to the Ural River with many meanders for about 150 kilometres (93 mi) (straight-line distance) before ...
1 sty 2022 · The Sakmara is partly fed by groundwater, reducing seasonal and interannual flow variation. It is a snow-fed river with maximum discharge in spring (∼70% of total annual discharge). During spring floods, discharge can exceed 5300 m 3 /s.
The Bolshoy Ik (Russian: Большой Ик, literally Greater Ik; Bashkir: Оло Ыйыҡ, Olo Iyıq) is a tributary of the Sakmara, which flows south from the southern end of the Ural Mountains in Bashkortostan and Orenburg Oblast, Russia.
In the geologic timescale, the Sakmarian is an age or stage of the Permian period. It is a subdivision of the Cisuralian Epoch or Series. The Sakmarian lasted between 293.52 and 290.1 million years ago (Ma). It was preceded by the Asselian and followed by the Artinskian. [4]
19 mar 2007 · The aim of this study was to determine how Unio bivalve shells fragment within the channel of the Sakmara River (southern Urals, Russia). The Sakmara River has an abundant bivalve population and a highly variable flow regime which, at low flow, allowed much of the channel bed to be examined.
The Sakmara is a river in Russia that drains the southern tip of the Ural Mountains south into the river Ural. It is 798 kilometres (496 mi) long, and has a drainage basin of 30,200 square kilometres (11,700 sq mi).
17 wrz 2021 · The Ural’s tributaries also play a role in supplying it with water, with the largest being the Sakmara, the Elek and the Chagan. The river’s source freezes in early November while the middle and lower reaches of the river freeze in late November.
