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The sediments to the west of the Ural Mountains are formed of limestone, dolomite and sandstone left from ancient shallow seas. The eastern side is dominated by basalts. [6] Wooded Ural Mountains in winter. The western slope of the Ural Mountains has predominantly karst topography, especially in the Sylva basin, which is a tributary of the ...
The mountains were formed by folding, and represent an anticline. [2] The Verkhoyansk Range was covered by glaciers during the Last Glacial Period and the mountains in the northern section, such as the Orulgan Range, display a typical Alpine relief. There are coal, silver, lead, tin, and zinc deposits in the mountains.
Ural (Russian: Урал) is a geographical region located around the Ural Mountains, between the East European and West Siberian plains. It is considered a part of the Eurasian Steppe , extending approximately from the North to the South; from the Arctic Ocean to the end of the Ural River near Orsk city.
The Ural Mountains — a major mountain range of eastern European Russia, Siberia, and northwestern Kazakhstan. Pages in category "Ural Mountains" The following 37 pages are in this category, out of 37 total.
The craton is bounded on the east by the long tract of compressed and highly deformed rock that constitutes the Ural orogen. In Asiatic Russia, the area between the Ural Mountains and the Yenisei River is the young West Siberian Plain. East of the Yenisei River is the ancient Central Siberian Plateau, extending to the Lena River.
Other notable peaks lie along the Iremel mountain ridge (Bolshoy Iremel and Maly Iremel), the Nurgush, highest point 1,406 m (4,613 ft), and the Nakas, highest point 667.6 m (2,190 ft). [1] The Southern Urals extend some 550 km (340 mi) up to the sharp westward bend of the Ural River and terminate in the wide Mugodzhar Hills. The foothills of ...
Highest mountain in Adygea Tabozhok [56] Табожок 3201 m 10,502 ft: 633 m 2,077 ft: 22.4 km 13.92 mi Kuray Mountains Altai Mountains Altai Republic: Gaykomd [57] Гайкомд 3152 m 10,341 ft: 1231 m 4,039 ft: 9.8 km 6.09 mi
The Ural is conventionally considered part of the boundary between the continents of Europe and Asia. The Ural rises near Mount Kruglaya in the Ural Mountains, flows south parallel and west of the north-flowing Tobol, through Magnitogorsk, and around the southern end of the Urals, through Orsk where it turns west for about 300 kilometres (190 ...