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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 Urals montane tundra and taiga ecoregion (WWF ID: PA0610) covers the main ridge of the Ural Mountains (both sides) - a 2,000 km (north-south) by 300 km (west-east) region. The region is on the divide between European and Asian ecoregions, and also the meeting point of tundra and taiga.
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.
Reverted to version as of 10:57, 18 October 2014 In all maps Georgia is part of Georgia. There is at list 10 versions of borders of Europe in most of them Georgia is part of Europa: 20:04, 18 October 2014: 537 × 536 (238 KB) Politologia: Reverted to version as of 10:57, 18 October 2014 In all maps Georgia is part of Georgia.
Topographic map of Russia. The Great Russian Regions are eight geomorphological regions of the Russian Federation displaying characteristic forms of relief. Seven of them are parts of Siberia, located east of the Ural Mountains. [1]
The Ural Mountains — a major mountain range of eastern European Russia, Siberia, and northwestern Kazakhstan. Pages in category "Ural Mountains" The following 39 pages are in this category, out of 39 total.
The Virgin Komi Forests are part of the Ural Mountains taiga ecoregion, characterized by a subarctic climate with long, cold winters and short, warm summers. This climate supports extensive peat bogs, rivers, and natural lakes, which play a crucial role in carbon sequestration and maintaining regional hydrology .
The Main Uralian Fault (MUF) runs north–south through the middle of the Ural Mountains for over 2,000 km. It separates both Europe from Asia and the three, or four, western megazones of the Urals from the three eastern megazones: namely the Pre-Uralian Foredeep, West Uralian, and the Central Uralian to the west, and the Tagil-Magnitogorskian, East Uralian, and Transuralian to the east.
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