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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 Polar Ural has an area of about 25,000 km 2 and a strongly dissected relief. The Near-Polar Ural is wider (up to 150 km) and higher than the Polar Ural. The Northern Ural consists of a series of parallel ridges with the height up to 1,000–1,300 m and longitudinal depressions, which are elongated from north to south.
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 .
Eastward, mainland Europe widens much like the mouth of a funnel, until the boundary with Asia is reached at the Ural Mountains and Ural River, the Caspian Sea, and the Caucasus Mountains. Land relief in Europe shows great variation within relatively small areas.
The relief of the Southern Urals is complex, with numerous valleys and parallel ridges directed south-west and meridionally. The range includes the Ilmensky Mountains separated from the main ridges by the Miass River. The maximum height is 1,640 m (5,380 ft) (Mount Yamantau) and the width reaches 250 km (160 mi).
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.
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.
This ecoregion covers the Ural Mountains in a band that is narrow from west-east, but runs up most of the divide between European and Asiatic Russia. It is a meeting zones of taiga and tundra tree and plant species. [3] The climate of the South Ural Reserve is Humid continental climate, warm summer (Köppen climate classification). This climate ...