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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 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. The Central Ural is the lowest part of Urals, with the highest mountain of 994 m (Basegi) and a smooth relief. The relief of Southern Ural is more complex, with numerous valleys ...
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 the Southern Urals extend up to 250 km (160 mi) with an average width between 40 km (25 mi) and 150 km (93 mi). [2] The Southern Urals include lakes such as Zyuratkul. [3]
Shaded relief map of the United States, showing 10 geological provinces. The richly textured landscape of the United States is a product of the dueling forces of plate tectonics, weathering and erosion. Over the 4.5 billion-year history of the Earth, tectonic upheavals and colliding plates have raised great mountain ranges while the forces of ...
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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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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.