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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 ...
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 39 pages are in this category, out of 39 total.
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.
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 ...
MOSCOW (Reuters) -Flood waters were rising in two cities in Russia's Ural mountains on Sunday after Europe's third-longest river burst through a dam, flooding at least 10,000 homes and forcing ...
The Ural Mountains, a 2,500 kilometre (1,600 mi) long mountain chain that runs north–south at approximately 60° E longitude, formed in the Ural orogeny, a long series of mountain-building events occurring at the eastern margin of what is now the East European craton in association with its collision with another microcontinent (the ...
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.