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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.
Mount Payer is a 1,472 metres (4,829 ft) high mountain located near the Arctic Circle in the Polar Urals, a subrange of the Urals.It rises in the middle part of the range, in Shuryshkarsky District, near the border of the Komi Republic.
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.
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.
Topography of Ural Mountains. The Sub-Ural Plateau is to the west of the southernmost extent of Ural The Sub-Ural Plateau ( Russian : Подуральское плато , romanized : Poduralskoe Plato ) is a low-elevation mountainous plateau mostly in west Kazakhstan and some northern parts are in Russia .
The Uralian orogeny refers to the long series of linear deformation and mountain building events that raised the Ural Mountains, starting in the Late Carboniferous and Permian periods of the Palaeozoic Era, c. 323–299 and 299–251 million years ago (Mya) respectively, and ending with the last series of continental collisions in Triassic to early Jurassic times.
The Research Range is 175 km long and the highest point is Mount Narodnaya (Гора Народная) or People's Mountain, at 1,894 m. The Research Range starts approximately at Mount Narodnaya and runs northeastward past Vorkuta almost to the Kara Sea and the Arctic Ocean. The primary rocks are metamorphic, mostly quartzites and slate.
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