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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 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 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.
The craton is bounded on the east by the long tract of compressed and highly deformed rock that constitutes the Ural orogen. In Asiatic Russia, the area between the Ural Mountains and the Yenisei River is the young West Siberian Plain. East of the Yenisei River is the ancient Central Siberian Plateau, extending to the Lena River.
The Manpupuner rock formations. The Manpupuner rock formations (Man-Pupu-Nyor; Mansi: Мань-Пупыг-Нёр [manʲ.pupiɣ noːr], literally ’Small Idol Mountain’; Komi: Болвано-Из [bolvano iz], literally ’Idol Stone’) are a set of 7 stone pillars located west of the Ural Mountains in the Troitsko-Pechorsky District of the Komi Republic.
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 Ural River, which rises in the Ural Mountains and flows into the Caspian Sea, swelled several metres in just hours on Friday due to melt water, bursting through a dam embankment in the city of ...
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.