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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.
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.
English: Map of Europe. The continental boundary to Asia as indicated is the standard convention following the Caucasus crest, the Ural River and the Urals Mountains to the Sea of Kara The continental boundary to Asia as indicated is the standard convention following the Caucasus crest, the Ural River and the Urals Mountains to the Sea of Kara
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 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.
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The Polar Urals (Russian: Полярный Урал) are a mountain range in the western part of the Yamalo-Nenets Autonomous Okrug and the northeastern part of Komi, Russian Federation. The border between Europe and Asia runs along the main ridge of the Polar Urals. [ 1 ]