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Ural Mountains - Climate, Geology, Biodiversity: The climate is of the continental type, marked by temperature extremes that become increasingly evident both from north to south and from west to east. The Pay-Khoy Range and the Polar Urals enjoy the moderating influence of the Arctic and the North Atlantic oceans, particularly in winter. In the Mughalzhar Hills and the Southern Urals there are ...
Dec 20, 2015 · The Urals rise like a long and narrow spine across western Russia, forming a natural divide between Europe and Asia. The mountain range spans 2,500 kilometers (1,550 miles) passing through Arctic tundra to the north and through forested and semi-desert landscapes to the south. Continental collisions gave rise to the Urals between 250 and 300 ...
Map of the Ural Mountains The Village of Kolchedan in the Ural Mountains in 1912 Work at the Bakalskii mine. The Ural Mountains (Russian: Ура́льские го́ры, romanized: Uralskiye gory), also known simply as the Urals, is a mountain range that runs roughly north and south through western Russia.
The Ural Mountains of Russia form the traditional boundary between Europe and Asia. The Urals are about 1,550 miles (2,500 kilometers) long. They extend from the Kara Sea in the north to the Ural River in the south. The highest peak is Mount Narodnaya at 6,217 feet (1,895 meters). The northern slopes of the Urals are mostly covered with forests.
Ural Mountains - Indigenous Peoples, Russia, Europe: Human habitation of the Urals dates to the distant past. The Nenets (Samoyed) people the Pay-Khoy region, and their language belongs to the Samoyedic group of languages, which is widespread throughout northern Siberia. Farther south live the Komi, Mansi, and Khanty, who speak a tongue belonging to the Ugric group of the Finno-Ugric languages ...
Uralian orogeny. 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 ...
