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Ural Mountains in summer. The Nether-Polar Ural are higher, and up to 150 km (93 mi) wider than the Polar Urals. They include the highest peaks of the range: Mount Narodnaya (1,895 m (6,217 ft)), Mount Karpinsky (1,878 m (6,161 ft)) and Manaraga (1,662 m (5,453 ft)). They extend for more than 225 km (140 mi) south to the Shchugor. The many ...
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 Riphean Mountains referred to the Ural Mountains. The Ural was considered the boundary between two worlds: civilized Europe and distant, "mysterious" Asia; where the world's civilizations converge: Eurasia. [clarification needed] By the early Common Era, great Migrations of nomads from the east – Huns, Avars, Slavs, and Bulgars.
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 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 worst hit areas in Russia are just to the south of the Ural Mountains, about 1,200 km (750 miles) east of Moscow. Emergencies have been declared in the Orenburg and Kurgan regions of the Urals ...
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 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.