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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 ...
It is the highest point in European Russia outside the Caucasus. This leads to its large topographic prominence of 1,772 metres (5,814 ft). Narodnaya is located in the Ural mountains water divide , and therefore on the border between Europe and Asia : the Naroda river flows south-east from the summit into the Ob river in Siberia , and the Kos ...
It is located 16.5 km west of Mount Narodnaya, the highest peak in the Ural mountains. [4] The slopes of the peak are gentle and grassy, but the summit is jagged and rocky. Manaraga translated from Nenets means "Bear Paw". [3]
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 Carpathian Mountains or Carpathians (/ k ɑːr ˈ p eɪ θ i ən z /) are a range of mountains forming an arc across Central Europe and Southeast Europe. Roughly 1,500 km (930 mi) long, it is the third-longest European mountain range after the Urals at 2,500 km (1,600 mi) and the Scandinavian Mountains at 1,700 km (1,100 mi).
Subpolar Urals: Yamantau: Ямантау 1,640 metres (5,380 ft) Bashkortostan: Southern Urals: Unnamed — 1,603 metres (5,259 ft) Stavropol Krai: Kabardian Range (south of Kislovodsk) [6] [7] Konzhakovskiy Kamen: Конжаковский Камень 1,569 metres (5,148 ft) Sverdlovsk Oblast: Konzhakov-Serebryan Massif, Northern Urals: Mount ...
Other notable peaks lie along the Iremel mountain ridge (Bolshoy Iremel and Maly Iremel), the Nurgush, highest point 1,406 m (4,613 ft), and the Nakas, highest point 667.6 m (2,190 ft). [1] The Southern Urals extend some 550 km (340 mi) up to the sharp westward bend of the Ural River and terminate in the wide Mugodzhar Hills. The foothills of ...
The Ural Mountains, a 2,500 kilometre (1,600 mi) long mountain chain that runs north–south at approximately 60° E longitude, formed in the Ural orogeny, a long series of mountain-building events occurring at the eastern margin of what is now the East European craton in association with its collision with another microcontinent (the ...