Tundra Bolszeziemielska

Landscape of the Tundra of the Bolshevik soil Tundra Bolshevik (Russian: Большеземельская тундра, Bolszeziemielskaja tundra) is a hilly lowland in the northwestern part of Russia, on the Barents Sea, between the Pecs and Usa rivers and the Urals and Paj Choj. It is located in the Autonomous Region of the Autonomous Region of the Republic of Komi. It rises to the height of 100-150 m n.p.m., the highest part reaches 200-250 m n.p.m. The most prominent part is the area stretching between the estuary of Cylma and the Gulf of Khajdre, the so-called. The chrybiet is chopped. In the relief of the terrain of the Tundra Bolshevikel, hills and moraine hills dominate the so-called. Mustards, made of sand and clay. Throughout the eastern part of the lowlands, the Chernyszow Grotto runs through, mainly composed of Paleozoic settlements. The Bolshevik underground lies in the subpolar climate zone. The winters in the area are long and cold (the average January temperature in the northwest is -16 ° C, while in the south-east - -20 ° C), and the years are short and cool (the average July temperature is 8 to 12 ° C ). Frosts also occur during the summer months. In the southern part the annual rainfall is about 450 mm, while the northern part is about 250 mm. Tundra Bolszeziemielska has a dense river network, mainly composed of the tributaries of Pechora and Usa. In the upper reaches of the main rivers (eg Szapkin, Kołwa, Adźwa) there are many lakes (eg Vashutkiny, Szapkinskije). A large area of ​​lowland is covered with eternal freezing. A tundra is a plant vestiges, mainly mosses and shrubs. In the southern part of the lowland there is a lasotundra. South of the Arctic Circle is the taiga. Local people are involved in reindeer breeding and hunting. Part of the area of ​​the Tundra Bolshevikel is part of the Peak Coal Basin. There are also large deposits of crude oil and natural gas.

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