Pay-Khoy
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Pay-Khoy
The Pay-Khoy Range ( rus, хребет Пай-Хой) is a mountain range at the northern end of the Ural Mountains. It lies within the Nenets Autonomous Okrug. Geography The ridge is extended from northwest to southeast. It is located on the Yugorsky Peninsula, in the eastern part of the Nenets Autonomous Okrug. The ridge continues to Vaygach Island, thus separating the Barents Sea and the Kara Sea. The highest point of Pay-Khoy is the mountain of Moreiz (). The range separates the drainage basins of the (west, Barents Sea) and the Kara River (east, Kara Sea). The areas around Pay-Khoy do not have permanent population. The closest permanent settlements are Amderma and Ust-Kara, Nenets Autonomous Okrug The range is located in the tundra, to the north of the tree line. Geology The Pay-Khoy range forms a curved orogen together with the Ural Mountains, Vaygach Island and the Novaya Zemlya Novaya Zemlya (, also , ; rus, Но́вая Земля́, p=ˈnovəjə zʲɪmˈlʲa, ) ...
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Yugorsky Peninsula
The Yugorsky Peninsula (russian: Югорский полуостров) is a large peninsula in Nenets Autonomous Okrug, Russia. It is limited by the Khaypudyr Bay in the Pechora Sea to the west and by the Baydaratsk Bay in the Kara Sea to the north and east. Compared to the Barents Sea, which receives relatively warm currents from the Atlantic Ocean, the Kara Sea is much colder, remaining frozen for over nine months a year. Thus often, in the spring and in the fall, the eastern coast of the Yugorsky Peninsula is frozen, while its western coast is clear of ice. The Yugorsky Strait and, beyond it, Vaygach Island lie at the northwestern end of this peninsula. The Pay-Khoy Ridge occupies the peninsula and extends from northwest to southeast. In the southeastern end of the Yugorsky Peninsula lies the Kara meteorite crater, while the Ust-Kara site lies offshore, 15 km east of the small Kara or Karskaya Guba inlet. It was formerly believed that these two sites were two separat ...
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Urals
The Ural Mountains ( ; rus, Ура́льские го́ры, r=Uralskiye gory, p=ʊˈralʲskʲɪjə ˈɡorɨ; ba, Урал тауҙары) or simply the Urals, are a mountain range that runs approximately from north to south through European Russia, western Russia, from the coast of the Arctic Ocean to the river Ural (river), Ural and northwestern Kazakhstan.Ural Mountains
Encyclopædia Britannica on-line
The mountain range forms part of the Boundaries between the continents of Earth, conventional boundary between the regions of Europe and Asia. Vaygach Island and the islands of Novaya Zemlya form a further continuation of the chain to the north into the Arctic Ocean. The Ural Mountains are one of the richest mineral regions in the world, containing more than 1,000 varieties of valuable minerals. The mountains lie ...
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Ural Mountains
The Ural Mountains ( ; rus, Ура́льские го́ры, r=Uralskiye gory, p=ʊˈralʲskʲɪjə ˈɡorɨ; ba, Урал тауҙары) or simply the Urals, are a mountain range that runs approximately from north to south through western Russia, from the coast of the Arctic Ocean to the river Ural and northwestern Kazakhstan.Ural Mountains
Encyclopædia Britannica on-line
The mountain range forms part of the conventional boundary between the regions of and

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Federal Subject
The federal subjects of Russia, also referred to as the subjects of the Russian Federation (russian: субъекты Российской Федерации, subyekty Rossiyskoy Federatsii) or simply as the subjects of the federation (russian: субъекты федерации, subyekty federatsii), are the constituent entities of Russia, its top-level political divisions according to the Constitution of Russia. Kaliningrad Oblast is the only federal subject geographically separated from the rest of the Russian Federation by other countries. According to the Russian Constitution, the Russian Federation consists of republics, krais, oblasts, cities of federal importance, an autonomous oblast and autonomous okrugs, all of which are equal subjects of the Russian Federation. Three Russian cities of federal importance (Moscow, Saint Petersburg, and Sevastopol) have a status of both city and separate federal subject which comprises other cities and towns (Zelenograd, Troitsk, ...
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Mountain Ranges Of Russia
A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited summit area, and is usually higher than a hill, typically rising at least 300 metres (1,000 feet) above the surrounding land. A few mountains are isolated summits, but most occur in mountain ranges. Mountains are formed through tectonic forces, erosion, or volcanism, which act on time scales of up to tens of millions of years. Once mountain building ceases, mountains are slowly leveled through the action of weathering, through slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce colder climates than at sea level at similar latitude. These colder climates strongly affect the ecosystems of mountains: different elevations have different plants and animals. Because of the less hospitable terrain and ...
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Novaya Zemlya
Novaya Zemlya (, also , ; rus, Но́вая Земля́, p=ˈnovəjə zʲɪmˈlʲa, ) is an archipelago in northern Russia. It is situated in the Arctic Ocean, in the extreme northeast of Europe, with Cape Flissingsky, on the northern island, considered the easternmost point of Europe. To Novaya Zemlya's west lies the Barents Sea and to the east is the Kara Sea. Novaya Zemlya consists of two main islands, the northern Severny Island and the southern Yuzhny Island, which are separated by the Matochkin Strait. Administratively, it is incorporated as Novaya Zemlya District, one of the twenty-one in Arkhangelsk Oblast, Russia.Law #65-5-OZ Municipally, it is incorporated as Novaya Zemlya Urban Okrug.Law #258-vneoch.-OZ The population of Novaya Zemlya as of the 2010 Census was about 2,429, of whom 1,972 resided in Belushya Guba, an urban settlement that is the administrative center of Novaya Zemlya District. The indigenous population (from 1872 to the 1950s when it was resett ...
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Tundra
In physical geography, tundra () is a type of biome where tree growth is hindered by frigid temperatures and short growing seasons. The term ''tundra'' comes through Russian (') from the Kildin Sámi word (') meaning "uplands", "treeless mountain tract". There are three regions and associated types of tundra: Arctic tundra, alpine tundra, and Antarctic tundra. Tundra vegetation is composed of dwarf shrubs, sedges, grasses, mosses, and lichens. Scattered trees grow in some tundra regions. The ecotone (or ecological boundary region) between the tundra and the forest is known as the tree line or timberline. The tundra soil is rich in nitrogen and phosphorus. The soil also contains large amounts of biomass and decomposed biomass that has been stored as methane and carbon dioxide in the permafrost, making the tundra soil a carbon sink. As global warming heats the ecosystem and causes soil thawing, the permafrost carbon cycle accelerates and releases much of these soil-contained g ...
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Ust-Kara, Nenets Autonomous Okrug
Ust-Kara (russian: Усть-Ка́ра) is a village on the eastern border of Zapolyarny District, Nenets Autonomous Okrug, Russia. It had a population of 574 as of 2010, a decrease from its population of 677 in 2002. Geography The village is located at the mouth of the Kara, next to the border with Yamalo-Nenets Autonomous Okrug. The nearest major city is Vorkuta, which is about 200 km south. Southwest of the settlement is the Kara crater, which is one of the largest craters on Earth, at 65 km in diameter. History In 2003, there was a hepatitis A outbreak in the village. One year later, in 2004, the only school in the village burned down, followed by the decision to build a new one. Transport There is no road to Ust-Kara, so the village can only be reached by a flight from Naryan-Mar. Climate Ust-Kara has a subarctic climate ( Dfc). Notable people Andrey Rasbash Andrey Leonidovich Rasbash (russian: Андре́й Леони́дович Разба́ш; December 15, ...
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Kara River
The Kara (russian: Ка́ра) is a river draining to the Arctic Kara Sea in Russia. It flows through the Pai-Khoi Range in the Polar Ural region, and forms parts of the borders between the Yamalo-Nenets Autonomous Okrug, the Nenets Autonomous Okrug and the Komi Republic. The length of the river, from the confluence of the Malaya and Bolshaya Kara to the mouth in the Baydaratskaya Bay Baydaratskaya Bay or Baydarata Bay (russian: Байдарацкая губа, Baydaratskaya guba, Tundra Nenets language, Tundra Nenets: Пэдарита, ''Pėdarita'') is a gulf in Russia, located in the southern part of the Kara Sea between t ... is . Its drainage basin area is . The settlement of Ust-Kara is near the river mouth. The name of the river is derived from Nenets word meaning " hummocked ice".V.Yu. Vize, ''Karskoye more // Morya Sovetskoy Arktiki: Ocherki po istorii issledovaniya'' (Leningrad, 1939) — pp. 180—217 References Rivers of Yamalo-Nenets Autonomous Okrug R ...
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Drainage Basin
A drainage basin is an area of land where all flowing surface water converges to a single point, such as a river mouth, or flows into another body of water, such as a lake or ocean. A basin is separated from adjacent basins by a perimeter, the '' drainage divide'', made up of a succession of elevated features, such as ridges and hills. A basin may consist of smaller basins that merge at river confluences, forming a hierarchical pattern. Other terms for a drainage basin are catchment area, catchment basin, drainage area, river basin, water basin, and impluvium. In North America, they are commonly called a watershed, though in other English-speaking places, "watershed" is used only in its original sense, that of a drainage divide. In a closed drainage basin, or endorheic basin, the water converges to a single point inside the basin, known as a sink, which may be a permanent lake, a dry lake, or a point where surface water is lost underground. Drainage basins are similar ...
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Kara Sea
The Kara Sea (russian: Ка́рское мо́ре, ''Karskoye more'') is a marginal sea, separated from the Barents Sea to the west by the Kara Strait and Novaya Zemlya, and from the Laptev Sea to the east by the Severnaya Zemlya archipelago. Ultimately the Kara, Barents and Laptev Seas are all extensions of the Arctic Ocean north of Siberia. The Kara Sea's northern limit is marked geographically by a line running from Cape Kohlsaat in Graham Bell Island, Franz Josef Land, to Cape Molotov (Arctic Cape), the northernmost point of Komsomolets Island in Severnaya Zemlya. The Kara Sea is roughly long and wide with an area of around and a mean depth of . Its main ports are Novy Port and Dikson and it is important as a fishing ground although the sea is ice-bound for all but two months of the year. The Kara Sea contains the East-Prinovozemelsky field (an extension of the West Siberian Oil Basin), containing significant undeveloped petroleum and natural gas. In 2014, US gov ...
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