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Research Range
The Research Range (russian: Исследовательский хребет) is a mountain range at the northern end of the Ural Mountains. It extends north of the Arctic Circle, and forms the border between the Komi Republic and the Khanty–Mansi Autonomous Okrug. The Research Range is 175 km long and the highest point is Mount Narodnaya (Гора Народная) or People's Mountain, at 1,894 m. The Research Range starts approximately at Mount Narodnaya and runs northeastward past Vorkuta almost to the Kara Sea and the Arctic Ocean. The primary rocks are metamorphic, mostly quartzites and slate. There are numerous glaciers near the tops and on the upper slopes of the mountains, the rest is mostly arctic desert and tundra. In the foothills and steep river valleys, there is some taiga forest."Исследовательский хребет"'Great Soviet Encyclopedia'' Notable peaks * Mount Narodnaya or People's Mountain, 1894 m. * Mount Karpinsky, 1878 m. * Mount R ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Komi Republic
The Komi Republic (russian: Республика Коми; kv, Коми Республика), sometimes simply referred to as Komi, is a republic of Russia located in Eastern Europe. Its capital is the city of Syktyvkar. The population of the republic as of the 2010 Census was 901,189. History The Komi people first feature in the records of the Novgorod Republic in the 12th century, when East Slavic traders from Novgorod traveled to the Perm region in search of furs and animal hides. The Komi territories came under the influence of Muscovy in the late Middle Ages (late 15th to early 16th centuries). The site of Syktyvkar, settled from the 16th century, was known as Sysolskoye (Сысольскoe). In 1780, under Catherine the Great, it was renamed to Ust-Sysolsk (Усть-Сысольск) and used as a penal colony. Russians explored the Komi territory most extensively in the 19th and early 20th centuries, starting with the expedition led by Alexander von Keyserling in 18 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Metamorphic Rock
Metamorphic rocks arise from the transformation of existing rock to new types of rock in a process called metamorphism. The original rock (protolith) is subjected to temperatures greater than and, often, elevated pressure of or more, causing profound physical or chemical changes. During this process, the rock remains mostly in the solid state, but gradually recrystallizes to a new texture or mineral composition. The protolith may be an igneous, sedimentary, or existing metamorphic rock. Metamorphic rocks make up a large part of the Earth's crust and form 12% of the Earth's land surface. They are classified by their protolith, their chemical and mineral makeup, and their texture. They may be formed simply by being deeply buried beneath the Earth's surface, where they are subject to high temperatures and the great pressure of the rock layers above. They can also form from tectonic processes such as continental collisions, which cause horizontal pressure, friction, and distorti ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Antal Reguly
Antal Reguly ( hu, Reguly Antal, 1819–1858) was a Hungarian linguist and ethnographer notable for his contribution to the study of Uralic languages. In 1843-4 he became the first ethnographer to visit the Mansi (Vogul) people to collect data on their language and folklore. Reguly's field work among the Uralic peoples of Russia ruined his health, and he died young, leaving much of the material he had collected to be edited by his successors, including Pál Hunfalvy. Reguly also visited Finland and translated parts of ''The Kalevala'' into Hungarian. The Reguly Antal Memorial Library and Reguly Antal Ethnographic Museum and Folk Art Workshop is in the town of Zirc, in Veszprém county, Hungary. Mount Reguly in the Research Range is also named for him. See also * Matthias Castrén Matthias Alexander Castrén (2 December 1813 – 7 May 1852) was a Finnish Swedish ethnologist and philologist who was a pioneer in the study of the Uralic languages. He was an educator, aut ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount Karpinsky, Urals
Mount Karpinsky, or Karpinsky Mountain, is a peak in the circumpolar part of the Ural Mountains. It is part of the Research Range, and lies on the boundary between the Komi Republic and the Tyumen Oblast. Rising to a height of 1878 m, it is composed of quartzites and crystalline schists. The slopes are predominantly mountain tundra, but there are coniferous forests in the foothills. Mount Karpinsky was named for the geologist Aleksandr Petrovich Karpinsky. '' |
Great Soviet Encyclopedia
The ''Great Soviet Encyclopedia'' (GSE; ) is one of the largest Russian-language encyclopedias, published in the Soviet Union from 1926 to 1990. After 2002, the encyclopedia's data was partially included into the later ''Bolshaya rossiyskaya entsiklopediya'' (or '' Great Russian Encyclopedia'') in an updated and revised form. The GSE claimed to be "the first Marxist–Leninist general-purpose encyclopedia". Origins The idea of the ''Great Soviet Encyclopedia'' emerged in 1923 on the initiative of Otto Schmidt, a member of the Russian Academy of Sciences. In early 1924 Schmidt worked with a group which included Mikhail Pokrovsky, (rector of the Institute of Red Professors), Nikolai Meshcheryakov (Former head of the Glavit, the State Administration of Publishing Affairs), Valery Bryusov (poet), Veniamin Kagan (mathematician) and Konstantin Kuzminsky to draw up a proposal which was agreed to in April 1924. Also involved was Anatoly Lunacharsky, People's Commissar of Education ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Taiga
Taiga (; rus, тайга́, p=tɐjˈɡa; relates to Mongolic and Turkic languages), generally referred to in North America as a boreal forest or snow forest, is a biome characterized by coniferous forests consisting mostly of pines, spruces, and larches. The taiga or boreal forest has been called the world's largest land biome. In North America, it covers most of inland Canada, Alaska, and parts of the northern contiguous United States. In Eurasia, it covers most of Sweden, Finland, much of Russia from Karelia in the west to the Pacific Ocean (including much of Siberia), much of Norway and Estonia, some of the Scottish Highlands, some lowland/coastal areas of Iceland, and areas of northern Kazakhstan, northern Mongolia, and northern Japan (on the island of Hokkaidō). The main tree species, depending on the length of the growing season and summer temperatures, vary across the world. The taiga of North America is mostly spruce, Scandinavian and Finnish taiga consists of ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Slate
Slate is a fine-grained, foliated, homogeneous metamorphic rock derived from an original shale-type sedimentary rock composed of clay or volcanic ash through low-grade regional metamorphism. It is the finest grained foliated metamorphic rock. Foliation may not correspond to the original sedimentary layering, but instead is in planes perpendicular to the direction of metamorphic compression. The foliation in slate is called "slaty cleavage". It is caused by strong compression causing fine grained clay flakes to regrow in planes perpendicular to the compression. When expertly "cut" by striking parallel to the foliation, with a specialized tool in the quarry, many slates will display a property called fissility, forming smooth flat sheets of stone which have long been used for roofing, floor tiles, and other purposes. Slate is frequently grey in color, especially when seen, en masse, covering roofs. However, slate occurs in a variety of colors even from a single locality; for ex ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Quartzite
Quartzite is a hard, non- foliated metamorphic rock which was originally pure quartz sandstone.Essentials of Geology, 3rd Edition, Stephen Marshak, p 182 Sandstone is converted into quartzite through heating and pressure usually related to tectonic compression within orogenic belts. Pure quartzite is usually white to grey, though quartzites often occur in various shades of pink and red due to varying amounts of hematite. Other colors, such as yellow, green, blue and orange, are due to other minerals. The term ''quartzite'' is also sometimes used for very hard but unmetamorphosed sandstones that are composed of quartz grains thoroughly cemented with additional quartz. Such sedimentary rock has come to be described as orthoquartzite to distinguish it from metamorphic quartzite, which is sometimes called metaquartzite to emphasize its metamorphic origins. Quartzite is very resistant to chemical weathering and often forms ridges and resistant hilltops. The nearly pure silica conte ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Arctic Ocean
The Arctic Ocean is the smallest and shallowest of the world's five major oceans. It spans an area of approximately and is known as the coldest of all the oceans. The International Hydrographic Organization (IHO) recognizes it as an ocean, although some oceanographers call it the Arctic Mediterranean Sea. It has been described approximately as an estuary of the Atlantic Ocean. It is also seen as the northernmost part of the all-encompassing World Ocean. The Arctic Ocean includes the North Pole region in the middle of the Northern Hemisphere and extends south to about 60°N. The Arctic Ocean is surrounded by Eurasia and North America, and the borders follow topographic features: the Bering Strait on the Pacific side and the Greenland Scotland Ridge on the Atlantic side. It is mostly covered by sea ice throughout the year and almost completely in winter. The Arctic Ocean's surface temperature and salinity vary seasonally as the ice cover melts and freezes; its salinity is t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Khanty–Mansi Autonomous Okrug
Khanty-Mansi Autonomous Okrug–Yugra (Russian and Mansi: Ханты-Мансийский автономный округ — Югра, ''Khanty-Mansiysky avtonomny okrug — Yugra;'' Khanty: Хӑнты-Мансийской Aвтономной Округ) or Khantia-Mansia is a federal subject of Russia (an autonomous okrug of Tyumen Oblast). It has a population of 1,532,243 as of the 2010 Census. The peoples native to the region are the Khanty and the Mansi, known collectively as Ob-Ugric people, but today the two groups only constitute 2.1% of the region's population. The local languages, Khanty and Mansi, enjoy special status in the autonomous okrug and along with their distant relative Hungarian are part of the Ugric branch of the Finno-Ugric languages. Russian remains the only official language. In 2012, the majority (51%) of the oil produced in Russia came from Khanty-Mansi Autonomous Okrug, giving the region great economic importance in Russia and the world. It border ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
