Olyutor Range
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Olyutor Range
The Olyutor Range (russian: Олюторский хребет) is a range of mountains in Kamchatka Krai, Russian Far East. Administratively the range is part of Olyutorsky District.Google Earth The range is a mainland prolongation of the submerged Shirshov Ridge of the Bering Sea. Geography The Olyutor Range is a coastal mountain chain, with its eastern flank facing the Bering Sea. It is part of the Koryak Highland system. Despite the relatively small height of the range, its mountains have an alpine character with sharp, pointed ridgetops and steep slopes covered with scree. Deep river gorges and glacial valleys are widespread. The highest point is Greben, a high peak. To the north rises the Snegovoy Range and the southern part of the range forms the Olyutor Peninsula, jutting southwards with the Olyutor Gulf to the west. The southern end of the peninsula is Cape Olyutor (Mys Olyutorsky). Climate and flora The climate is influenced by the ocean. Summers are short and coo ...
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Greben (Kamchatka)
Greben (meaning "ridge" in Slavic languages) can refer to the following toponyms: *Greben (Višegrad), village in Bosnia and Herzegovina *Greben (mountain), mountain in Serbia and Bulgaria *Greben Hill, mountain in the Antarctica *Veliki Greben, mountain in northeastern Serbia *Greben' Island, minor island in Antarctica *Greben Island, minor island in Severnaya Zemlya Islands in the Russian Arctic {{geodis ...
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Scree
Scree is a collection of broken rock fragments at the base of a cliff or other steep rocky mass that has accumulated through periodic rockfall. Landforms associated with these materials are often called talus deposits. Talus deposits typically have a concave upwards form, where the maximum inclination corresponds to the angle of repose of the mean debris particle size. The exact definition of scree in the primary literature is somewhat relaxed, and it often overlaps with both ''talus'' and ''colluvium''. The term ''scree'' comes from the Old Norse term for landslide, ''skriða'', while the term ''talus'' is a French word meaning a slope or embankment. In high-altitude arctic and subarctic regions, scree slopes and talus deposits are typically adjacent to hills and river valleys. These steep slopes usually originate from late-Pleistocene periglacial processes. Notable scree sites in Eastern North America include the Ice Caves at White Rocks National Recreation Area in southern Ve ...
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Landforms Of Siberia
A landform is a natural or anthropogenic land feature on the solid surface of the Earth or other planetary body. Landforms together make up a given terrain, and their arrangement in the landscape is known as topography. Landforms include hills, mountains, canyons, and valleys, as well as shoreline features such as bays, peninsulas, and seas, including submerged features such as mid-ocean ridges, volcanoes, and the great ocean basins. Physical characteristics Landforms are categorized by characteristic physical attributes such as elevation, slope, orientation, stratification, rock exposure and soil type. Gross physical features or landforms include intuitive elements such as berms, mounds, hills, ridges, cliffs, valleys, rivers, peninsulas, volcanoes, and numerous other structural and size-scaled (e.g. ponds vs. lakes, hills vs. mountains) elements including various kinds of inland and oceanic waterbodies and sub-surface features. Mountains, hills, plateaux, and plains are the fo ...
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Koryak Mountains
The Koryak Mountains or Koryak Highlands () are an area of mountain ranges in Far-Eastern Siberia, Russia, located in Chukotka Autonomous Okrug and in Kamchatka Krai, with a small part in Magadan Oblast. The highest point in the system is the Mount Ledyanaya, located in the Ukelayat Range, in the central part of the mountains. Geography The Koryak Mountains rise south of the Anadyr River, and northeast of the Kamchatka Peninsula. The Koryak Highlands are one of the largest glacial systems in the northern part of the Russian Far East. There are numerous glaciers and ice fields in some of the ranges, with a total surface of . Subranges The system of the Koryak Mountains comprises a number of subranges,Oleg Leonidovič Kryžanovskij, ''A Checklist of the Ground-beetles of Russia and Adjacent Lands.'' p. 16 including: * Vetvey Range, highest point * Vaeg Range, highest point * Pakhachin Range, highest point * Apuk Range * Vatyna Range *Penzhina Range, highest point * Gizhigin ...
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List Of Mountains And Hills Of Russia
This is a list of mountains and hills of Russia. List by elevation Over 5000 meters 4000 to 4999 meters 3000 to 3999 meters 2000 to 2999 meters 1000 to 1999 meters Under 1000 metres See also *Highest points of Russian Federal subjects *List of Altai mountains *List of mountains in Mongolia *List of mountains in China *List of ultras of Northeast Asia *List of volcanoes in Russia *List of lakes of Russia Notes References External links Russia - Highest Mountainsfrom GeoNamesfrom World AtlasRussia mountainsfrom Peakery {{Russia topics Russia Russia Russia Mountains and hills Russia Russia Russia (, , ), or the Russian Federation, is a List of transcontinental countries, transcontinental country spanning Eastern Europe and North Asia, Northern Asia. It is the List of countries and dependencies by area, largest country in the ...
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Bering Tundra
The Bering tundra ecoregion (WWF ID: PA1102) is an ecoregion that covers a portion of northeastern Russia, between the Kolyma Mountains on the west, and the Bering Sea coast to the east. The area is an important stopping place for migratory birds. It has an area of . Location and description The ecoregion stretches approximately 1,000 km on alignment from southwest-to-northeast, between the Kolyma Mountains on the west, the Bering Sea coast to the east, and Kamchatka peninsula to the south. Climate The climate of Koryak is '' Humid continental climate, cool summer'' (Köppen climate classification (Dfc)). This climate is characterised by long cold winters (at least one month averaging below ), and short, cool summers (one to three months greater than , but no month averaging above ). Mean precipitation is about 358 mm/year. The mean temperature at the center of the ecoregion is in January, and in July. Flora and fauna The ecoregion supports flora and fa ...
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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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Erman's Birch
''Betula ermanii'', or Erman's birch, is a species of birch tree belonging to the family Betulaceae. It is an extremely variable species and can be found in Northeast China, Korea, Japan, and Russian Far East (Kuril Islands, Sakhalin, Kamchatka). It can grow to tall. It is noted for its peeling bark, which can sometimes be removed in sheets, but usually shreds and hangs from the trunk and under branches. Yellow-brown male catkins appear with the leaves in spring. Erman's birch is widely cultivated outside its natural range. The cultivar 'Grayswood Hill' has gained the Royal Horticultural Society's Award of Garden Merit. Leading tree nurseries including Barcham Trees stock the species. It is consequently a frequently encountered street tree in London and other British towns and cities. File:Betula ermanii SE4 02 MG 5041.jpg, Street tree in Brockley Brockley is a district and an wards of the United Kingdom, electoral ward of south London, England, in the London Borough ...
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Dwarf Forest
Dwarf forest, elfin forest, or pygmy forest is an uncommon ecosystem featuring miniature trees, inhabited by small species of fauna such as rodents and lizards. They are usually located at high elevations, under conditions of sufficient air humidity but poor soil. There are two main dwarf forest ecosystem types, involving different species and environmental characteristics: coastal temperate and montane tropical regions. Temperate coastal dwarf forest is common for parts of Southern California. Montane tropical forests are found across tropical highlands of Central America, northern South America and Southeast Asia. There are also other isolated examples of dwarf forests scattered across the world, while the largest dwarf forest is found in the Philippines. High-elevation tropical dwarf forest High-elevation tropical locations in cloud forests contain mossy wet elfin forests due to high-elevation precipitation. These regions are characterized by low rainfall, with most of the wa ...
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Cape Olyutor
Cape Olyutor (russian: мыс Олюторский) is a cape in the Bering Sea, in Koryak Okrug of Kamchatka Krai, Russia. It points south at the southern end of the Olyutor Peninsula, the southern end of the Olyutor Range. Google Earth It was named after the Alyutor ethnic group. The Kereks, a former maritime hunting people of the Russian Bering Sea coast, were living between the cape and the Gulf of Anadyr. See also *Captain Vladimir Voronin Vladimir Ivanovich Voronin (russian: Владимир Иванович Воронин; October 17, 1890 – October 18, 1952) was a Soviet Navy captain, born in Sumsky Posad, in the present Republic of Karelia, Russia. In 1932 he commanded the e ... References * Armstrong, T., The Russians in the Arctic, London, 1958. Landforms of Kamchatka Krai Landforms of the Bering Sea Olyutorsky {{KamchatkaKrai-geo-stub ...
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Olyutor Gulf
The Olyutor Bay (russian: Олюторский залив) is a gulf or bay of the Bering Sea in Olyutorsky District, northern part of Kamchatka Krai, Russia. Geography It is bounded on the west by the Govena Peninsula which separates it from Korfa Bay and on the east by the Olyutor Peninsula, the southern part of the Olyutor Range. Beyond Cape Olyutor lies the Bering Sea.Google Earth It extends roughly inland and is at its widest. The deepest spot is about . The western shore is dominated by the Pylgin Range, which has a maximum elevation of . The bay is normally covered by fast ice from December to May. It has a large tidal range of up to . See also * Shirshov Ridge The Shirshov Ridge is located on the eastern border of the Commander Basin below the Kamchatka Peninsula. It extends directly southward for a distance of 750 km toward the Aleutian arc in the eastern part of the Bering Sea (see figure).E. V ... References Bays of the Bering Sea Bays of Russia ...
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Olyutor Peninsula
Olyutor Peninsula (russian: Олюторский полуостров) is a peninsula in Kamchatka Krai, Russian Federation. The nearest town is Tilichiki, Olyutorsky District. Google Earth The peninsula is named after the Olyutor people, the ancient inhabitants of the area.Leontiev V.V. , Novikova K.A. ''Toponymic dictionary of the North-East of the USSR'' / scientific. ed. G. A. Menovshchikov ; FEB AS USSR . North-East complex. Research Institute. Lab. archeology, history and ethnography. - Magadan: Magadan . book. publishing house , 1989. - S. 290. - 456 p. — ISBN 5-7581-0044-7 . Geography The Olyutor Peninsula is the southern extremity of the Olyutor Range, jutting southwards with the Olyutor Gulf to the west and the Bering Sea to the east. The southern end of the peninsula is Cape Olyutor (Mys Olyutorsky). The peninsula and its attached mountain range to the north are a mainland prolongation of the submerged Shirshov Ridge The Shirshov Ridge is located on the eastern b ...
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