Straumsvola Mountain
Straumsvola Mountain () is a prominent mountain 6 nautical miles (11 km) north of Jutulrora Mountain in the northwest part of the Sverdrup Mountains, overlooking the east side of Jutulstraumen Glacier in Queen Maud Land Queen Maud Land () is a roughly region of Antarctica Territorial claims in Antarctica, claimed by Norway as a dependent territory. It borders the claimed British Antarctic Territory 20th meridian west, 20° west, specifically the Caird Coast, .... Plotted from air photos by the German Antarctic Expedition (1938–39). Remapped by Norwegian cartographers from surveys and air photos by Norwegian-British-Swedish Antarctic Expedition (NBSAE) (1949–52) and air photos by the Norwegian expedition (1958–59) and named Straumsvola (the stream mountain). See also * Ottehallet Slope References Mountains of Queen Maud Land Princess Martha Coast {{PrincessMarthaCoast-geo-stub ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Mountain
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 above the surrounding land. A few mountains are inselberg, isolated summits, but most occur in mountain ranges. mountain formation, Mountains are formed through tectonic plate, 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 Slump (geology), slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce Alpine climate, colder climates than at sea level at similar latitude. These colder climates strongly affect the Montane ecosystems, ecosystems of mountains: different elevations hav ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Sverdrup Mountains
The Sverdrup Mountains () are a group of mountains about long, standing just west of the Gjelsvik Mountains in Queen Maud Land, East Antarctica. With its summit at , Hamartind Peak forms the highest point in the Sverdrup Mountains. Discovery and naming First photographed from the air and roughly plotted by the Third German Antarctic Expedition (3rd GAE), 1938–1939. Mapped in detail by Norwegian cartographers from surveys and aerial photographs taken by the Norwegian–British–Swedish Antarctic Expedition (NBSAE), and again by a later Norwegian expedition. Named for Harald Sverdrup, Chairman of the Norwegian Committee for the NBSAE. Norwegian–British–Swedish Antarctic Expedition Norwegian–British–Swedish Antarctic Expedition (NBSAE), 1949–1952 Norwegian Expedition Luncke Expedition, 1958–1959 List of important geographical features of the Sverdrup Mountains See also * List of mountains of Queen Maud Land This list of mountains of Queen Maud Land contai ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Jutulstraumen Glacier
Jutulstraumen Glacier is a large glacier in Queen Maud Land, Antarctica, about long, draining northward to the Fimbul Ice Shelf between the Kirwan Escarpment, Borg Massif and Ahlmann Ridge on the west and the Sverdrup Mountains on the east. It was mapped by Norwegian cartographers from surveys and air photos by the Norwegian–British–Swedish Antarctic Expedition (1949–52) and air photos by the Norwegian expedition (1958–59) and named Jutulstraumen (the giant's stream). More specifically jutulen are troll-like figures from Norwegian folk tales. The ice stream reaches speeds of around 4 metres per day near the coast where it is heavily crevassed. See also * List of glaciers in the Antarctic There are many glaciers in the Antarctic. This set of lists does not include ice sheets, ice caps or ice fields, such as the Antarctic ice sheet, but includes glacial features that are defined by their flow, rather than general bodies of ice ... * List of Antarctic ice stre ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Queen Maud Land
Queen Maud Land () is a roughly region of Antarctica Territorial claims in Antarctica, claimed by Norway as a dependent territory. It borders the claimed British Antarctic Territory 20th meridian west, 20° west, specifically the Caird Coast, Coats Land on the West, and the Australian Antarctic Territory 45th meridian east, 45° east, specifically Enderby Land on the East. In addition, a small unclaimed area from 1939 was annexed in June 2015. Positioned in East Antarctica, it makes out about one-fifth of the continent, and is named after the Norwegian Maud of Wales, Queen Maud (1869–1938). In 1930, the Norwegian Hjalmar Riiser-Larsen was the first person known to have set foot in the territory. On 14 January 1939, the territory was claimed by Norway. On 23 June 1961, Queen Maud Land became part of the Antarctic Treaty System, making it a demilitarised zone. It is one of dependencies of Norway, two Antarctic claims made by Norway, the other being Peter I Island. They are adm ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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New Swabia
New Swabia ( Norwegian and ) was an area of Antarctica explored, with the intention to claim it, by Nazi Germany between 1938 and 1939, within the Norwegian territorial claim of Queen Maud Land. The region was named after the expedition's ship, , itself named after the German region of Swabia.McGonigal, David, Antarctica', frances lincoln ltd, 2009, , p. 367 Although the name "New Swabia" is occasionally mentioned in historical contexts, it is not an officially recognized cartographic name in modern use. The area is now part of Queen Maud Land, governed under the Antarctic Treaty System. Geography New Swabia is divided into an ice-covered northern foreland, which gradually rises from the coast and the edge of the ice shelf to over 1,000 m ( Ritscher Upland and Helle Slope). To the south, it is followed by a region of nunataks rising from the ice and mountain ranges with heights over 3,000 m. These mountain ranges dam up the glaciers of the polar plateau to over 2,000 m. The high ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Ottehallet Slope
Ottehallet Slope () is an ice slope between Straumsvola Mountain and Brekkerista Ridge in the Sverdrup Mountains of Queen Maud Land Queen Maud Land () is a roughly region of Antarctica Territorial claims in Antarctica, claimed by Norway as a dependent territory. It borders the claimed British Antarctic Territory 20th meridian west, 20° west, specifically the Caird Coast, .... Mapped by Norwegian cartographers from surveys and air photos by Norwegian-British-Swedish Antarctic Expedition (NBSAE) (1949–52) and air photos by the Norwegian expedition (1958–59) and named Ottehallet (the early-morning slope). Ice slopes of Queen Maud Land Princess Martha Coast {{PrincessMarthaCoast-geo-stub ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Mountains Of Queen Maud Land
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 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 climate, mountains t ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |