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Northrup Head
Suvorov Glacier () is a glacier, 5 nautical miles (9 km) wide, flowing east from the Wilson Hills and discharging into the sea south of Northrup Head and Belousov Point. Mapped by the Soviet Antarctic Expedition, 1958, and named after V.S. Suvorov, Soviet mechanic who perished in the Arctic. See also *Heth Ridge Suvorov Glacier () is a glacier, 5 nautical miles (9 km) wide, flowing east from the Wilson Hills and discharging into the sea south of Northrup Head and Belousov Point. Mapped by the Soviet Antarctic Expedition The Soviet Antarctic ... References Glaciers of Pennell Coast Glaciers of Oates Land {{OatesLand-glacier-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Glacier
A glacier (; ) is a persistent body of dense ice that is constantly moving under its own weight. A glacier forms where the accumulation of snow exceeds its Ablation#Glaciology, ablation over many years, often Century, centuries. It acquires distinguishing features, such as Crevasse, crevasses and Serac, seracs, as it slowly flows and deforms under stresses induced by its weight. As it moves, it abrades rock and debris from its substrate to create landforms such as cirques, moraines, or fjords. Although a glacier may flow into a body of water, it forms only on land and is distinct from the much thinner sea ice and lake ice that form on the surface of bodies of water. On Earth, 99% of glacial ice is contained within vast ice sheets (also known as "continental glaciers") in the polar regions, but glaciers may be found in mountain ranges on every continent other than the Australian mainland, including Oceania's high-latitude oceanic island countries such as New Zealand. Between lati ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Wilson Hills
Wilson Hills () is a group of scattered hills, nunataks and ridges that extend NW-SE for about between Matusevich Glacier and Pryor Glacier in Antarctica. They were discovered by Lieutenant Harry Pennell, Royal Navy, on the Terra Nova Expedition in February 1911 during Robert Falcon Scott's last expedition, and named after Edward Adrian Wilson, a zoologist with the expedition, who perished with Scott on the return journey from the South Pole. Geological features Axthelm Ridge Axthelm Ridge () is a narrow ridge, 4 miles (6 km) long, 1.5 miles (2.4 km) southeast of Parkinson Peak. Mapped by United States Geological Survey (USGS) from surveys and U.S. Navy air photos, 1960–63. Named by Advisory Committee on Antarctic Names (US-ACAN) for Commander Charles E. Axthelm, U.S. Navy, Flag Secretary to the Commander of the U.S. Naval Support Force, Antarctica, during Operation Deep Freeze 1969 and 1970; executive officer on the USS ''Glacier'' during Operation Deep Fre ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Northrup Head
Suvorov Glacier () is a glacier, 5 nautical miles (9 km) wide, flowing east from the Wilson Hills and discharging into the sea south of Northrup Head and Belousov Point. Mapped by the Soviet Antarctic Expedition, 1958, and named after V.S. Suvorov, Soviet mechanic who perished in the Arctic. See also *Heth Ridge Suvorov Glacier () is a glacier, 5 nautical miles (9 km) wide, flowing east from the Wilson Hills and discharging into the sea south of Northrup Head and Belousov Point. Mapped by the Soviet Antarctic Expedition The Soviet Antarctic ... References Glaciers of Pennell Coast Glaciers of Oates Land {{OatesLand-glacier-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Belousov Point
Belousov Point () is an ice-covered headland forming the southern tip of the Anderson Peninsula, located just north of the terminus of Suvorov Glacier, situated in Victoria Land, Antarctica. The geographical headland was first mapped by the Soviet Antarctic Expedition of 1958 and named for the Soviet polar captain Mikhail P. Belousov, 1904–46. The headland lies on the Pennell Coast, a portion of Antarctica lying between Cape Williams and Cape Adare Cape Adare is a prominent cape of black basalt forming the northern tip of the Adare Peninsula and the north-easternmost extremity of Victoria Land, East Antarctica. Description Marking the north end of Borchgrevink Coast and the west e .... References * Headlands of Victoria Land Pennell Coast {{VictoriaLand-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Soviet Antarctic Expedition
The Soviet Antarctic Expedition (SAE or SovAE) (russian: Советская антарктическая экспедиция, САЭ, ''Sovetskaya antarkticheskaya ekspeditsiya'') was part of the Arctic and Antarctic Research Institute of the Soviet Committee on Antarctic Research of the Academy of Sciences of the USSR. The Soviet Union's Ministry of Sea Transport was responsible for the administration, logistics and supply of the expeditions. The first Soviet contact with Antarctica was in January 1947 when the Slava whaling flotilla began whaling in Antarctic waters. Stations The first Soviet Antarctic station, '' Mirny'', was established near the coast on February 13, 1956. This was added to in December 1957 by another station, ''Vostok'' built inland near the south geomagnetic pole. Year-round stations * Mirny (established February 13, 1956) * Vostok (established December 16, 1957) * Novolazarevskaya (established January 18, 1961) * Molodyozhnaya (established January 1 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Heth Ridge
Suvorov Glacier () is a glacier, 5 nautical miles (9 km) wide, flowing east from the Wilson Hills and discharging into the sea south of Northrup Head and Belousov Point. Mapped by the Soviet Antarctic Expedition The Soviet Antarctic Expedition (SAE or SovAE) (russian: Советская антарктическая экспедиция, САЭ, ''Sovetskaya antarkticheskaya ekspeditsiya'') was part of the Arctic and Antarctic Research Institute of the So ..., 1958, and named after V.S. Suvorov, Soviet mechanic who perished in the Arctic. See also * Heth Ridge References Glaciers of Pennell Coast Glaciers of Oates Land {{OatesLand-glacier-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Glaciers Of Pennell Coast
A glacier (; ) is a persistent body of dense ice that is constantly moving under its own weight. A glacier forms where the accumulation of snow exceeds its ablation over many years, often centuries. It acquires distinguishing features, such as crevasses and seracs, as it slowly flows and deforms under stresses induced by its weight. As it moves, it abrades rock and debris from its substrate to create landforms such as cirques, moraines, or fjords. Although a glacier may flow into a body of water, it forms only on land and is distinct from the much thinner sea ice and lake ice that form on the surface of bodies of water. On Earth, 99% of glacial ice is contained within vast ice sheets (also known as "continental glaciers") in the polar regions, but glaciers may be found in mountain ranges on every continent other than the Australian mainland, including Oceania's high-latitude oceanic island countries such as New Zealand. Between latitudes 35°N and 35°S, glaciers occur only in ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
