Husky Dome
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Husky Dome
Husky Dome () is a snow dome rising to , marking the highest point of the Husky Heights, between the heads of Brandau Glacier and Ramsey Glacier in the Queen Maud Mountains of Antarctica. It was named by the New Zealand Geological Survey Antarctic Expedition, 1961–62, after their Husky Husky is a general term for a dog used in the polar regions, primarily and specifically for work as sled dogs. It refers to a traditional northern type, notable for its cold-weather tolerance and overall hardiness. Modern racing huskies that mai ... dogs which they drove to the summit of this feature. References Mountains of the Ross Dependency Dufek Coast {{DufekCoast-geo-stub ...
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Husky Heights
The Husky Heights () are relatively flat, ice-covered heights southeast of Haynes Table, overlooking the head of Brandau Glacier in the Queen Maud Mountains of Antarctica. They were named by the Advisory Committee on Antarctic Names in association with Husky Dome Husky Dome () is a snow dome rising to , marking the highest point of the Husky Heights, between the heads of Brandau Glacier and Ramsey Glacier in the Queen Maud Mountains of Antarctica. It was named by the New Zealand Geological Survey Antarctic ..., the highest point on these heights. References Mountains of the Ross Dependency Dufek Coast {{DufekCoast-geo-stub ...
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Brandau Glacier
Brandau Glacier () is a wide tributary glacier, long, flowing westward from an ice divide between Haynes Table and Husky Heights to enter Keltie Glacier just west of Ford Spur. It was named by the Advisory Committee on Antarctic Names for Lieutenant Commander James F. Brandau, U.S. Navy, a pilot with Squadron VX-6, Operation Deepfreeze 1964 and 1965. See also * Advisory Committee on Antarctic Names * Glaciology * 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. Th ... References Glaciers of Dufek Coast {{DufekCoast-glacier-stub ...
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Ramsey Glacier
Ramsey Glacier () is a glacier about 45 nautical miles (80 km) long, originating in the Bush Mountains near the edge of the polar plateau and flowing north to the Ross Ice Shelf eastward of Den Hartog Peak. Discovered by the United States Antarctic Service (USAS) on Flight C of February 29-March 1, 1940, and named by Advisory Committee on Antarctic Names (US-ACAN), on the recommendation of R. Admiral Byrd, for Admiral DeWitt Clinton Ramsey, U.S. Navy, Vice Chief A vice is a practice, behaviour, or habit generally considered immoral, sinful, criminal, rude, taboo, depraved, degrading, deviant or perverted in the associated society. In more minor usage, vice can refer to a fault, a negative character tra ... of Naval Operations during U.S. Navy Operation Highjump, 1946–47. See also * Four Ramps References Glaciers of Dufek Coast {{DufekCoast-glacier-stub ...
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Queen Maud Mountains
The Queen Maud Mountains are a major group of mountains, ranges and subordinate features of the Transantarctic Mountains, lying between the Beardmore and Reedy Glaciers and including the area from the head of the Ross Ice Shelf to the Antarctic Plateau in Antarctica. Captain Roald Amundsen and his South Pole party ascended Axel Heiberg Glacier near the central part of this group in November 1911, naming these mountains for the Norwegian queen Maud of Wales. Despite the name, they are not located within Queen Maud Land. Elevations bordering the Beardmore Glacier, at the western extremity of these mountains, were observed by the British expeditions led by Ernest Shackleton (1907–09) and Robert Falcon Scott (1910-13), but the mountains as a whole were mapped by several American expeditions led by Richard Evelyn Byrd (1930s and 1940s), and United States Antarctic Program (USARP) and New Zealand Antarctic Research Program (NZARP) expeditions from the 1950s through the 1970s. Featu ...
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New Zealand Geological Survey Antarctic Expedition
The New Zealand Geological Survey Antarctic Expedition (NZGSAE) describes a series of scientific explorations of the continent Antarctica. The expeditions were notably active throughout the 1950s and 1960s. Features named by the expeditions 1957–1958 expedition The 1957–1958 expedition went to the Ross Dependency and named the Borchgrevink Glacier. Other features named include: * Carter Ridge * Felsite Island * Halfway Nunatak * Hedgehog Island * Moraine Ridge 1958–1959 expedition * Cadwalader Beach * Cape Hodgson * Carter Ridge * Isolation Point * Mountaineer Range * Mount Aurora * Mount Hayward * Mount Henderson (White Island) * Mount Bird. 1960–1961 expedition * Deverall Island * Lonewolf Nunataks 1961–1962 expedition * Aurora Heights * The Boil * Ford Spur * Graphite Peak * Half Century Nunatak * Half Dome Nunatak * Hump Passage * Last Cache Nunatak * Lookout Dome * Montgomerie Glacier * Mount Fyfe * Mount Macdonald * Snowshoe Pass * Turret Nu ...
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Husky
Husky is a general term for a dog used in the polar regions, primarily and specifically for work as sled dogs. It refers to a traditional northern type, notable for its cold-weather tolerance and overall hardiness. Modern racing huskies that maintain arctic breed traits (also known as Alaskan huskies) represent an ever-changing crossbreed of the fastest dogs. Huskies have continued to be used in sled-dog racing, as well as expedition and trek style tour businesses, and as a means of essential transportation in rural communities. Huskies are also kept as pets, and groups work to find new pet homes for retired racing and adventure-trekking dogs. History Nearly all dogs' genetic closeness to the gray wolf is due to admixture. However, several Arctic breeds also show a genetic closeness with the now-extinct Taimyr wolf of North Asia due to admixture: the Siberian Husky and Greenland Dog (which are also historically associated with Arctic human populations) and to a lesser ex ...
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Mountains Of The Ross Dependency
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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