Guardian Nunatak
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Guardian Nunatak
Guardian Nunatak () is a rock exposure, high, on the ice-covered spur that descends from Mount Robert Scott east-northeastward toward the western edge of Hood Glacier, near the juncture with Ross Ice Shelf The Ross Ice Shelf is the largest ice shelf of Antarctica (, an area of roughly and about across: about the size of France). It is several hundred metres thick. The nearly vertical ice front to the open sea is more than long, and between hi .... It is, as it were, guarding the entrance to the glacier, hence the name given by the New Zealand Alpine Club Antarctic Expedition, 1959–60. References Nunataks of Antarctica Dufek Coast {{DufekCoast-geo-stub ...
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Mount Robert Scott
Mount Robert Scott () is a small, flat, snow-covered mountain that rises over 1,000 m and is situated immediately south of Ebony Ridge in the Commonwealth Range. It is lying between Mount Harcourt and Mount Kathleen and overlooking the east side of the Beardmore Glacier at its junction with the Ross Ice Shelf. It was discovered by the British Antarctic Expedition (1907–09) under Ernest Shackleton, who named this feature for Captain Robert F. Scott, RN. Shackleton had been a member of Scott's Southern Polar Party Southern may refer to: Businesses * China Southern Airlines, airline based in Guangzhou, China * Southern Airways, defunct US airline * Southern Air, air cargo transportation company based in Norwalk, Connecticut, US * Southern Airways Express, ... which reached 8217S on the ''Discovery'' expedition (1901–04). Mountains of the Ross Dependency Dufek Coast {{DufekCoast-geo-stub ...
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Hood Glacier
Hood Glacier () is a glacier about long draining northward from Siege Dome in the Commonwealth Range of Antarctica. It enters the Ross Ice Shelf between the Commonwealth Range and the Separation Range. The glacier was discovered by the Southern Polar Party of the British Antarctic Expedition, 1907–09, under Ernest Shackleton, and was named for Admiral Sir Horace Hood, under whom Jameson Adams, a member of the party, had served in HMS ''Berwick''. The outcropping known as the Chevron Rocks Chevron Rocks () is a distinctive rock outcrop at the north end of Retrospect Spur, near the head of Hood Glacier in the Queen Maud Mountains. A New Zealand New Zealand ( mi, Aotearoa ) is an island country in the southwestern Pacific Oc ... is located near the head of Hood Glacier. References Glaciers of Dufek Coast {{DufekCoast-glacier-stub ...
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Ross Ice Shelf
The Ross Ice Shelf is the largest ice shelf of Antarctica (, an area of roughly and about across: about the size of France). It is several hundred metres thick. The nearly vertical ice front to the open sea is more than long, and between high above the water surface. Ninety percent of the floating ice, however, is below the water surface. Most of Ross Ice Shelf is in the Ross Dependency claimed by New Zealand. It floats in, and covers, a large southern portion of the Ross Sea and the entire Roosevelt Island located in the east of the Ross Sea. The ice shelf is named after Sir James Clark Ross, who discovered it on 28 January 1841. It was originally called "The Barrier", with various adjectives including "Great Ice Barrier", as it prevented sailing further south. Ross mapped the ice front eastward to 160° W. In 1947, the U.S. Board on Geographic Names applied the name "Ross Shelf Ice" to this feature and published it in the original U.S. Antarctic Gazetteer. In Januar ...
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New Zealand Alpine Club Antarctic Expedition
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Nunataks Of Antarctica
A nunatak (from Inuit ''nunataq'') is the summit or ridge of a mountain that protrudes from an ice field or glacier that otherwise covers most of the mountain or ridge. They are also called glacial islands. Examples are natural pyramidal peaks. When rounded by glacial action, smaller rock promontories may be referred to as rognons. The word is of Greenlandic origin and has been used in English since the 1870s. Description The term is typically used in areas where a permanent ice sheet is present and the nunataks protrude above the sheet.J. J. Zeeberg, ''Climate and Glacial History of the Novaya Zemlya Archipelago, Russian Arctic''. pp. 82–84 Nunataks present readily identifiable landmark reference points in glaciers or ice caps and are often named. While some nunataks are isolated, sometimes they form dense clusters, such as Queen Louise Land in Greenland. Nunataks are generally angular and jagged, which hampers the formation of glacial ice on their tops, although snow can a ...
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