Russet Pikes
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Russet Pikes
Russet Pikes () are Antarctic peaks just east of the mouth of Gaul Cove on Horseshoe Island. Surveyed by Falkland Islands Dependencies Survey The British Antarctic Survey (BAS) is the United Kingdom's national polar research institute. It has a dual purpose, to conduct polar science, enabling better understanding of global issues, and to provide an active presence in the Antarctic on ... (FIDS) in 1955–57. The name is descriptive; reddish-brown colour is visible on the feature most of the year, the slopes being too steep to retain snow cover for any length of time. Mountains of Graham Land Fallières Coast {{FallièresCoast-geo-stub ...
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Russet Pikes, Antarctica
Russet may refer to: *Russet (cloth), a coarse woolen cloth of brown or grey colour *Russet (color), a dark reddish brown color *Russeting, reddish-brown and coarse anomaly of fruit skin **Russet apple **Russet potato A russet potato is a type of potato that is large, with dark brown skin and few eyes. The flesh is white, dry, soft, and mealy, and it is suitable for baking, mashing, and french fries. Russet potatoes are also known as Idaho potatoes in the Unit ... * Russet, West Virginia, an unincorporated community {{disambig ...
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Gaul Cove
Gaul Cove () is a cove indenting the northeast side of Horseshoe Island, off the coast of Graham Land, Antarctica. It was named by the UK Antarctic Place-Names Committee for Kenneth M. Gaul, first leader of the Falkland Islands Dependencies Survey The British Antarctic Survey (BAS) is the United Kingdom's national polar research institute. It has a dual purpose, to conduct polar science, enabling better understanding of global issues, and to provide an active presence in the Antarctic on ... Horseshoe Island station in 1955. See also * Russet Pikes References Coves of Graham Land Fallières Coast {{FallièresCoast-geo-stub ...
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Horseshoe Island (Antarctica)
Horseshoe Island is an island long and wide occupying most of the entrance to Square Bay, along the west coast of Graham Land, Antarctica. It was discovered and named by the British Graham Land Expedition under John Rymill who mapped the area by land and from the air in 1936–37. Its name is indicative of the crescentic alignment of the peaks which give a comparable shape to the island. Station Y Lying at the north-western end of the island is Station Y , also known as Horseshoe Base, an inactive but relatively unaltered and completely equipped British research station of the late 1950s. It includes ‘Blaiklock’, a nearby refuge hut. The station was occupied from 11 March 1955 to 21 August 1960, when its personnel were transferred to Stonington Island's Station E. In 1969 it was reopened from 7 March to 11 July to complete local survey work. The site has been designated a Historic Site or Monument (HSM 63), following a proposal by the United Kingdom to the Antarctic T ...
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Falkland Islands Dependencies Survey
The British Antarctic Survey (BAS) is the United Kingdom's national polar research institute. It has a dual purpose, to conduct polar science, enabling better understanding of global issues, and to provide an active presence in the Antarctic on behalf of the UK. It is part of the Natural Environment Research Council (NERC). With over 400 staff, BAS takes an active role in Antarctic affairs, operating five research stations, one ship and five aircraft in both polar regions, as well as addressing key global and regional issues. This involves joint research projects with over 40 UK universities and more than 120 national and international collaborations. Having taken shape from activities during World War II, it was known as the Falkland Islands Dependencies Survey until 1962. History Operation Tabarin was a small British expedition in 1943 to establish permanently occupied bases in the Antarctic. It was a joint undertaking by the Admiralty and the Colonial Office. At the end of t ...
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Mountains Of Graham 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 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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