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Lake Garwood
Lake Garwood is a lake at the lower end of Garwood Valley on the Scott Coast of Victoria Land, Antarctica. The lake receives meltwater from Garwood Glacier at the valley head. It was named by Thomas Griffith Taylor Thomas Griffith "Grif" Taylor (1 December 1880 – 5 November 1963) was an English-born geographer, anthropologist and world explorer. He was a survivor of Captain Robert Scott's Terra Nova Expedition to Antarctica (1910–1913). Taylor was a se ... of the British Antarctic Expedition, 1910–13, in association with Garwood Glacier. References Lakes of Victoria Land Scott Coast {{ScottCoast-geo-stub ...
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Garwood Valley
Garwood Valley () is a valley opening on the coast of Victoria Land, Antarctica, just south of Cape Chocolate. It is largely ice-free, but is occupied near its head by the Garwood Glacier. It was named by Thomas Griffith Taylor Thomas Griffith "Grif" Taylor (1 December 1880 – 5 November 1963) was an English-born geographer, anthropologist and world explorer. He was a survivor of Captain Robert Scott's Terra Nova Expedition to Antarctica (1910–1913). Taylor was a se ... of the British Antarctic Expedition, 1910–13, in association with Garwood Glacier. References Valleys of Victoria Land McMurdo Dry Valleys {{McMurdoDryValleys-geo-stub ...
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Garwood Glacier
Garwood Glacier () is a glacier occupying the northwest part of Garwood Valley, in Victoria Land, Antarctica. It was first mapped by the British National Antarctic Expedition (1901–04), but was not named until 1911, when Thomas Griffith Taylor of the British Antarctic Expedition, 1910–13, named it for Edmund J. Garwood, professor of geology and mineralogy at the University of London. Projection Peak rises above its head at the most southeastern point of Hobbs Ridge. See also * Colleen Lake * List of glaciers in the Antarctic * Glaciology Glaciology (; ) is the scientific study of glaciers, or more generally ice and natural phenomena that involve ice. Glaciology is an interdisciplinary Earth science that integrates geophysics, geology, physical geography, geomorphology, climato ... References Glaciers of Scott Coast {{ScottCoast-glacier-stub ...
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Valley Head
The head of the valley or, less commonly, the valley head, refers to the uppermost part of a valley.Leser (2005), p. 935. Description The head of a valley may take widely differing forms; for example, in highland regions the valley often ends in a broad, evenly sloping hollow. The higher the head of the valley, the more likely it is to resemble the geomorphological shape of a cirque. In glacial valleys or trough valleys, it may be referred to as the trough head or trough end.Leser (2005), p. 978. In mountains with predominantly crystalline rock the heads of the valleys are generally very wet, sometimes boggy and often support lush alpine meadows, whilst those made of limestone are usually dry and covered in talus or gravel. Where there has been ice age glaciation, the valley bottoms are modified by moraines and mountain lakes are common. See also * Structural basin * U-shaped or trough valley * Landform * Valley step A valley step (german: Talstufe or ''Talschwelle'') i ...
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Thomas Griffith Taylor
Thomas Griffith "Grif" Taylor (1 December 1880 – 5 November 1963) was an English-born geographer, anthropologist and world explorer. He was a survivor of Captain Robert Scott's Terra Nova Expedition to Antarctica (1910–1913). Taylor was a senior academic geographer at universities in Sydney, Chicago, and Toronto. His writings on geography and race were controversial. Early life Taylor was born in the town of Walthamstow, England, to parents James Taylor, a metallurgical chemist, and Lily Agnes, née Griffiths. Within a year after his birth, the family had moved to Serbia where his father was manager of a copper mine. Three years later, they returned to Britain when his father became director of analytical chemistry for a major steelworks company. In 1893, the family emigrated to New South Wales Australia, where James secured a position as a government metallurgist. Taylor, age 13, attended The King's School in Sydney. He enrolled in arts at the University of Sydney in 1899, ...
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British Antarctic Expedition, 1910–13
The ''Terra Nova'' Expedition, officially the British Antarctic Expedition, was an expedition to Antarctica which took place between 1910 and 1913. Led by Captain Robert Falcon Scott, the expedition had various scientific and geographical objectives. Scott wished to continue the scientific work that he had begun when leading the ''Discovery'' Expedition from 1901 to 1904, and wanted to be the first to reach the geographic South Pole. He and four companions attained the pole on 17 January 1912, where they found that a Norwegian team led by Roald Amundsen had preceded them by 34 days. Scott's party of five died on the return journey from the pole; some of their bodies, journals, and photographs were found by a search party eight months later. The expedition, named after its supply ship, was a private venture financed by public contributions and a government grant. It had further backing from the Admiralty, which released experienced seamen to the expedition, and from the Royal ...
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Lakes Of Victoria Land
A lake is an area filled with water, localized in a basin, surrounded by land, and distinct from any river or other outlet that serves to feed or drain the lake. Lakes lie on land and are not part of the ocean, although, like the much larger oceans, they do form part of the Earth's water cycle. Lakes are distinct from lagoons, which are generally coastal parts of the ocean. Lakes are typically larger and deeper than ponds, which also lie on land, though there are no official or scientific definitions. Lakes can be contrasted with rivers or streams, which usually flow in a channel on land. Most lakes are fed and drained by rivers and streams. Natural lakes are generally found in mountainous areas, rift zones, and areas with ongoing glaciation. Other lakes are found in endorheic basins or along the courses of mature rivers, where a river channel has widened into a basin. Some parts of the world have many lakes formed by the chaotic drainage patterns left over from the last ice ...
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