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Tot Pond
Tot Pond is the smaller and western of two closely spaced frozen ponds in the floor of Alatna Valley, filled by overflow from the larger adjacent Rum Pond, in the Convoy Range, Victoria Land. Named by a 1989-90 New Zealand Antarctic Research Program (NZARP) field party (Trevor Chinn Sir Trevor Edwin Chinn (born 24 July 1935) is a British businessman, philanthropist, and political activist. Business career Chinn was educated at Clifton College and King's College, Cambridge and started his career at Lex Garages (later Le ...) in association with Rum Pond; in nautical circles a tot is a traditional small issue of rum. Lakes of Victoria Land Scott Coast {{ScottCoast-geo-stub ...
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Alatna Valley
Alatna Valley (sometimes incorrectly spelled ''Atlanta Valley'') is an ice-free valley lying 4 miles (6 km) north of Mount Gran and trending east-northeast for about 10 miles (16 km) along the southeast side of the Convoy Range. It is one of the northernmost of the McMurdo Dry Valleys. Parker Calkin, U.S. geologist, made stratigraphic studies in the valley during the 1960–1961 season. Named by Advisory Committee on Antarctic Names in 1963 for the gasoline tanker which participated in Operation Deep Freeze Operation Deep Freeze (OpDFrz or ODF) is codename for a series of United States missions to Antarctica, beginning with "Operation Deep Freeze I" in 1955–56, followed by "Operation Deep Freeze II", "Operation Deep Freeze III", and so on. (There w ... 1958–1959 and 1959–1960, and in keeping with other ship names in the Convoy Range. References * Valleys of Victoria Land McMurdo Dry Valleys {{McMurdoDryValleys-geo-stub ...
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Rum Pond
Rum Pond () is the larger and eastern of two closely spaced frozen ponds in the floor of Alatna Valley, Convoy Range, in Victoria Land Victoria Land is a region in eastern Antarctica which fronts the western side of the Ross Sea and the Ross Ice Shelf, extending southward from about 70°30'S to 78°00'S, and westward from the Ross Sea to the edge of the Antarctic Plateau. I .... The name is one of a group in Convoy Range reflecting a nautical theme. Named after this traditional naval beverage by a 1989-90 New Zealand Antarctic Research Program (NZARP) field party. Lakes of Victoria Land Scott Coast {{ScottCoast-geo-stub ...
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Convoy Range
Convoy Range () is a broad mountain range in Antarctica. Much of the range has a nearly flat plateau-like summit, extending south from the Fry Saddle and ending at Mackay Glacier. The range has steep cliffs on its east side, but it slopes gently into the Cambridge Glacier on the western side. The New Zealand Northern Survey Party of the Commonwealth Trans-Antarctic Expedition (1956–58) worked in this area in 1957. The party named the range for the main convoy into McMurdo Sound in the 1956–57 season, with the names of the various vessels being used for features in the range. Features Taff Y Bryn () is a ridgelike summit capped by dolerite (about 1,600 m), situated 1 nautical mile (1.9 km) west of Flagship Mountain in the Convoy Range. It is named after the River Taff in Wales, the toponym in Welsh literally means "Hill of the Taff." It was named by the 1976–77 Victoria University of Wellington Antarctic Expedition (VUWAE) led by Christopher J. Burgess. Othe ...
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Victoria Land
Victoria Land is a region in eastern Antarctica which fronts the western side of the Ross Sea and the Ross Ice Shelf, extending southward from about 70°30'S to 78°00'S, and westward from the Ross Sea to the edge of the Antarctic Plateau. It was discovered by Captain James Clark Ross in January 1841 and named after Queen Victoria. The rocky promontory of Minna Bluff is often regarded as the southernmost point of Victoria Land, and separates the Scott Coast to the north from the Hillary Coast of the Ross Dependency to the south. The region includes ranges of the Transantarctic Mountains and the McMurdo Dry Valleys (the highest point being Mount Abbott in the Northern Foothills), and the flatlands known as the Labyrinth. The Mount Melbourne is an active volcano in Victoria Land. Early explorers of Victoria Land include James Clark Ross and Douglas Mawson. In 1979, scientists discovered a group of 309 meteorites in Antarctica, some of which were found near the Allan Hills in ...
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Trevor Chinn (glaciologist)
Trevor James Hill Chinn (9 August 1937 – 20 December 2018) was a New Zealand glaciologist, who conducted extensive surveys of the glaciers of New Zealand's Southern Alps. Early life Growing up near the town of Te Taho (about eight kilometers from Whataroa) in South Westland, near the Franz Josef Glacier, Trevor Chinn was fascinated by water and glaciers at an early age. While at the University of Canterbury Chinn joined the tramping club, and graduated with a BSc in geology. Trevor was the second of four children to Alfred and Myrtle (née Sweney) Chinn. Career During the early 1960s Chinn worked for the North Canterbury Catchment Board, near Christchurch. In his role as field hydrologist, Chinn quickly learned the elements of river gauging and meticulous record keeping. Following a training period with the Ministry of Works, Chinn was invited to apply for a field role carrying out snow surveys on the Tasman Glacier and in the wider Mackenzie Basin. This new job was with t ...
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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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