Mount Henderson (Britannia Range)
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Mount Henderson (Britannia Range)
Mount Henderson () is a prominent mountain. It is high, and stands west of Mount Olympus in the Britannia Range of Antarctica. Discovered and named by the British National Antarctic Expedition, 1901-04. Location Mount Henderson is in the western Britannia Range to the south of Derrick Peak and west of Mount Olympus and Mount McClintock. Mount Quackenbush is to the southeast. Features Nearby features include: Mount Selby . A mountain rising over high between Mount Henderson and Mount Olympus. Named by the New Zealand Antarctic Place-Names Committee (NZ-APC) for M.J. Selby, Professor of Earth Sciences, University of Waikato, Hamilton, New Zealand. Selby was a member of field parties in Antarctica, 1969–70, 1971–72, and 1978–79, the last doing geological work in Britannia Range. Tamarus Valley . Ice-free valley lying south of Sabrina Ridge and northeast of Mount Henderson. Named in association with Britannia by a University of Waikato The University of ...
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Britannia Range (Antarctica)
The Britannia Range () is a range of mountains bounded by the Hatherton Glacier and Darwin Glacier (Antarctica), Darwin Glacier on the north and the Byrd Glacier on the south, westward of the Ross Ice Shelf in Antarctica. Exploration and naming The Britannia Range was discovered by the British National Antarctic Expedition (1901–04) under Robert Falcon Scott. It was named after HMS ''Britannia'', a vessel utilized as the Britannia Royal Naval College in England, which had been attended by several officers of Scott's expedition. Location The Britannia Range is east of the Antarctic Plateau. It is south of the Darwin Mountains and the Cook Mountains, which are north of the Hatherton Glacier and the Darwin Glacier (Antarctica), Darwin Glacier. At the mouth of the Darwin Glacier the range adjoins the Gawn Ice Piedmont, which extends into the Ross Ice Shelf to the east. The Byrd Glacier flows northeast past the south side of the Gawn Ice Piedmont. It divides the Britannia Range f ...
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Mount Olympus (Antarctica)
Mount McClintock () is the highest mountain () in the Britannia Range in Antarctica, surmounting the south end of Forbes Ridge, east of Mount Olympus. Discovery and name Mount McClintock was discovered by the British National Antarctic Expedition (BrNAE; 1901–04) and named for Admiral Sir Leopold McClintock, Royal Navy, a member of the Ship Committee for the expedition. Location Mount McClintock is in the central Britannia Range to the east of Mount Olympus. Forbes Ridge extends north from the mountain to the east of Hinton Glacier. Dusky Ridge extends north between Hinton Glacier and Lieske Glacier. Johnstone Ridge extends north from Mount Olympus to the west of Lieske Glacier. Peckham Glacier flows south from Mount McClintock into Byrd Glacier. Mount Quackenbush is to the southwest, and Mount Aldrich is to the northeast. It is located within the claimed Australian Antarctic Territory and is therefore claimed as Australia's highest peak. Western features Feature ...
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British National Antarctic Expedition
The ''Discovery'' Expedition of 1901–1904, known officially as the British National Antarctic Expedition, was the first official British exploration of the Antarctic regions since the voyage of James Clark Ross sixty years earlier (1839–1843). Organized on a large scale under a joint committee of the Royal Society and the Royal Geographical Society (RGS), the new expedition carried out scientific research and geographical exploration in what was then largely an untouched continent. It launched the Antarctic careers of many who would become leading figures in the Heroic Age of Antarctic Exploration, including Robert Falcon Scott who led the expedition, Ernest Shackleton, Edward Wilson, Frank Wild, Tom Crean and William Lashly. Its scientific results covered extensive ground in biology, zoology, geology, meteorology and magnetism. The expedition discovered the existence of the only McMurdo Dry Valleys, snow-free Antarctic valleys, which contains the longest river of ...
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C80202s5 Ant
C8, C08, C.VIII or C-8 may refer to: Transportation Aviation * AEG C.VIII, a World War I German armed reconnaissance aircraft * AGO C.VIII, a World War I German reconnaissance aircraft * Cierva C.8, a 1926 Spanish experimental autogyro * De Havilland Canada C-8 Buffalo, a military transport aircraft of the 1960s * Fairchild C-8, a military transport aircraft of the 1930s * Fokker C.VIII, a 1928 Dutch reconnaissance aircraft * Chicago Express Airlines (defunct) IATA code Automotive * Citroën C8, a brand of minivan * Sauber C8, a 1985 racing car * Spyker C8, a sportscar produced by car manufacturer Spyker Cars * Eighth generation Chevrolet Corvette (C8) Nautical * HMS ''C8'', a 1907 C-class submarine of the Royal Navy * USS ''Raleigh'' (C-8), an 1892 protected cruiser of the United States Navy Rail * LSWR C8 class, a London and South Western Railway locomotive class * C-8 (Cercanías Madrid) * LNER Class C8, a class of 2 4-cylinder compound locomotives ...
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Derrick Peak
Derrick Peak () is a prominent ice-free peak, high, overlooking the south side of Hatherton Glacier, west of the north end of Johnstone Ridge. Name Derrick Peak was named by the Advisory Committee on Antarctic Names for Robert O. Derrick of the United States Weather Bureau, who served as assistant to the United States Antarctic Research Program Representative at Christchurch from 1960 until his death in 1966. Location Derrick Peak is in the north of the Britannia Range, overlooking the Hatherton Glacier to the north, which forms the boundary with the Darwin Mountains. It is east of a line of relatively ice-free valleys and ridges along the south side of Hatherton Glacier, north of Mount Henderson and west of Johnstone Ridge and Dusky Ridge. Most of the nearby features were named in association with Britannia by a University of Waikato (New Zealand) geological party, 1978-79, led by M.J. Selby. Western features Nearby features to the west include: Lindum Valley . Ice- ...
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Mount McClintock
Mount McClintock () is the highest mountain () in the Britannia Range in Antarctica, surmounting the south end of Forbes Ridge, east of Mount Olympus. Discovery and name Mount McClintock was discovered by the British National Antarctic Expedition (BrNAE; 1901–04) and named for Admiral Sir Leopold McClintock, Royal Navy, a member of the Ship Committee for the expedition. Location Mount McClintock is in the central Britannia Range to the east of Mount Olympus. Forbes Ridge extends north from the mountain to the east of Hinton Glacier. Dusky Ridge extends north between Hinton Glacier and Lieske Glacier. Johnstone Ridge extends north from Mount Olympus to the west of Lieske Glacier. Peckham Glacier flows south from Mount McClintock into Byrd Glacier. Mount Quackenbush is to the southwest, and Mount Aldrich is to the northeast. It is located within the claimed Australian Antarctic Territory and is therefore claimed as Australia's highest peak. Western features Feat ...
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Mount Quackenbush
Hughes Basin () is a large basinlike névé which is bounded except to the south by the Ravens Mountains, Mount Henderson, Mount Olympus and Mount Quackenbush. The feature is long and the ice surface descends north–south from near Mount Olympus to near Darnell Nunatak, where there is discharge to Byrd Glacier. Name Hughes Basin was named after Terence J. Hughes of the Department of Geological Sciences and Institute of Quaternary Studies, University of Maine, Orono, who made an intensive study of the Byrd Glacier, 1978-79, entailing photogrammetric determination of the elevation of the ice surface and its velocity, radio-echo sounding from LC-130 aircraft, and ground survey from fixed stations close to Byrd Glacier and moving stations on the glacier itself. Location Hughes Basin is a large circular feature in the southwest of the Britannia Range to the south of Mount Henderson. Features in or surrounding the névé include Mount Henderson, Mount Olympus, Mount Quackenbush ...
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New Zealand Antarctic Place-Names Committee
New Zealand Antarctic Place-Names Committee (NZ-APC) is an adjudicating committee established to authorize the naming of features in the Ross Dependency on the Antarctic continent. It is composed of the members of the New Zealand Geographic Board plus selected specialists on Antarctica. This committee works in collaboration with similar place-naming authorities in Australia, Great Britain and the United States to reach concurrence on each decision. The NZ-APC committee was established in 1956. Names attributed by the committee * Alberich Glacier, named after Alberich, king of the elves and chief of the Nibelungen * Arena Saddle, named in conjunction with Arena Valley * Brawhm Pass, named after the six party members of the University of New South Wales expeditions of 1964–65 and 1966–67 * Caliper Cove, named for descriptive features * Canada Stream, named in conjunction with Canada Glacier * Cape Crossfire, named for descriptive features * Cuneiform Cliffs, named for de ...
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University Of Waikato
The University of Waikato (), established in 1964, is a Public university, public research university located in Hamilton, New Zealand, Hamilton, New Zealand. An additional campus is located in Tauranga. The university performs research in numerous disciplines such as education, social sciences, and management and is an innovator in environmental science, marine and freshwater ecology, engineering and computer science. It offers degrees in health, engineering, computer science, management, Māori language, Māori and Indigenous Studies, the Arts, the arts, psychology, social sciences and education. History In the mid-1950s, regional and national leaders recognised the need for a new university and urged the then University of New Zealand (UNZ) and the government to establish one in Hamilton. Their campaign coincided with a shortage of school teachers, and after years of lobbying, Minister of Education Philip Skoglund agreed to open a teachers' college in the region. In 1960, th ...
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Mountains Of Oates 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 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 climate, mountains te ...
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