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Sphinx Peak
The Destination Nunataks () are a group of peaks and nunataks, long and wide, rising to at Pyramid Peak and including Sphinx Peak, Andrews Peak, Mummy Ridge, and unnamed nunataks to the northwest, located in northeast Evans Névé, northwest of the Barker Range, Victoria Land, Antarctica. Exploration and naming This group was visited in 1970–71 by a Victoria University of Wellington Antarctic Expedition (VUWAE) geological party led by M.G. Laird. The name "Destination Rocks" was originally used for the feature because these nunataks were near the northern limits of Laird's expedition. The name Destination Nunataks, as approved by the New Zealand Antarctic Place-Names Committee (NZ-APC) and the United States Advisory Committee on Antarctic Names (US-ACAN) in 1985, applies to the entire group described rather than to just two nunataks at the southeast end as indicated on some maps. Location The Destination Nunataks lie at the end of a ridge extended southeast from the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 78th parallel south, 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 Victoria of the United Kingdom, 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. History Early explorers of Victoria Land include James Clark Ross and Douglas Mawson. In 1979, scientists discovered a group of 309 Meteorite, meteorites in Antarctica, some of which were found near the Allan Hills in Victoria Land. The meteorites appeared to have undergone little change since they were formed at what scientists believe was the birth of the Solar System. In 1981, Lichen, lichens fo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Nunatak
A nunatak (from Inuit language, Inuit ) 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 often form natural pyramidal peaks. Isolated nunataks are also called glacial islands, and smaller nunataks rounded by glacial action may be referred to as rognons. The word is of Greenlandic language, Greenlandic origin and has been used in English since the 1870s. Description The term ''nunatak'' is typically used in areas where a permanent ice sheet is present and the ridge protrudes 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 are isolated, they can also form dense clusters, such as Queen Louise Land in Greenland. Nunataks are generally angular and jagged, hampering the formation of glacial ice on thei ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Evans Névé
Rennick Glacier () is a broad glacier, nearly long, which is one of the largest in Antarctica. It rises on the polar plateau westward of Mesa Range and is wide, narrowing to near the coast. It takes its name from Rennick Bay where the glacier reaches the sea. Early exploration The seaward part of the glacier was photographed by United States Navy Operation Highjump, 1946–47. The upper reaches of the Rennick Glacier were discovered and explored by the U.S. Victoria Land Traverse (VLT) in February 1960, and the first ascent made of Welcome Mountain by John Weihaupt, Alfred Stuart, Claude Lorius and Arnold Heine of the VLT party. On February 10, 1960, Lieutenant Commander Robert L. Dale, pilot of U.S. Navy (USN) Squadron VX-6, evacuated the VLT from , on this glacier, and then conducted an aerial photographic reconnaissance to Rennick Bay on the coast before returning the VLT team to McMurdo Station. Course The Rennick Glacier rises to the east of the Tobin Mesa in th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Barker Range
Barker Range () is a mountain range trending northwest–southeast and including Jato Nunatak, Mount Watt, Mount McCarthy, and Mount Burton, located at the southwest side of the Millen Range in the Victory Mountains, Victoria Land, Antarctica. It was named by the New Zealand Antarctic Place-Names Committee (NZ-APC) for James Barker, leader at Scott Base, 1972. Location The Barker Range is southeast of the Destination Nunataks. It is to the east of the Evans Névé and the head of the Mariner Glacier. The Webb Névé is to the south of the range. The Miller Range of the Victory Mountains is to the east. At the east of the range, the Wood Glacier flowing from the northwest converges with Osuga Glacier from the southwest to form Trafalgar Glacier. Features Jato Nunatak . A small but distinctive nunatak at the north end of Barker Range. Named by the Southern Party of the New Zealand Federated Mountain Clubs Antarctic Expedition (NZFMCAE), 1962-63, after the JATO bottles used ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Victoria University Of Wellington Antarctic Expedition
The Antarctic Research Centre (ARC) is part of the School of Geography, Environment and Earth Sciences at Victoria University of Wellington. Its mission is to research " Antarctic climate history and processes, and their influence on the global climate system. The current director of the Antarctic Research Centre is Associate Professor Robert McKay. Directors * 1972–2007: Professor Peter Barrett * 2008–2016: Professor Tim Naish * 2017–2019: Professor Andrew Mackintosh * 2020–present: Professor Robert McKay History In December 1957, geology students Barrie McKelvey and Peter Webb along with biologist Ron Balham conducted an expedition to the then unexplored McMurdo Dry Valleys via the Royal New Zealand Navy Antarctic support ship HMNZS ''Endeavour''. This expedition formed the basic for the annual Victoria University of Wellington Antarctic Expeditions, which continue to the present day. Since this first expedition, over 400 staff and students have travelled to t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Advisory Committee On Antarctic Names
The Advisory Committee on Antarctic Names (ACAN or US-ACAN) is an advisory committee of the United States Board on Geographic Names responsible for recommending commemorative names for features in Antarctica. History The committee was established in 1943 as the Special Committee on Antarctic Names (SCAN). It became the Advisory Committee on Antarctic Names in 1947. Fred G. Alberts was Secretary of the Committee from 1949 to 1980. By 1959, a structured nomenclature was reached, allowing for further exploration, structured mapping of the region and a unique naming system. A 1990 ACAN gazeeter of Antarctica listed 16,000 names. Description The United States does not recognise territorial boundaries within Antarctica, so ACAN assigns names to features anywhere within the continent, in consultation with other national nomenclature bodies where appropriate, as defined by the Antarctic Treaty System. The research and staff support for the ACAN is provided by the United States Geologi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
C72193s5 Ant
C7, C07 or C-7 may refer to: Vehicles (including military) * C-7 Caribou, a military transport aircraft * AEG C.VII, a World War I German armed reconnaissance aircraft * AGO C.VII, a World War I German reconnaissance aircraft * Albatros C.VII, a World War I German military reconnaissance aircraft * C-7, a United States Navy C class blimp and the first airship inflated with helium * Chevrolet Corvette (C7), the seventh generation of a sports car made by General Motors * Fokker C.VII, a 1928 Dutch reconnaissance seaplane * HMS ''C7'', a British Royal Navy C-class submarine * Sauber C7, a 1983 Group C prototype race car * USS ''Cincinnati'' (C-7), a United States Navy protected cruiser Science * Caldwell 7 (NGC 2403), a spiral galaxy in Camelopardalis Technology * Nokia C7-00, a touch screen mobile from Nokia * VIA C7, an IA-32 central processing unit by VIA Technologies * C7, an incandescent light bulb of the size typically used in nightlights and Christmas lighting usually ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
West Quartzite Range
West Quartzite Range () is a range, the western of two parallel quartzite ranges, situated at the east side of Houliston Glacier in the Concord Mountains, Antarctica. It was named by the Northern Party of the New Zealand Federated Mountain Clubs Antarctic Expedition (NZFMCAE), 1962–63, after the distinctive geological formation of the feature. Location The West Quartzite Range is part of the Concord Mountains. The range runs northwest–southeast, parallel to the East Quartzite Range to the east. The Houliston Glacier to its west separates it from the Neall Massif and Jago Nunataks. The Salamander Range of the Freyberg Mountains is further to the west. The line of the range extends towards the Destination Nunataks to the southeast. The Black Glacier lies to the north of the Leitch Massif, the northern end of the range. Features Leitch Massif . A mountain massif that forms the northern part of the West Quartzite Range. Named by the northern party of NZFMCAE, 1962-6 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Millen Range
The Millen Range () is a prominent northwest–southeast trending mountain range, located west of the Cartographers Range in the Victory Mountains of Antarctica. Peaks in the range include Inferno, Omega, Le Couteur, Head, Cirque, Gless, Turret, Crosscut and Mount Aorangi. It was named by the New Zealand Federated Mountain Clubs Antarctic Expedition (NZFMCAE) of 1962–63, for John M. Millen, leader of the expedition. Location The Millen Range in the western Victory Mountains extends in a southeast direction to the east of the East Quartzite Range, Destination Nunataks and Barker Range. It is bounded to the east by the Pearl Harbor Glacier, Muller Glacier, Lensen Glacier and Wood Glacier. Features Features include, from northwest to southeast, Inferno Peak . A peak north of Le Couteur Peak in the north end of Millen Range. So named by the Southern Party of NZFMCAE, 1962-63, because geologic examination showed it contained the granite/greywacke contact, with baking of ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Victory Mountains
The Victory Mountains () are a major group of mountains in Victoria Land, Antarctica, about long and wide, which is bounded primarily by Mariner and Tucker glaciers and the Ross Sea. They are north of the Mountaineer Range, east of the Freyberg Mountains and south of the Concord Mountains and the Admiralty Mountains. The division between the Victory Mountains and the Concord Mountains (to the northwest) is not precise but apparently lies in the vicinity of Thomson Peak. Exploration and name A Ross Sea aspect of the mountains was first obtained by early British expeditions of James Clark Ross, Carsten Borchgrevink, Robert Falcon Scott and Ernest Shackleton. The mapping of the interior mountains was largely done from air photos taken by the United States Navy and surveys undertaken by New Zealand and American parties in the 1950s and 1960s. The Victory Mountains were named by the New Zealand Geological Survey Antarctic Expedition (NZGSAE) 1957-58, because of the proximity ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Salamander Range
Salamander Range () is a distinctive linear range between Canham Glacier and Black Glacier, in the Freyberg Mountains, Antarctica. The range was named by the Northern Party of New Zealand Geological Survey Antarctic Expedition (NZGSAE), 1963–64, from the nickname given to Lord Freyberg by Sir Winston Churchill, for the lizard that is untouched by fire. Location The Salamander Range runs from northwest to southeast between the Canham Glacier to the west and the Black Glacier to the east. The Lanterman Range is to the north and the Leitch Massif to the northwest. The Alamein Range is west of the Canham Glacier and the Neall Massif and West Quartzite Range are east of the Black Glacier. The Evans Névé is to the south. Features of the range include, from north to south, Galatos Peak, Mount Pedersen, Mount Apolotok, Mount Hennessey, Mount Tukotok and Mount Staley. Mello Nunatak.and Symes Nunatak are to the south. Features Geographical features of Salamander Range incl ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
