Mount Ellis (Gallatin County, Montana)
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Mount Ellis (Gallatin County, Montana)
Midnight Plateau () is a prominent ice-covered plateau, over high, forming the central feature of the Darwin Mountains in Antarctica Antarctica () is Earth's southernmost and least-populated continent. Situated almost entirely south of the Antarctic Circle and surrounded by the Southern Ocean, it contains the geographic South Pole. Antarctica is the fifth-largest contine .... It is the only area of snow accumulation in the Darwin Mountains. The plateau was discovered by the Victoria University of Wellington Antarctic Expedition of 1962–63 and so named because the feature was visited by expedition members at midnight on December 27, 1962. Further reading * Gunter Faure, Teresa M. Mensing, 'The Transantarctic Mountains: Rocks, Ice, Meteorites and Water'', P 298 References Plateaus of Oates Land East Antarctica {{OatesLand-geo-stub ...
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Darwin Mountains
The Darwin Mountains is a group of mountains between the Darwin and Hatherton glaciers in Antarctica. Discovered by the British National Antarctic Expedition (1901–04) and named for Major Leonard Darwin, at that time Honorary Secretary of the Royal Geographical Society. Features * Access Slope * Colosseum Ridge * Communication Heights * Conant Valley * Corell Cirque * Darwin Glacier * Darwin Névé * Duncan Bluff * Exodus Glacier * Exodus Valley * Friedmann Peak * Grant Valley * Green Glacier * Hale Valley * Harvey Cirque * Haskell Ridge * Hatherton Glacier * Island Arena * Junction Spur * Kennett Ridge * Lindstrom Ridge * Mason Nunatak * McKay Valley * Meteorite Hills * Midnight Plateau * Misthound Cirque * Mount Ash * Mount Ellis * Muchmore Valley * Overturn Glacier * Polarmail Ledge * Prebble Icefalls * Richardson Hill * Scheuermann Spur * Score Ridge * Skilton Ledge * Smith Heights Smith Heights () is the highest part of the jumble of peaks betwe ...
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Antarctica
Antarctica () is Earth's southernmost and least-populated continent. Situated almost entirely south of the Antarctic Circle and surrounded by the Southern Ocean, it contains the geographic South Pole. Antarctica is the fifth-largest continent, being about 40% larger than Europe, and has an area of . Most of Antarctica is covered by the Antarctic ice sheet, with an average thickness of . Antarctica is, on average, the coldest, driest, and windiest of the continents, and it has the highest average elevation. It is mainly a polar desert, with annual precipitation of over along the coast and far less inland. About 70% of the world's freshwater reserves are frozen in Antarctica, which, if melted, would raise global sea levels by almost . Antarctica holds the record for the lowest measured temperature on Earth, . The coastal regions can reach temperatures over in summer. Native species of animals include mites, nematodes, penguins, seals and tardigrades. Where vegetation o ...
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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 the ...
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Plateaus Of Oates Land
In geology and physical geography, a plateau (; ; ), also called a high plain or a tableland, is an area of a highland consisting of flat terrain that is raised sharply above the surrounding area on at least one side. Often one or more sides have deep hills or escarpments. Plateaus can be formed by a number of processes, including upwelling of volcanic magma, extrusion of lava, and erosion by water and glaciers. Plateaus are classified according to their surrounding environment as intermontane, piedmont, or continental. A few plateaus may have a small flat top while others have wide ones. Formation Plateaus can be formed by a number of processes, including upwelling of volcanic magma, extrusion of lava, Plate tectonics movements and erosion by water and glaciers. Volcanic Volcanic plateaus are produced by volcanic activity. The Columbia Plateau in the north-western United States is an example. They may be formed by upwelling of volcanic magma or extrusion of lava. The un ...
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