Exodus Valley
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Exodus Valley
Exodus Valley () is a steep moraine-filled valley which descends northward from Midnight Plateau Midnight Plateau () is a prominent ice-covered plateau, over high, forming the central feature of the Darwin Mountains in Antarctica. It is the only area of snow accumulation in the Darwin Mountains. The plateau was discovered by the Victoria Univ ... between Colosseum Ridge and Exodus Glacier, in the Darwin Mountains of Antarctica. It was so named by the Victoria University of Wellington Antarctic Expedition (1962–63) because the valley is virtually the only easy route of descent from Midnight Plateau. References Valleys of Oates Land {{OatesLand-geo-stub ...
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Moraine
A moraine is any accumulation of unconsolidated debris (regolith and rock), sometimes referred to as glacial till, that occurs in both currently and formerly glaciated regions, and that has been previously carried along by a glacier or ice sheet. It may consist of partly rounded particles ranging in size from boulders (in which case it is often referred to as boulder clay) down to gravel and sand, in a groundmass of finely-divided clayey material sometimes called glacial flour. Lateral moraines are those formed at the side of the ice flow, and terminal moraines were formed at the foot, marking the maximum advance of the glacier. Other types of moraine include ground moraines (till-covered areas forming sheets on flat or irregular topography) and medial moraines (moraines formed where two glaciers meet). Etymology The word ''moraine'' is borrowed from French , which in turn is derived from the Savoyard Italian ("mound of earth"). ''Morena'' in this case was derived from Provenà ...
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Midnight Plateau
Midnight Plateau () is a prominent ice-covered plateau, over high, forming the central feature of the Darwin Mountains in Antarctica. It is the only area of snow accumulation in the Darwin Mountains. The plateau was discovered by the 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 clim ... 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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Colosseum Ridge
Colosseum Ridge () is a ridge between Haskell Ridge and Richardson Hill in the Darwin Mountains. The ridge contains pyramidal peaks and five large cirques, the appearance of the latter bearing a resemblance to the Colosseum The Colosseum ( ; it, Colosseo ) is an oval amphitheatre in the centre of the city of Rome, Italy, just east of the Roman Forum. It is the largest ancient amphitheatre ever built, and is still the largest standing amphitheatre in the world to ... in Rome. It was mapped and named by the Victoria University of Wellington Antarctic Expedition (1962–63). References * Further reading * UNITED STATES GEOLOGICAL SURVEY, GAZETTEER OF THE ANTARCTIC', 1989 Ridges of Oates Land Colosseum {{OatesLand-geo-stub ...
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Exodus Glacier
Exodus Glacier is a steep, smooth glacier northeast of Mount Ellis, flowing from the northern edge of Midnight Plateau to the southwest side of Island Arena, in the Darwin Mountains of Antarctica. It was named by the Victoria University of Wellington Antarctic Expedition, 1962–63, in association with nearby Exodus Valley Exodus Valley () is a steep moraine-filled valley which descends northward from Midnight Plateau Midnight Plateau () is a prominent ice-covered plateau, over high, forming the central feature of the Darwin Mountains in Antarctica. It is the only a .... References Glaciers of Oates Land {{OatesLand-glacier-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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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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