Island Arena

	Island Arena Island Arena () is a broad valley occupied by a lateral lobe of the Darwin Glacier, Antarctica, indenting the north side of the Darwin Mountains between Colosseum Ridge and Kennett Ridge. An islandlike nunatak, Richardson Hill, rises above the ice of the valley. The descriptive name was given 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 clima ... (1962–63). References Landforms of Oates Land Valleys of Antarctica {{OatesLand-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu]
	Darwin Glacier (Antarctica) Darwin Glacier () is a large glacier in Antarctica. It flows from the polar plateau eastward between the Darwin Mountains and the Cook Mountains to the Ross Ice Shelf. The lower part of the glacier was mapped by the British National Antarctic Expedition, 1901–04, and the whole area traversed by New Zealand parties of the Commonwealth Trans-Antarctic Expedition (1956–58). The glacier was named in association with the Darwin Mountains (themselves named after Leonard Darwin). Robertson Buttress is the westernmost in a series of large rock buttresses on the south side of Darwin Glacier between Alley Glacier and Gaussiran Glacier. See also * Erewhon Basin * List of glaciers in the Antarctic * Glaciology * The Nozzle * Walker Cirque Walker Cirque () is a prominent glacier-filled cirque at the west side of the terminus of McCleary Glacier in Cook Mountains. The cirque opens to Darwin Glacier (Antarctica), Darwin Glacier near the head. Named after Carlton Walker, Facilities, Mai ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu]
	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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu]
	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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu]
	Kennett Ridge Kennett Ridge () is a rocky ridge, long, which descends eastward from the northeast end of Midnight Plateau in the Darwin Mountains of Antarctica. It was mapped 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 ... (1962–63) and named for James P. Kennett, a geologist with the expedition. References Ridges of Oates Land {{OatesLand-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu]
picture info	Nunatak A nunatak (from Inuit ''nunataq'') 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 are also called glacial islands. Examples are natural pyramidal peaks. When rounded by glacial action, smaller rock promontories may be referred to as rognons. The word is of Greenlandic origin and has been used in English since the 1870s. Description The term is typically used in areas where a permanent ice sheet is present and the nunataks protrude 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 nunataks are isolated, sometimes they form dense clusters, such as Queen Louise Land in Greenland. Nunataks are generally angular and jagged, which hampers the formation of glacial ice on their tops, although snow can a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu]
	Richardson Hill 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 between Kenne ... [...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 the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu]
picture info	Landforms Of Oates Land A landform is a natural or anthropogenic land feature on the solid surface of the Earth or other planetary body. Landforms together make up a given terrain, and their arrangement in the landscape is known as topography. Landforms include hills, mountains, canyons, and valleys, as well as shoreline features such as bays, peninsulas, and seas, including submerged features such as mid-ocean ridges, volcanoes, and the great ocean basins. Physical characteristics Landforms are categorized by characteristic physical attributes such as elevation, slope, orientation, stratification, rock exposure and soil type. Gross physical features or landforms include intuitive elements such as berms, mounds, hills, ridges, cliffs, valleys, rivers, peninsulas, volcanoes, and numerous other structural and size-scaled (e.g. ponds vs. lakes, hills vs. mountains) elements including various kinds of inland and oceanic waterbodies and sub-surface features. Mountains, hills, plateaux, and plains are the fou ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu]