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Kempe Glacier
Kempe Glacier () is a short alpine glacier in Antarctica, bounded on the north by Dismal Ridge and on the south by the Mount Kempe – Mount Dromedary ridge, whose chief nourishment is névé fields on the north slopes of Mount Kempe. The glacier drains northeast toward Roaring Valley. It was named by the New Zealand 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 ..., 1960–61, for its association with Mount Kempe. References Glaciers of Victoria Land Scott Coast {{ScottCoast-geo-stub ...
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Glacier
A glacier (; ) is a persistent body of dense ice that is constantly moving under its own weight. A glacier forms where the accumulation of snow exceeds its Ablation#Glaciology, ablation over many years, often Century, centuries. It acquires distinguishing features, such as Crevasse, crevasses and Serac, seracs, as it slowly flows and deforms under stresses induced by its weight. As it moves, it abrades rock and debris from its substrate to create landforms such as cirques, moraines, or fjords. Although a glacier may flow into a body of water, it forms only on land and is distinct from the much thinner sea ice and lake ice that form on the surface of bodies of water. On Earth, 99% of glacial ice is contained within vast ice sheets (also known as "continental glaciers") in the polar regions, but glaciers may be found in mountain ranges on every continent other than the Australian mainland, including Oceania's high-latitude oceanic island countries such as New Zealand. Between lati ...
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Dismal Ridge
Mount Dromedary ( is a hump-shaped mountain, over high, standing east of Mount Kempe Mount Kempe () is a peak, high, midway between Mount Huggins and Mount Dromedary in the Royal Society Range of Victoria Land, Antarctica. It was discovered by the British National Antarctic Expedition (1901–04) which named it for Sir Alfred Br ... in the Royal Society Range of Victoria Land, Antarctica. First mapped by the BrNAE, 1901–04, but named by the BrAE, 1910–13. Named for the appearance of the mountain which resembles a dromedary's hump. References Sources * Mountains of Victoria Land Scott Coast {{ScottCoast-geo-stub ...
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Mount Kempe
Mount Kempe () is a peak, high, midway between Mount Huggins and Mount Dromedary in the Royal Society Range of Victoria Land, Antarctica. It was discovered by the British National Antarctic Expedition (1901–04) which named it for Sir Alfred Bray Kempe, at that time Treasurer of the Royal Society. Auster Pass is a high pass between Mount Huggins Mount Huggins () is a large conical mountain, high, surmounting the heads of Allison Glacier, Dale Glacier, and Potter Glacier in the Royal Society Range of Antarctica. It was discovered by the British National Antarctic Expedition (1901–0 ... and Mount Kempe. References Mountains of Victoria Land Scott Coast {{ScottCoast-geo-stub ...
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Mount Dromedary (Antarctica)
Mount Dromedary ( is a hump-shaped mountain, over high, standing east of Mount Kempe Mount Kempe () is a peak, high, midway between Mount Huggins and Mount Dromedary in the Royal Society Range of Victoria Land, Antarctica. It was discovered by the British National Antarctic Expedition (1901–04) which named it for Sir Alfred Br ... in the Royal Society Range of Victoria Land, Antarctica. First mapped by the BrNAE, 1901–04, but named by the BrAE, 1910–13. Named for the appearance of the mountain which resembles a dromedary's hump. References Sources * Mountains of Victoria Land Scott Coast {{ScottCoast-geo-stub ...
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Névé
Névé is a young, granular type of snow which has been partially melted, refrozen and compacted, yet precedes the form of ice. This type of snow is associated with glacier formation through the process of ''nivation''. Névé that survives a full season of ablation turns into firn, which is both older and slightly denser. Firn eventually becomes glacial ice – the long-lived, compacted ice that glaciers are composed of. Glacier formation can take days to years depending on freeze-thaw factors. Névé is annually observed in skiing slopes, and is generally disliked as an icy falling zone. Névé has a minimum density of 500 kg/m3, which is roughly half of the density of liquid water at 1 atm. Névé can also refer to the alpine Alpine may refer to any mountainous region. It may also refer to: Places Europe * Alps, a European mountain range ** Alpine states, which overlap with the European range Australia * Alpine, New South Wales, a Northern Village * Alpine Nati ...
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Roaring Valley
Roaring Valley () is a moraine-filled valley on the north side of Mount Dromedary, formerly occupied by the coalescing glaciers that descend northeast and north from Mount Kempe and Mount Dromedary. The New Zealand Victoria University of Wellington Antarctic Expedition New is an adjective referring to something recently made, discovered, or created. New or NEW may refer to: Music * New, singer of K-pop group The Boyz Albums and EPs * ''New'' (album), by Paul McCartney, 2013 * ''New'' (EP), by Regurgitator ... (VUWAE), 1960-61 named this feature after they experienced strong winds at most campsites in the area—but none as violent and destructive force as the winds that struck their camp at the valley mouth. See also * Lake Porkchop References Valleys of Victoria Land Scott Coast {{ScottCoast-geo-stub ...
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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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Glaciers Of Victoria Land
A glacier (; ) is a persistent body of dense ice that is constantly moving under its own weight. A glacier forms where the accumulation of snow exceeds its ablation over many years, often centuries. It acquires distinguishing features, such as crevasses and seracs, as it slowly flows and deforms under stresses induced by its weight. As it moves, it abrades rock and debris from its substrate to create landforms such as cirques, moraines, or fjords. Although a glacier may flow into a body of water, it forms only on land and is distinct from the much thinner sea ice and lake ice that form on the surface of bodies of water. On Earth, 99% of glacial ice is contained within vast ice sheets (also known as "continental glaciers") in the polar regions, but glaciers may be found in mountain ranges on every continent other than the Australian mainland, including Oceania's high-latitude oceanic island countries such as New Zealand. Between latitudes 35°N and 35°S, glaciers occur only in ...
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