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Lambert Glacier information


An icefall feeding into the Lambert Glacier, Antarctica

71°S 70°E / 71°S 70°E / -71; 70

Lambert Glacier is a major glacier in East Antarctica. At about 80 km (50 mi) wide, over 400 km (250 mi) long, and about 2,500 m (8,200 ft) deep, it is the world's largest glacier. It drains 8% of the Antarctic ice sheet to the east and south of the Prince Charles Mountains and flows northward to the Amery Ice Shelf.[1] It flows in part of Lambert Graben and exits the continent at Prydz Bay.

This glacier was delineated and named in 1952 by American geographer John H. Roscoe who made a detailed study of this area from aerial photographs taken by Operation Highjump, 1946–47. He gave the name "Baker Three Glacier", using the code name of the Navy photographic aircraft and crew that made three flights in this coastal area in March 1947 resulting in geographic discoveries. The glacier was described in Gazetteer No. 14, Geographic Names of Antarctica (U.S. Board on Geographic Names, 1956), but the feature did not immediately appear on published maps. As a result the name Lambert Glacier, as applied by the Antarctic Names Committee of Australia (ANCA) in 1957 following mapping of the area by Australian National Antarctic Research Expeditions (ANARE) in 1956, has become established for this feature. It was named for Bruce P. Lambert, Director of National Mapping in the Australian Department of National Development.[2]

  1. ^ Cite error: The named reference tulloch was invoked but never defined (see the help page).
  2. ^ Cite error: The named reference gnis was invoked but never defined (see the help page).

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Lambert Glacier

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71°S 70°E / 71°S 70°E / -71; 70 Lambert Glacier is a major glacier in East Antarctica. At about 80 km (50 mi) wide, over 400 km (250 mi) long, and about...

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Fisher Glacier

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It is a major tributary of the Lambert Glacier. The glacier is unusual in periodically surging. The Fisher Glacier was sighted from Australian National...

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Icefall

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feeding into the Lambert Glacier, Antarctica. The Khumbu Icefall on Mount Everest A small icefall on east lobe of the new Crater Glacier on Mount St. Helens...

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Dome A

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East Antarctica, approximately midway between the enormous head of Lambert Glacier and the geographic South Pole, within the Australian claim. Dome Argus...

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Laurentide ice sheet

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dissipated north of the Alaska Range where the air was too dry to form glaciers. It is believed that the Cordilleran ice melted rapidly, in less than 4000...

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Lambert Graben

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Lambert Graben is a graben in Antarctica. It intersects the coast at Prydz Bay and contains the largest glacier in the world, Lambert Glacier. The graben...

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Ice age

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sheets and alpine glaciers. Earth's climate alternates between ice ages, and greenhouse periods during which there are no glaciers on the planet. Earth...

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Prydz Bay

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interior. The Lambert Glacier flows from Lambert Graben into the Amery Ice Shelf on the south-west side of Prydz Bay. Other major glaciers drain into the...

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Last Glacial Period

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severe in others. During this last glacial period, alternating episodes of glacier advance, and retreat occurred. Within the last glacial period, the Last...

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Proglacial lake

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either by the damming action of a moraine during the retreat of a melting glacier, a glacial ice dam, or by meltwater trapped against an ice sheet due to...

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Pleistocene

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loess deposits as well as in the large amounts of material moved about by glaciers. Less common are cave deposits, travertines and volcanic deposits (lavas...

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Esker

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streams that flowed within and under glaciers. They tended to form around the time of the glacial maximum, when the glacier was slow and sluggish. After the...

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Canadian Shield

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Hardangerfjord Killary Harbour Monte Rosa Svalbard Antarctica Antarctica Lambert Glacier Ross Ice Shelf Time periods Quaternary glaciation Illinoian Stage Interglacial...

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Hardangerfjord

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third largest glacier is found on the Folgefonna peninsula, along of the Hardangerfjord. With its three parts, the Folgefonna glacier covers an area...

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Interglacial

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Hardangerfjord Killary Harbour Monte Rosa Svalbard Antarctica Antarctica Lambert Glacier Ross Ice Shelf Time periods Quaternary glaciation Illinoian Stage Interglacial...

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Terminal moraine

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end moraine, is a type of moraine that forms at the terminal (edge) of a glacier, marking its maximum advance. At this point, debris that has accumulated...

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Stadial and interstadial

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Hardangerfjord Killary Harbour Monte Rosa Svalbard Antarctica Antarctica Lambert Glacier Ross Ice Shelf Time periods Quaternary glaciation Illinoian Stage Interglacial...

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Glacial erratic

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They can be transported by glaciers, and are thereby one of a series of indicators which mark the path of prehistoric glacier movement. Their lithographic...

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Younger Dryas

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generally accepted to have lasted around 200 years. In northern Scotland, the glaciers were thicker and more extensive than during the Younger Dryas. The Older...

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Lambert River

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The Lambert River is a river of the West Coast Region of New Zealand's South Island. It flows north from the Lambert Glacier in the Southern Alps, joining...

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Little Ice Age

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southwards in the North Atlantic, as did glaciers in Greenland. Anecdotal evidence suggests expanding glaciers almost worldwide. Based on radiocarbon dating...

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Last Glacial Maximum

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evidence for another abrupt rise in the sea level about 14,500 years ago. Glacier fluctuations around the Strait of Magellan suggest the peak in glacial...

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Kame

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in a depression on a retreating glacier, and is then deposited on the land surface with further melting of the glacier. Kames are often associated with...

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Wisconsin glaciation

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glaciation during the last glacial period, including the North American alpine glacier advance, known as the Pinedale glaciation. The Wisconsin glaciation extended...

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Prince Charles Mountains

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standing just east of Mount Rymill at the junction of Fisher Glacier and Lambert Glacier. It was mapped from air photos taken by the RAAF Antarctic Flight...

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Ice stream

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The largest in East Antarctica is Lambert Glacier. In West Antarctica the large Pine Island and Thwaites Glaciers are currently the most out of balance...

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Till plain

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main body of a glacier and melts in place, depositing the sediments it carried. Ground moraines are formed with melts out of the glacier in irregular heaps...

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Lake Agassiz

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estimated to have been 231 metres (758 ft) deep, with greater depths near the glacier. As the ice sheet melted northward, Lake Agassiz found a lower outlet through...

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