Wilma Glacier
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Wilma Glacier
Wilma Glacier is the western of two glaciers entering the southern part of Edward VIII Ice Shelf in Kemp Land, East Antarctica. The second, eastern glacier is Robert Glacier. Discovery and naming Wilma Glacier and Robert Glacier were both seen by an ANARE (Australian National Antarctic Research Expeditions) party led by Robert E. Dovers in November 1954. Dovers, accompanied by G. Schwartz, was carrying out a sledge journey and survey of Edward VIII Bay at the time. Wilma Glacier was named by Robert George Dovers for Dovers' wife. Dovers was officer in charge and surveyor at Mawson Station in 1954.Gazetteer of the Australian Antarctic Data CentreWilma Glacier Accessed 23 May 2010. See also * Glaciology * Kemp Land * List of glaciers in the Antarctic There are many glaciers in the Antarctic. This set of lists does not include ice sheets, ice caps or ice fields, such as the Antarctic ice sheet, but includes glacial features that are defined by their flow, rather than general bo ...
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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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Kemp Land
Kemp Land is a thin sliver of Antarctica including, and lying inland from, the Kemp Coast. Part of the Australian Antarctic Territory, Australian Antarctic claim it is defined as lying between 56° 25' E and 59° 34' E, and, as with other sectors of the Antarctic, is deemed being limited by the 60° S parallel. It is bounded in the east by Mac. Robertson Land and in the west by Enderby Land. Kemp Land includes one major group of islands, the Øygarden Group.Kemp Land
on Scientific Committee on Antarctic Research, SCAR website
It reaches a height of 3,346 feet above sea level.


Exploration

Named after Peter Kemp (sealer), Peter Kemp, who, in t ...
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Edward VIII Ice Shelf
Edward VIII Ice Shelf is an ice shelf occupying the head of Edward VIII Bay in Antarctica. The northern part of this feature was called Innviksletta (the inner bay plain) by Norwegian cartographers, who mapped it from aerial photos taken by the Lars Christensen Expedition Lars is a common male name in Scandinavian countries. Origin ''Lars'' means "from the city of Laurentum". Lars is derived from the Latin name Laurentius, which means "from Laurentum" or "crowned with laurel". A homonymous Etruscan name was bo ... in 1936–37. The area was first visited in 1954 by an ANARE ( Australian National Antarctic Research Expeditions) sledge party. The entire ice shelf was then mapped and named in association with Edward VIII Bay. See also * List of glaciers and ice shelves in Antarctica References {{coord, 66, 50, S, 56, 33, E, display=title, type:landmark_scale:2000000 Ice shelves of Antarctica ...
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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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Edward VIII Bay
Edward VIII Bay is a bay about in extent, located between Edward VIII Plateau (a dome-shaped, ice-covered peninsula near Magnet Bay) and the Øygarden Group of islands in Antarctica. The head of the bay is occupied by the Edward VIII Ice Shelf. The bay was discovered in 1936 by Discovery Investigations personnel on the RRS ''William Scoresby'', and named for Edward VIII, then King of the United Kingdom. Kvarsnes Foreland is a prominent, rocky foreland projecting into the south side of Edward VIII Bay close west of the Øygarden Group. Kvarsnes Bay is a small bay at the southwest side of Kvarsnes Foreland, and is named in association with it. Rund Bay ("Round Bay") is a small bay indenting the south shore of Edward VIII Bay immediately east of Kvarsnes Foreland. These features were mapped and named by Norwegian cartographers from aerial photographs taken by the Lars Christensen Expedition Lars is a common male name in Scandinavian countries. Origin ''Lars'' means "from th ...
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East Antarctica
East Antarctica, also called Greater Antarctica, constitutes the majority (two-thirds) of the Antarctic continent, lying on the Indian Ocean side of the continent, separated from West Antarctica by the Transantarctic Mountains. It lies almost entirely within the Eastern Hemisphere and its name has been accepted for more than a century. It is generally higher than West Antarctica and includes the Gamburtsev Mountain Range in the center. The geographic South Pole is located within East Antarctica. Apart from small areas of the coast, East Antarctica is permanently covered by ice and it has relatively low biodiversity, with only a small number of species of terrestrial plants, animals, algae, and lichens. The coasts are the breeding ground for various seabirds and penguins, and the leopard seal, Weddell seal, elephant seal, crabeater seal and Ross seal breed on the surrounding pack ice in summer. Location and description Almost completely covered in thick, permanent ice, East A ...
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Robert Glacier
Robert Glacier is the eastern of two glaciers in Kemp Land entering the southern part of Edward VIII Bay . It was seen by Robert Dovers and G. Schwartz in 1954 while carrying out a sledge journey and survey of Edward VIII Bay . The other (western) glacier is Wilma Glacier. It was named by ANCA for Dovers, who was surveyor and officer in charge at Mawson Station in 1954. It is part of the Australian Antarctic Gazetteer and the SCAR Composite Gazetteer of Antarctica. See also * List of glaciers in the Antarctic *Wilma Glacier * Kemp Land * Glaciology Glaciology (; ) is the scientific study of glaciers, or more generally ice and natural phenomena that involve ice. Glaciology is an interdisciplinary Earth science that integrates geophysics, geology, physical geography, geomorphology, climato ... References * External links data.aad.gov.au Glaciers of Enderby Land {{Antarctica-glacier-stub ...
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Australian National Antarctic Research Expeditions
The Australian National Antarctic Research Expeditions (ANARE ) is the historical name for the Australian Antarctic Program (AAp) administered for Australia by the Australian Antarctic Division (AAD). History Australia has had a long involvement in south polar regions since as early as Douglas Mawson's Australasian Antarctic Expedition in 1911. Further Australian exploration of the Antarctic continent was conducted during the British Australian and New Zealand Antarctic Research Expedition (BANZARE), which was conducted over the years 1929–1931. The Australian National Antarctic Research Expeditions were established in 1947 with expeditions to Macquarie Island and Heard Island. In 1948 the Australian Antarctic Division (AAD) was established to administer the expedition program. ANARE Name The name ANARE fell out of official use in the early 2000s. However current and former Australian Antarctic expeditioners continue to use the term informally as a means of identifica ...
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Mawson Station
The Mawson Station, commonly called Mawson, is one of three permanent bases and research outposts in Antarctica managed by the Australian Antarctic Division (AAD). Mawson lies in Holme Bay in Mac. Robertson Land, East Antarctica in the Australian Antarctic Territory, a territory claimed by Australia. Established in 1954, Mawson is Australia's oldest Antarctic station and the oldest continuously inhabited Antarctic station south of the Antarctic Circle. Mawson was named in honour of the Australian Antarctic explorer Sir Douglas Mawson. Mawson was listed on the Register of the National Estate in 2001 and listed on the Commonwealth Heritage List on 22 June 2004, reflecting the post-World War Two revival of Australia's scientific research and territorial interests in Antarctica. Purpose Mawson Station is a base for scientific research programs including an underground cosmic ray detector, various long-term meteorological aeronomy and geomagnetic studies, as well as ongoing cons ...
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Glaciology
Glaciology (; ) is the scientific study of glaciers, or more generally ice and natural phenomena that involve ice. Glaciology is an interdisciplinary Earth science that integrates geophysics, geology, physical geography, geomorphology, climatology, meteorology, hydrology, biology, and ecology. The impact of glaciers on people includes the fields of human geography and anthropology. The discoveries of water ice on the Moon, Mars, Europa and Pluto add an extraterrestrial component to the field, which is referred to as "astroglaciology". Overview A glacier is an extended mass of ice formed from snow falling and accumulating over a long period of time; glaciers move very slowly, either descending from high mountains, as in valley glaciers, or moving outward from centers of accumulation, as in continental glaciers. Areas of study within glaciology include glacial history and the reconstruction of past glaciation. A glaciologist is a person who studies glaciers. A glacial geologist ...
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List Of Glaciers In The Antarctic
There are many glaciers in the Antarctic. This set of lists does not include ice sheets, ice caps or ice fields, such as the Antarctic ice sheet, but includes glacial features that are defined by their flow, rather than general bodies of ice. The lists include outlet glaciers, valley glaciers, cirque glaciers, tidewater glaciers and ice streams. Ice streams are a type of glacier and many of them have "glacier" in their name, e.g. Pine Island Glacier. Ice shelves are listed separately in the List of Antarctic ice shelves. For the purposes of these lists, the Antarctic is defined as any latitude further south than 60° (the continental limit according to the Antarctic Treaty System). List by letters * List of glaciers in the Antarctic: A–H * List of glaciers in the Antarctic: I–Z See also * List of Antarctic and subantarctic islands * List of Antarctic ice rises * List of Antarctic ice shelves * List of Antarctic ice streams * List of glaciers * List of subantar ...
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