Coker Ice Rise ( 69°4′S67°8′W / 69.067°S 67.133°W Coordinates: 69°4′S67°8′W / 69.067°S 67.133°W ) is a small ice rise in Wordie Ice Shelf, 6 nautical miles (11 km) west-northwest of the Triune Peaks, Fallières Coast. It was photographed from the air by the Ronne Antarctic Research Expedition, 1947–48, and surveyed by the Falkland Islands Dependencies Survey, 1958. It was named by the Advisory Committee on Antarctic Names for Walter B. Coker, U.S. Navy, radioman, Palmer Station winter party, 1969. [1]
A geographic coordinate system is a coordinate system that enables every location on Earth to be specified by a set of numbers, letters or symbols. The coordinates are often chosen such that one of the numbers represents a vertical position and two or three of the numbers represent a horizontal position; alternatively, a geographic position may be expressed in a combined three-dimensional Cartesian vector. A common choice of coordinates is latitude, longitude and elevation. To specify a location on a plane requires a map projection.
An ice rise is a clearly defined elevation of the otherwise totally flat ice shelf, typically dome-shaped and rising 100 to 200 metres above the surrounding ice shelf. An ice rise forms where the ice shelf touches the rocky seabed because of an elevation in the seabed that remains below sea level.. The ice shelf flows over the seabed elevation, completely covering it with ice, thereby forming an ice rise. The resulting tension forms crevasses around the ice rise.
The Wordie Ice Shelf was a confluent glacier projecting as an ice shelf into the SE part of Marguerite Bay between Cape Berteaux and Mount Edgell, along the western coast of Antarctic Peninsula.
The Usarp Mountains is a major Antarctic mountain range, lying westward of the Rennick Glacier and trending N-S for about 190 kilometres (118 mi). The feature is bounded to the north by Pryor Glacier and the Wilson Hills. Its important constituent parts include Welcome Mountain, Mount Van der Hoeven, Mount Weihaupt, Mount Stuart, Mount Lorius, Smith Bench, Mount Roberts, Pomerantz Tableland, Daniels Range, Emlen Peaks, Helliwell Hills and Morozumi Range.
Patuxent Ice Stream is a broad Antarctic ice stream between the Patuxent Range and Pecora Escarpment in the Pensacola Mountains, draining northwestward to the upper part of Foundation Ice Stream. Mapped by U.S. Geological Survey (USGS) from surveys and U.S. Navy (USN) air photos, 1956-66. Named by Advisory Committee on Antarctic Names (US-ACAN) for its proximity to the Patuxent Range.
Alison Ice Stream is an ice stream about 8 nautical miles (15 km) long flowing into Eltanin Bay south of Wirth Peninsula, Antarctica. It was named by the Advisory Committee on Antarctic Names after Alison Cook, a British Antarctic Survey computer specialist, part of the United States-UK cooperative project to compile glaciological and coastal change maps of the Antarctic Peninsula in the late 1990s and early 2000s.
Bandy Island is a small ice-covered island lying in Hull Bay, 3 kilometres (1.5 nmi) west of Lynch Point in coastal Marie Byrd Land. It was mapped by the United States Geological Survey from surveys and from U.S. Navy aerial photographs, 1962–67, and named by the Advisory Committee on Antarctic Names after Orville L. Bandy (1917–73), professor of geology at the University of California, Los Angeles, and a participant since 1961 in several United States Antarctic Research Program projects. In 1964 and 1966, respectively, he was chief scientist on cruises 7 and 17 of RV Anton Bruun, and took part in several cruises of USNS Eltanin.
California Plateau is an undulating ice-covered plateau, 30 nautical miles (56 km) long and from 2 to 12 nautical miles wide, which rises to 3,000 metres (10,000 ft) at the eastern side of Scott Glacier. The plateau reaches a maximum height of 3,275 metres (10,745 ft) in Mount Blackburn at the southern end. The northwestern side of the plateau is marked by the steep rock cliffs of Watson Escarpment; the southeastern side grades gradually to the elevation of the interior ice. It was mapped by the United States Geological Survey from ground surveys and from U.S. Navy aerial photography, 1960–64, and named by the Advisory Committee on Antarctic Names for the several branches of the University of California which have sent numerous researchers to work in Antarctica.
Cape Calmette is a cape marking the western extremity of a rocky peninsula which rises more than 625 metres (2,050 ft) and projects from the west coast of Graham Land for 3 nautical miles (6 km) to form the southern shore of Calmette Bay. It was discovered in 1909 by the French Antarctic Expedition under Jean-Baptiste Charcot, who from a distance mistook this cape for an island; the British Graham Land Expedition under John Rymill, 1934–37, determined the true nature of the feature. It was named by Charcot for Gaston Calmette, editor of Le Figaro, who furnished the French Antarctic Expedition with copies of this newspaper for the two years preceding the expedition.
Neumann Peak is a peak on the north end of Hansen Island, in Hanusse Bay in Graham Land. Mapped from air photos taken by Ronne Antarctic Research Expedition (RARE), 1947–48, and Falkland Islands and Dependencies Aerial Survey Expedition (FIDASE), 1956-57. Named by United Kingdom Antarctic Place-Names Committee (UK-APC) for Franz Ernst Neumann (1798–1895), German physicist who made an important contribution to understanding of the thermal conductivity of ice.
Wade Ice Rise is a small ice rise in Wordie Ice Shelf, 8 nautical miles (15 km) northwest of Triune Peaks, Fallières Coast. Photographed from the air by Ronne Antarctic Research Expedition (RARE), 1947–48, and surveyed by Falkland Islands Dependencies Survey (FIDS), 1958. Named in 1977 by Advisory Committee on Antarctic Names (US-ACAN) after George W. Wade, Jr., U.S. Navy, Chief Construction Electrician, Palmer Station, winter party 1970.
Mount Jenkins is a mountain, 1,705 metres (5,600 ft) high, standing 7 nautical miles (13 km) northeast of Mount Edward in the Sweeney Mountains of Palmer Land, Antarctica. It was discovered and photographed by the Ronne Antarctic Research Expedition, 1947–48, was mapped by the United States Geological Survey from surveys and U.S. Navy air photos, 1961–67, and was named by the Advisory Committee on Antarctic Names for W.H. Jenkins, a hospital corpsman at South Pole Station, winter party 1963.
Mount Ethelred is a mainly ice-covered mountain, 2,470 metres (8,100 ft) high, 3 nautical miles (6 km) southeast of Mount Ethelwulf and 8 nautical miles (15 km) inland from George VI Sound, in the Douglas Range of Alexander Island, Antarctica. The mountain was probably first observed by Lincoln Ellsworth, who photographed the east side of the Douglas Range from the air on November 23, 1935; its east face was roughly surveyed in 1936 by the British Graham Land Expedition. It was resurveyed in 1948 by the Falkland Islands Dependencies Survey (FIDS) and named for Ethelred I, Saxon King of England, 865–871. The west face of the mountain was mapped from air photos taken by the Ronne Antarctic Research Expedition, 1947–48, by D. Searle of the FIDS in 1960. Mount Ethelred is the seventh highest peak of Alexander Island, proceeded by Mount Calais.
Lofgren Peninsula is an ice-covered peninsula about 22 nautical miles (40 km) long, projecting between Cadwalader Inlet and Morgan Inlet on the northeast side of Thurston Island, Antarctica. The northern extremity of the peninsula is Cape Menzel, a bold rock cape. These features were discovered in helicopter flights from the USS Burton Island and the USS Glacier of the U.S. Navy Bellingshausen Sea Expedition in February 1960, and was named by the Advisory Committee on Antarctic Names. The peninsula was named for Charles E. Lofgren, personnel officer with the Byrd Antarctic Expedition, 1928–30. The cape was named for Reinhard W. Menzel, a geomagnetist-seismologist with the Eights Station winter party, 1965.
Miller Ice Rise is an ice rise nearly 2 nautical miles (4 km) long and 1 nautical mile (2 km) wide at the ice front (1974) of the Wordie Ice Shelf, 16 nautical miles (30 km) west-northwest of the Triune Peaks, in southern Marguerite Bay, Antarctica. It was surveyed by the Falkland Islands Dependencies Survey in 1948–49, and was photographed from the air by the U.S. Navy in 1966. The feature was named, in 1977, by the Advisory Committee on Antarctic Names for Richard Miller, a U.S. Navy chief radioman at Palmer Station in the winter party of 1968.
Mount Henderson is a massive mountain, 970 metres (3,180 ft) high, rising through the ice sheet 5 nautical miles (9 km) southeast of Holme Bay and a like distance northeast of the north end of the Masson Range, Antarctica. It was First sighted from the crow's nest of the Discovery on 3 January 1930, during British Australian New Zealand Antarctic Research Expedition (1929-31) and again seen from the airplane on 5 January 1930. The position was first plotted and the mountain named by BANZARE on 14 February 1931 by the leader of the British Australian New Zealand Antarctic Research Expedition - Mawson, who named it after in 1929 W. Henderson, Director of the Australian Department of External Affairs, and a member of the Australian Antarctic Committee.
McClary Glacier is a glacier 10 nautical miles (19 km) long and 2 nautical miles (4 km) wide on the west coast of Graham Land, Antarctica. It flows southwest along the north side of Butson Ridge into Marguerite Bay between Cape Calmette and the Debenham Islands. The glacier was first roughly surveyed by the British Graham Land Expedition, 1936–37, and resurveyed by the Falkland Islands Dependencies Survey, 1946–50. It was named by the UK Antarctic Place-Names Committee for George B. McClary, father of Nelson McClary, mate on the Port of Beaumont during the Ronne Antarctic Research Expedition, 1947–48.
Sölch Glacier is a glacier on the Pernik Peninsula of the Loubet Coast in Graham Land, flowing west to Salmon Cove just north of Kanchov Peak on the east side of Lallemand Fjord. It was mapped from air photos taken by the Falkland Islands and Dependencies Aerial Survey Expedition, 1956–57, and named by United Kingdom Antarctic Place-Names Committee for Johann Sölch (1883–1951), an Austrian glacial geologist and glaciologist.
Relay Hills is a group of low, ice-covered hills, mainly conical in shape, between Mount Edgell and Kinnear Mountains in western Antarctic Peninsula. First roughly surveyed from the ground by British Graham Land Expedition (BGLE), 1936-37. Photographed from the air by Ronne Antarctic Research Expedition (RARE), November 1947. Resurveyed by Falkland Islands Dependencies Survey (FIDS), November 1958. The name, applied by the United Kingdom Antarctic Place-Names Committee (UK-APC), arose because both the BGLE and the FIDS sledging parties had to relay their loads through this area to the head of Prospect Glacier.
Landauer Point is a point on the east coast of Adelaide Island, marking the west side of the north entrance to Tickle Channel in Graham Land, Antarctica. It was mapped by the Falkland Islands Dependencies Survey from air photos taken by the Ronne Antarctic Research Expedition, 1947–48, and the Falkland Islands and Dependencies Aerial Survey Expedition, 1956–57. The point was named by the UK Antarctic Place-Names Committee for Joseph K. Landauer, an American physicist who has studied the mechanical properties of ice and glacier flow.
League Rock is a distinctive rounded rock lying southwest of Box Reef, off the south end of Adelaide Island, Antarctica. It was surveyed by the Royal Navy Hydrographic Survey Unit, 1962–63, and was so named by the UK Antarctic Place-Names Committee because the rock lies one league distant from what was then Adelaide Station.
Linchpin Ice Rise is a small ice rise northeast of Miller Ice Rise, situated near the ice front of Wordie Ice Shelf on the Fallières Coast of Antarctica. The feature was mapped from U.S. Landsat imagery, 1974–79, and was so named by the UK Antarctic Place-Names Committee because the ice rise plays a key role (linchpin) in maintaining the position of the ice front, as observed in 1979.
Beacon Hill is an ice-covered, dome-shaped hill of elevation 1,810 m which rises 120 m above the surrounding plateau ice surface. It is situated in the south part of Hemimont Plateau in Graham Land, Antarctica 2.5 mi northeast of McLeod Hill. The hill surmounts the divide between Northeast Glacier and Bills Gulch. It was surveyed and named by the U.S. Antarctic Service (USAS), 1939-41; the hill may have been the site of a beacon at that time. The U.S. Antarctic Service (USAS) operated a plateau weather station close southwestward of the hill throughout November and December 1940.
The United States Geological Survey is a scientific agency of the United States government. The scientists of the USGS study the landscape of the United States, its natural resources, and the natural hazards that threaten it. The organization has four major science disciplines, concerning biology, geography, geology, and hydrology. The USGS is a fact-finding research organization with no regulatory responsibility.
The Geographic Names Information System (GNIS) is a database that contains name and locative information about more than two million physical and cultural features located throughout the United States of America and its territories. It is a type of gazetteer. GNIS was developed by the United States Geological Survey in cooperation with the United States Board on Geographic Names (BGN) to promote the standardization of feature names.
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