Hamilton Glacier | |
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Location of King Edward VII Land (marked in orange) within the Ross Dependency | |
Location of Hamilton Glacier in Antarctica | |
Location | King Edward VII Land |
Coordinates | 77°33′S157°25′W / 77.550°S 157.417°W |
Length | 5 nmi (9 km; 6 mi) |
Thickness | unknown |
Terminus | Cape Colbeck |
Status | unknown |
Hamilton Glacier is a glacier about 5 nautical miles (9 km) long draining northwest from Edward VII Peninsula south of Cape Colbeck, Antarctica. It was named by the Advisory Committee on Antarctic Names after Gordon S. Hamilton of the faculty, University of Maine, who was a theoretical and field researcher of ice motion in the West Antarctic ice stream area from the 1980s. [1]
Alexandra Mountains is a group of low, separated mountains in the north portion of Edward VII Peninsula, just southwest of Sulzberger Bay in Marie Byrd Land, Antarctica. Discovered in January–February 1902 by the British National Antarctic Expedition during an exploratory cruise of the Discovery along the Ross Ice Shelf. Named for Alexandra, then Queen of the United Kingdom.
Hammond Glacier is located on the northeast side of the Haines Mountains, flowing northwest for about 40 nautical miles (70 km) to Sulzberger Ice Shelf in the Ford Ranges of Marie Byrd Land, Antarctica. It was discovered in 1934 by the Byrd Antarctic Expedition, and named by Richard E. Byrd for John Hays Hammond, an American mining engineer and philanthropist.
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.
Shell Glacier is a western lobe of the Mount Bird icecap. It descends steeply in the valley north of Trachyte Hill and Harrison Bluff in the center of the ice-free area on the lower western slopes of Mount Bird, Ross Island. Mapped and so named by the New Zealand Geological Survey Antarctic Expedition (NZGSAE), 1958–59, because of the marine shell content of the moraines.
Flask Glacier, is a gently-sloping glacier, 25 nautical miles long, flowing east from Bruce Plateau to enter Scar Inlet between Daggoo Peak and Spouter Peak in Graham Land, Antarctica. The lower reaches of this glacier were surveyed and photographed by the Falklands Islands Dependencies Survey (FIDS) in 1947. The entire glacier was photographed by the Falkland Islands and Dependencies Aerial Survey Expedition in 1955–56, and mapped by the FIDS in 1957. It was named by the UK Antarctic Place-names Committee after the third mate on the Pequod in Herman Melville's Moby-Dick; or, The White Whale.
Withrow Glacier is a glacier on Edward VII Peninsula, flowing northwest into Bartlett Inlet just east of Cape Colbeck. Mapped from surveys by the United States Geological Survey (USGS) and U.S. Navy air photos (1959–65). Named by Advisory Committee on Antarctic Names (US-ACAN) for Commander W.H. Withrow, U.S. Navy, of the staff of the Commander, Naval Support Force, Antarctica, who was officer in charge of Detachment One at Christchurch, New Zealand, 1965-66.
Arthur Glacier is a valley glacier in Antarctica. It is about 25 nautical miles (50 km) long, and flows west to Sulzberger Ice Shelf between the Swanson Mountains on the north and Mount Rea and Mount Cooper on the south, in the Ford Ranges of Marie Byrd Land. It was discovered by members of West Base of the United States Antarctic Service, in aerial flights and from ground surveys in November–December 1940. It was named by the Advisory Committee on Antarctic Names for Rear Admiral Arthur C. Davis, a leader in aviation in the U.S. Navy.
Boyd Glacier is a heavily crevassed glacier flowing west-northwest for about 45 nautical miles (80 km) to the Sulzberger Ice Shelf between Bailey Ridge and Mount Douglass in the Ford Ranges of Marie Byrd Land. It was discovered on aerial flights of the Byrd Antarctic Expedition in 1934, and named for Vernon D. Boyd, an expedition machinist, and a member of West Base of the United States Antarctic Service (1939–41).
Carlson Glacier is a glacier, 9 nautical miles (17 km) long, flowing northward from between Mount Edgell and the Relay Hills into Wordie Ice Shelf, Fallières Coast. It was photographed from the air by the U.S. Navy in 1966, and surveyed by the British Antarctic Survey between 1970 and 1973. It was named by the Advisory Committee on Antarctic Names after Captain Burford A. Carlson, U.S. Navy, Staff Meteorologist, Naval Support Force, Antarctica, Operation Deep Freeze, 1970 and 1971.
Croom Glacier is a steep, broad glacier flowing to the head of Smith Inlet between Moe Point and Hughes Ice Piedmont, on the east coast of Palmer Land. It was mapped by the United States Geological Survey in 1974, and named by the Advisory Committee on Antarctic Names for John M. Croom, who was a United States Antarctic Research Program biologist at Palmer Station in 1968–69 and a U.S. Exchange Scientist at the Soviet Bellingshausen Station in 1970.
Dalton Glacier is a broad glacier on the east side of the Alexandra Mountains on Edward VII Peninsula, flowing northward into Butler Glacier just south of Sulzberger Bay. It was mapped from surveys by the United States Geological Survey and from U.S. Navy air photos (1959–65), and named by the Advisory Committee on Antarctic Names for Lieutenant Brian C. Dalton, MC, U.S. Navy, officer in charge at Byrd Station, 1957. Blades Glacier merges with Dalton Glacier on the north side of Edward VII Peninsula.
Krebs Ridge is an east–west ridge which forms the north wall of Gurling Glacier and terminates at the southwest head of Smith Inlet, on the east coast of Palmer Land, Antarctica. It was mapped by the United States Geological Survey in 1974, and was named by the Advisory Committee on Antarctic Names for William N. Krebs, a United States Antarctic Research Program biologist at Palmer Station in 1972.
Stewart Glacier is a glacier on the north side of Edward VII Peninsula, flowing northeast along the east side of Howard Heights into Sulzberger Ice Shelf mapped by United States Geological Survey (USGS) from surveys and U.S. Navy air photos, 1959-65. Named by Advisory Committee on Antarctic Names (US-ACAN) for Lieutenant Commander Wayne B. Stewart, U.S. Navy, co-pilot in LC-130F Hercules aircraft during Operation Deep Freeze 1968.
Depot Glacier is a well-defined valley glacier, flanked by lateral moraines, which terminates in a high vertical ice cliff at the head of Hope Bay, in the northeast end of the Antarctic Peninsula. It was discovered by the Swedish Antarctic Expedition, 1901–04, under Otto Nordenskiöld, and so named by him because, as seen from Antarctic Sound, it appeared to be a possible site for a depot.
Peckham Glacier is a steep tributary glacier in the Britannia Range, flowing south from Mount McClintock into Byrd Glacier. Named by Advisory Committee on Antarctic Names (US-ACAN) for Verne E. Peckham, biologist, McMurdo Station winter party 1962, who with use of SCUBA gear made numerous dives under the sea ice of McMurdo Sound at Winter Quarters Bay and off Cape Evans.
Eliason Glacier is a glacier 5 nautical miles (9 km) long close west of Mount Hornsby, flowing south from Detroit Plateau into the ice piedmont north of Larsen Inlet, Nordenskjöld Coast in northern Graham Land, Antarctica. It was mapped from surveys by the Falkland Islands Dependencies Survey (1960–61), and was named by the UK Antarctic Place-Names Committee after the Eliason motor sledge, invented in 1942 in Sweden, now made in Canada, and used in Arctic Canada since 1950 and in the Antarctic since 1960.
Fleming Glacier is a broad glacier 25 nautical miles (46 km) long on the west side of the Antarctic Peninsula, flowing west-northwest and terminating in Forster Ice Piedmont to the east of the Wordie Ice Shelf. The glacier was charted by the British Graham Land Expedition (BGLE) under John Rymill, 1934–37, and was photographed from the air by the United States Antarctic Service on September 29, 1940. This hitherto unnamed feature was named by the Advisory Committee on Antarctic Names in 1947 for Reverend W.L.S. Fleming, Dean of Trinity Hall, Cambridge University; also, chaplain, chief scientist, and geologist of the BGLE.
Hale Glacier is a glacier about 6 nautical miles (11 km) long, located just east of Mount Simpson on Thurston Island, Antarctica, and flowing southwest to the Abbot Ice Shelf in Peacock Sound. It was delineated from air photos taken by U.S. Navy Squadron VX-6 in January 1960, and was named by the Advisory Committee on Antarctic Names (US-ACAN) for Lieutenant Bill J. Hale, U.S. Navy, a helicopter pilot aboard USS Burton Island who made exploratory flights to Thurston Island in February 1960.
Scambos Glacier is a glacier about 35 nautical miles (60 km) long draining to the Sulzberger Ice Shelf. Named by Advisory Committee on Antarctic Names (US-ACAN) after Theodore A. Scambos, National Snow and Ice Data Center, Boulder, Colorado, expert in the use of remotely sensed data for field and theoretical studies of Antarctic ice behavior from the 1980s to the present.
Horton Glacier is a glacier at the east side of Mount Barre and Mount Gaudry, flowing southeast from Adelaide Island into Ryder Bay, Antarctica. It was named by the UK Antarctic Place-Names Committee in 1977 for Colin P. Horton, a British Antarctic Survey builder at the nearby Rothera Station, 1976–77.
Coordinates: 77°33′S157°25′W / 77.550°S 157.417°W
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