Following is a list of glaciers of Kaiser Wilhelm II Land in Antarctica. This list may not reflect recently named glaciers in Kaiser Wilhelm II Land.
Following is a list of glaciers of Kaiser Wilhelm II Land in Antarctica. This list may not reflect recently named glaciers in Kaiser Wilhelm II Land.
66°49′S90°20′E / 66.817°S 90.333°E . Channel glacier, about 9 nautical miles (17 km; 10 mi) wide and 7 nautical miles (13 km; 8.1 mi) long, flowing north from the continental ice to Posadowsky Bay just west of Cape Torson. Mapped from aerial photographs taken by United States Navy (USN) Operation Highjump (OpHjp), 1946-47. Named by the Advisory Committee on Antarctic Names (US-ACAN) for the USS Burton Island, one of the two icebreakers of USN Operation Windmill (OpWml), 1947-48, which assisted in establishing astronomical control stations along Wilhelm II, Queen Mary, Knox and Budd Coasts. [1]
66°36′S91°30′E / 66.600°S 91.500°E . Channel glacier, 5 nautical miles (9.3 km; 5.8 mi) wide and 6 nautical miles (11 km; 6.9 mi) long, flowing north from the continental ice to the coast close east of Krause Point. Delineated from aerial photographs taken by USN OpHjp, 1946-47, and named by US-ACAN for Ens. Teddy E. Jones, USNR, photo interpreter with the Naval Photographic Interpretation Center, who served as recorder and assistant with the USN OpWml parties which established astronomical control stations along Wilhelm II, Knox and Budd Coasts in 1947–48. [2]
66°45′S88°20′E / 66.750°S 88.333°E . Coastal glacier about 15 nautical miles (28 km; 17 mi) long, flowing north to the east end of the West Ice Shelf, 15 nautical miles (28 km; 17 mi) west of Gaussberg. Delineated from aerial photographs taken by USN OpHjp, 1946-47. Named by the ANCA for Emil Philippi, geologist with the Gauss expedition under Erich von Drygalski, 1901-03, who made scientific observations in the vicinity of Gaussberg. [3]
66°50′S89°25′E / 66.833°S 89.417°E Glacier about 9 nautical miles (17 km; 10 mi) long, flowing north to Posadowsky Bay immediately east of Gaussberg. The glacier was observed from the summit of Gaussberg by the Gauss expedition under Drygalski, 1901-03. It was named after Drygalski's Posadowsky Bay by US-ACAN in 1955 following studies of the aerial photographs taken by USN OpHjp, 1946-47. [4]
The Reedy Glacier is a major glacier in Antarctica, over 100 nautical miles long and 6 to 12 nautical miles wide, descending from the polar plateau to the Ross Ice Shelf between the Michigan Plateau and Wisconsin Range in the Transantarctic Mountains. It marks the limits of the Queen Maud Mountains on the west and the Horlick Mountains on the east.
The Byrd Glacier is a major glacier in Antarctica, about 136 km (85 mi) long and 24 km (15 mi) wide. It drains an extensive area of the Antarctic plateau, and flows eastward to discharge into the Ross Ice Shelf.
The Keltie Glacier is a large Antarctic glacier, 30 nautical miles (56 km) long, draining from Pain Névé southwest around the southern extremity of the Commonwealth Range, and then northwest to enter Beardmore Glacier at Ranfurly Point. It was discovered by the British Antarctic Expedition, 1907–09, under Ernest Shackleton, who named it for Sir John Scott Keltie, Secretary of the Royal Geographical Society, 1892–1915.
The Amundsen Glacier is a major Antarctic glacier, about 7 to 11 km wide and 150 km (80 nmi) long. It originates on the Antarctic Plateau where it drains the area to the south and west of Nilsen Plateau, then descends through the Queen Maud Mountains to enter the Ross Ice Shelf just west of the MacDonald Nunataks.
The Hughes Range84°30′S175°30′E is a high massive north–south trending mountain range in Antarctica, surmounted by six prominent summits, of which Mount Kaplan at 4,230 metres (13,880 ft) is the highest. The range is located east of Canyon Glacier in the Queen Maud Mountains and extends 45 nautical miles from the confluence of Brandau Glacier and Keltie Glacier in the south, to the Giovinco Ice Piedmont in the north.
Shackleton Glacier is a major Antarctic glacier, over 60 nautical miles long and from 5 to 10 nautical miles wide, descending from the Antarctic Plateau from the vicinity of Roberts Massif and flowing north through the Queen Maud Mountains to enter the Ross Ice Shelf between Mount Speed and Waldron Spurs. Discovered by the United States Antarctic Service (USAS) (1939–41) and named by the Advisory Committee on Antarctic Names (US-ACAN) for Sir Ernest Shackleton, British Antarctic explorer.
The Priestley Glacier is a major valley glacier, about 60 nautical miles long, originating at the edge of the Polar Plateau of Victoria Land, Antarctica. The glacier drains southeast between the Deep Freeze Range and Eisenhower Range to enter the northern end of the Nansen Ice Sheet. It was first explored by the Northern Party of the British Antarctic Expedition, 1910–13, and named for Raymond Priestley, a geologist with the Northern Party.
Scott Glacier is a glacier, 7 miles (11.3 km) wide and over 20 miles (32 km) long, flowing north-northwest to the Antarctic coast between Denman Glacier and Mill Island. It was discovered by the Western Base Party of the Australasian Antarctic Expedition (1911-1914) under Mawson and named for Capt. Robert F. Scott.
The David Glacier is a glacier over 60 nautical miles long, flowing east from the polar plateau through the Prince Albert Mountains to the coast of Victoria Land, Antarctica. It enters Ross Sea between Cape Philippi and Cape Reynolds to form the floating Drygalski Ice Tongue. It is the most imposing outlet glacier in Victoria Land. It is fed by two main flows which drain an area larger than 200,000 square kilometres, with an estimated ice discharge rate of 7.8 +/- 0.7 km³/year. The David Glacier was discovered by Ernest Shackleton's "Northern Party," in November 1908, under the leadership of Prof. T.W. Edgeworth David, of Sydney University, for whom the feature was named.
The Scott Glacier is a major glacier, 120 nautical miles long, that drains the East Antarctic Ice Sheet through the Queen Maud Mountains to the Ross Ice Shelf. The Scott Glacier is one of a series of major glaciers flowing across the Transantarctic Mountains, with the Amundsen Glacier to the west and the Leverett and Reedy glaciers to the east.
Gilchrist Glacier is a short channel glacier flowing to Budd Coast 9 nautical miles (17 km) northwest of Fox Glacier. Delineated by G.D. Blodgett (1955) from aerial photographs taken by U.S. Navy Operation Highjump (1946–47). Named by Advisory Committee on Antarctic Names (US-ACAN) after Edward Gilchrist, Acting Surgeon on the sloop Wilkes.
Nansen Ice Sheet is a 30 nautical miles long by 10 nautical miles wide ice shelf. It is nourished by the Priestley and Reeves Glaciers and abuts the north side of the Drygalski Ice Tongue, along the coast of Victoria Land, Antarctica. This feature was explored by the South Magnetic Polar Party of the British Antarctic Expedition, 1907-09 and by the Northern Party of the British Antarctic Expedition, 1910-13. Frank Debenham, geologist with the latter expedition, applied the name Nansen Sheet as the feature is adjacent to Mount Nansen, the dominating summit in the area.
Posadowsky Glacier is a glacier about 9 nautical miles long, flowing north to Posadowsky Bay immediately east of Gaussberg. Posadowsky Bay is an open embayment, located just east of the West Ice Shelf and fronting on the Davis Sea in Kaiser Wilhelm II Land. Kaiser Wilhelm II Land is the part of East Antarctica lying between Cape Penck, at 87°43'E, and Cape Filchner, at 91°54'E, and is claimed by Australia as part of the Australian Antarctic Territory. Other notable geographic features in this area include Drygalski Island, located 45 mi NNE of Cape Filchner in the Davis Sea, and Mirny Station, a Russian scientific research station.
Peterson Glacier is a glacier flowing west into Penney Bay opposite Herring Island in the Windmill Islands. Mapped from aerial photographs taken by U.S. Navy (USN) OpHjp, 1946–47, and named for Louie N. Peterson, radio operator and recorder with the U.S. Navy (USN) OpWml parties which established astronomical control stations along Wilhelm II, Knox and Budd Coasts during January–February 1948.
Bennett Platform is a high, nearly flat, snow-free mesa of dark rock of Antarctica, about 5 nautical miles long and 2.5 nautical miles wide, located immediately east of Mount Black, on the west side of Shackleton Glacier.
Whittle Glacier is a short channel glacier flowing northeast to Colvocoresses Bay and terminating in a small glacier tongue 6 nautical miles northwest of Williamson Glacier. Delineated from air photos taken by U.S. Navy Operation Highjump (1946–47), and named by Advisory Committee on Antarctic Names (US-ACAN) for Dr. J.S. Whittle, Assistant Surgeon on the sloop Vincennes of the United States Exploring Expedition (1838–42) under Lieutenant Charles Wilkes.
The Holland Range is a rugged coastal mountain range in the Ross Dependency, Antarctica, on the west coast of the Ross Ice Shelf. It is about 60 nautical miles (110 km) long.
Ramsey Glacier is a glacier about 45 nautical miles long in Antarctica. It originates in the Bush Mountains near the edge of the polar plateau and flows north through the Queen Maud Mountains of Antarctica to the Ross Ice Shelf eastward of Den Hartog Peak.
Roscoe Glacier is an Antarctic channel glacier, 12 nautical miles (22 km) long and 3 to 5 nautical miles (9 km) wide, debouching from a small valley onto the west portion of Shackleton Ice Shelf, midway between Cape Moyes and Junction Corner. Charted as a valley depression during a southern reconnaissance in March 1912 by F. Wild and other members of the Western Base Party of the Australasian Antarctic Expedition under Mawson. Delineated from aerial photographs taken by U.S. Navy Operation Highjump, 1946–47, and named by the Advisory Committee on Antarctic Names (US-ACAN) for John H. Roscoe, geographer, author of Antarctic Bibliography, and scientific advisor to the director of United States Antarctic Program. Roscoe served as photogrammetrist with the central task group of U.S. Navy Operation Highjump, 1946–47, and with U.S. Navy Operation Windmill, 1947–48, and assisted the latter group in establishing astronomical control stations along Wilhelm II, Queen Mary, Knox and Budd Coasts.
This article incorporates public domain material from websites or documents of the United States Board on Geographic Names.