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Thurston Island is a largely ice-covered, glacially dissected island, 135 nautical miles long and 55 nautical miles wide, lying between Amundsen Sea and Bellingshausen Sea a short way off the northwest end of Ellsworth Land, Antarctica. The island is separated from the mainland by Peacock Sound, which is occupied by the west portion of Abbot Ice Shelf.
Hope Bay is a bay 3 nautical miles long and 2 nautical miles wide, indenting the tip of the Antarctic Peninsula and opening on Antarctic Sound.
The Darwin Glacier is a large glacier in Antarctica. It flows from the polar plateau eastward between the Darwin Mountains and the Cook Mountains to the Ross Ice Shelf. The Darwin and its major tributary the Hatherton are often treated as one system, the Darwin–Hatherton.
Mount Bird is a 1,765 metres (5,791 ft) high shield volcano standing about 7 nautical miles south of Cape Bird, the northern extremity of Ross Island. It was mapped by the British National Antarctic Expedition, 1901–04, under Robert Falcon Scott, and apparently named by them after Cape Bird.
Cape Evans is a rocky cape on the west side of Ross Island, Antarctica, forming the north side of the entrance to Erebus Bay.
Meade Nunatak is a nunatak 3 nautical miles (6 km) north of Blanchard Hill, rising to 990 metres (3,250 ft) in the Pioneers Escarpment, Shackleton Range, Antarctica. It was photographed from the air by the U.S. Navy, 1967, and was surveyed by the British Antarctic Survey, 1968–71. In association with the names of pioneers of polar life and travel grouped in this area, it was named by the UK Antarctic Place-Names Committee in 1971 after English mountaineer Charles Francis Meade, the designer of the Meade tent.
The Gabbro Hills are a group of rugged ridges and coastal hills which border the Antarctic Ross Ice Shelf between Barrett Glacier and Gough Glacier and extend south to Ropebrake Pass. They were so named by the Southern Party of the New Zealand Geological Survey Antarctic Expedition (NZGSAE) (1963–64) because of the prevalence of gabbro, a dark, plutonic rock, in the area.
Pryor Glacier is a glacier flowing northeastward, to the north of Mount Shields and Yermak Point, into Rennick Bay. The feature is about 30 nautical miles long and forms a physical separation between Wilson Hills and Usarp Mountains.
Dead End Glacier is a glacier flowing east from the south end of the Salvesen Range of South Georgia into the west side of Salomon Glacier. It was surveyed by the South Georgia Survey in the period 1951–57, and so named by the UK Antarctic Place-Names Committee because there is no route for sledging parties from the head of this glacier to the north shore of Drygalski Fjord.
Andvord Bay is a bay, 9 nautical miles long and 3 nautical miles wide, which lies between Beneden Head and Duthiers Point along the west coast of Graham Land, Antarctica.
Aronson Corner is the cliffed extremity of a snow-capped ridge between Mummery Cliff and Chevreul Cliffs in Pioneers Escarpment, Shackleton Range. It was photographed from the air by the U.S. Navy, 1967, and surveyed by the British Antarctic Survey, 1968–71. In association with the names of pioneers of polar life and travel, it was named by the United Kingdom Antarctic Place-Names Committee after Louis V. Aronson, American founder of the Ronson Corporation, who in about 1910 developed the first practical petrol lighter, known originally as the "trench match."
Whymper Spur is a rock spur rising to about 1,250 m eastward of Blanchard Hill in Pioneers Escarpment, Shackleton Range. Named by the United Kingdom Antarctic Place-Names Committee (UK-APC) in 1971 after English mountaineer and artist Edward Whymper (1840–1911), who made the first ascent of the Matterhorn, Switzerland, July 14, 1865; designer of the prototype of the Whymper tent, 1861–62.
Pioneers Escarpment is a mostly snow-covered north-facing escarpment in Antarctica, interrupted by occasional bluffs and spurs, between Slessor Glacier on the north and Shotton Snowfield on the south, in the Shackleton Range.
Flagstaff Glacier is a very small glacier lying immediately north of Flagstaff Hill on Keller Peninsula, King George Island, in the South Shetland Islands. The name arose locally in about 1958 and derives from association with Flagstaff Hill.
Goldsmith Glacier is a glacier flowing west-northwest through the Theron Mountains of Antarctica, 6 nautical miles (11 km) south of Tailend Nunatak. It was first mapped in 1956–57 by the Commonwealth Trans-Antarctic Expedition (CTAE) and named for Rainer Goldsmith, medical officer with the advance party of the CTAE in 1955–56.
The Goodenough Glacier is a broad sweeping glacier to the south of the Batterbee Mountains, flowing from the west shore of Palmer Land, Antarctica, into George VI Sound and the George VI Ice Shelf.
Lucchitta Glacier is a glacier about 20 nautical miles (37 km) long flowing south from the Hudson Mountains of Antarctica into Pine Island Bay. It was named by the Advisory Committee on Antarctic Names after geologist Baerbel K. Lucchitta of the United States Geological Survey, Flagstaff, Arizona, a specialist in the use of satellite imagery for geological and glaciological studies from the early 1980s to the early 2000s (decade), and one of the pioneers in the use of imagery for glacier velocity measurements in Antarctica.
Mount Skidmore is a mountain on the east side of the mouth of Stratton Glacier in the Shackleton Range. It was first mapped in 1957 by the CTAE, and it was photographed in 1967 by U.S. Navy trimetrogon aerial photography. It was named by the United Kingdom Antarctic Place-Names Committee (UK-APC) for Michael J. Skidmore, a British Antarctic Survey (BAS) geologist at the Brunt Ice Shelf between 1966 and 1969 who worked in the Shackleton Range from 1968 to 1969.
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.
La Grange Nunataks is a scattered group of nunataks extending west for 22 nautical miles (41 km) from the mouth of Gordon Glacier, on the north side of the Shackleton Range, Antarctica. They were first mapped in 1957 by the Commonwealth Trans-Antarctic Expedition (CTAE), and were photographed in 1967 by U.S. Navy aircraft. They were named by the UK Antarctic Place-Names Committee for Johannes J. La Grange, a South African meteorologist with the CTAE. Not: Beney Nunataks.
References
This article incorporates public domain material from "Blanchard Hill". Geographic Names Information System . United States Geological Survey.
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