The Lister Heights ( 80°31′S28°35′W / 80.517°S 28.583°W Coordinates: 80°31′S28°35′W / 80.517°S 28.583°W ) are rock heights on the east side of Stratton Glacier, 4 nautical miles (7 km) southwest of Flat Top in the western part of the Shackleton Range, Antarctica. They were first mapped in 1957 by the Commonwealth Trans-Antarctic Expedition (CTAE) and named for Hal Lister, a glaciologist with the transpolar party of the CTAE in 1956–58, and leader at the expedition's advance base, South Ice, in 1957. [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.
Stratton Glacier is a glacier 20 nautical miles (37 km) long, flowing north from Pointer Nunatak and then northwest to the north of Mount Weston, in the Shackleton Range. First mapped in 1957 by the Commonwealth Trans-Antarctic Expedition and named for David G. Stratton, surveyor and deputy leader of the transpolar party of the Commonwealth Trans-Antarctic Expedition in 1956-58.
Flat Top is a distinctive table mountain, 1,330 m, with steep rocky cliffs, 4 nautical miles northeast of Lister Heights in the west part of the Shackleton Range in Antarctica. First seen and given this descriptive name during the early reconnaissance flights of the Commonwealth Trans-Antarctic Expedition, 1955-58. Visited and mapped by the Commonwealth Trans-Antarctic Expedition in 1957.
The Shackleton Range is a mountain range in Antarctica. Rising at Holmes Summit to 1,875 metres (6,152 ft), it extends in an east-west direction for about 160 kilometres (99 mi) between the Slessor and Recovery glaciers.
The Slessor Glacier is a glacier at least 120 km long and 80 km wide, flowing west into the Filchner Ice Shelf to the north of the Shackleton Range. First seen from the air and mapped by the Commonwealth Trans-Antarctic Expedition (CTAE) in 1956. Named by the CTAE for RAF Marshal Sir John Slessor, chairman of the expedition committee.
Skelton Glacier is a large glacier flowing from the polar plateau into the Ross Ice Shelf at Skelton Inlet on the Hillary Coast, south of Victoria Land, Antarctica.
Gordon Glacier is an Antarctic glacier of at least 24 nautical miles in length flowing in a northerly direction beginning in the Crossover Pass, flowing through the Shackleton Range to finally meet the Slessor Glacier. The glacier was first mapped in 1957 by the CTAE, and named after George Patrick Pirie-Gordon, 15th Laird of Buthlaw, who was a member of the Committee of Management and treasurer of the CTAE between 1955 and 1958.
Jutulstraumen Glacier is a large glacier in Queen Maud Land, Antarctica, about 120 nautical miles (220 km) long, draining northward to the Fimbul Ice Shelf between the Kirwan Escarpment, Borg Massif and Ahlmann Ridge on the west and the Sverdrup Mountains on the east. It was mapped by Norwegian cartographers from surveys and air photos by the Norwegian–British–Swedish Antarctic Expedition (1949–52) and air photos by the Norwegian expedition (1958–59) and named Jutulstraumen. More specifically jutulen are troll-like figures from Norwegian folk tales. The ice stream reaches speeds of around 4 metres per day near the coast where it is heavily crevassed.
Blaiklock Glacier is a glacier 16 nautical miles (30 km) long, flowing north from Turnpike Bluff, then northwest to Mount Provender and Mount Lowe in the western part of the Shackleton Range. It was first mapped in 1957 by the Commonwealth Trans-Antarctic Expedition (CTAE), and named for Kenneth V. Blaiklock, the leader of the advance party of the CTAE in 1955–56 and a surveyor with the transpolar party in 1956–58.
Otter Highlands is a group of peaks and ridges extending NW-SE for 17 nautical miles (31 km) from Mount Lowe to Wyeth Heights, located west of Blaiklock Glacier and forming the west end of the Shackleton Range. Surveyed by the Commonwealth Trans-Antarctic Expedition in 1957. Named by the United Kingdom Antarctic Place-Names Committee (UK-APC) in 1972 after the De Havilland Otter aircraft which supported the CTAE.
Coalseam Cliffs are rock cliffs forming the northwest part of Mount Faraway in the Theron Mountains. They were first mapped in 1956–57 by the Commonwealth Trans-Antarctic Expedition (CTAE), and so named because a coal seam was found when members of the CTAE made an aircraft landing there in 1957.
The Jutulpløgsla Crevasses form a crevasse field halfway up Jutulstraumen Glacier, about 8 nautical miles (15 km) southeast of Nashornet Mountain, in Queen Maud Land, Antarctica. They were mapped by Norwegian cartographers from surveys and air photos by the Norwegian–British–Swedish Antarctic Expedition (1949–52) and from air photos by the Norwegian expedition (1958–59) and named Jutulpløgsla.
Fuchs Dome is a large ice-covered dome rising over 1,525 metres (5,000 ft), between Stratton Glacier and Gordon Glacier in the central part of the Shackleton Range, Antarctica. It was first mapped in 1957 by the Commonwealth Trans-Antarctic Expedition (CTAE) and named for Sir Vivian E. Fuchs, leader of the CTAE 1955–58.
Mount Greenfield is an ice-free mountain rising to 1,490 metres (4,890 ft) and surmounting the western extremity of Stephenson Bastion in the Shackleton Range of Antarctica. It was mapped in 1957 by the Commonwealth Trans-Antarctic Expedition (CTAE) and named after George C. Greenfield, a literary agent of the CTAE from 1955–58.
Glen Glacier is a glacier at least 7 nautical miles (13 km) long, flowing south in the Shackleton Range of Antarctica to join Recovery Glacier to the west of the Read Mountains. It was first mapped in 1957 by the Commonwealth Trans-Antarctic Expedition (CTAE) and named for Alexander R. Glen, a member of the Committee of Management of the CTAE, 1955–58.
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 Morris Hills are a scattered group of hills 6 nautical miles (11 km) northeast of Petersen Peak, in the La Grange Nunataks of the north-central Shackleton Range, Antarctica. They were first mapped in 1957 by the Commonwealth Trans-Antarctic Expedition (CTAE), and photographed in 1967 by the U.S. Navy. The hills were named by the UK Antarctic Place-Names Committee for Leslie F. Morris, a member of the Royal Society International Geophysical Year Expedition at Brunt Ice Shelf, who in 1957 spent several weeks helping with the final preparations for the CTAE transpolar journey.
Melville Point is a point marking the east side of the entrance to Siniff Bay on the coast of Marie Byrd Land, Antarctica. It was mapped by United States Geological Survey from surveys and U.S. Navy air photos, 1959–65, and was named by the Advisory Committee on Antarctic Names for Captain Frederick C. Melville, master of the barquentine City of New York in voyages to the Bay of Whales during the Byrd Antarctic Expedition, 1928–30.
Mount Haslop is a mountain, 760 metres (2,500 ft) high, which stands 2 nautical miles (4 km) south of Mount Lowe at the western extremity of the Shackleton Range in Antarctica. It was first mapped in 1957 by the Commonwealth Trans-Antarctic Expedition (CTAE) and named for Flight Lieutenant Gordon M. Haslop, Royal New Zealand Air Force (1922–1961), New Zealand second pilot of the Royal Air Force contingent of the CTAE in 1956-58.
Hei Glacier is a glacier flowing northwest between the Hamrane Heights and the Robin Heights in the Sverdrup Mountains of Queen Maud Land, Antarctica. It was photographed from the air by the Third German Antarctic Expedition (1938–39). It was mapped by Norwegian cartographers from surveys and air photos by the Norwegian–British–Swedish Antarctic Expedition (1949–52) and from air photos by the Norwegian expedition (1958–59) and named Heibreen.
Honnywill Peak is a rock peak, 1,220 metres (4,000 ft) high, immediately southeast of Williams Ridge on the west side of Stratton Glacier in the Shackleton Range of Antarctica. It was first mapped in 1957 by the Commonwealth Trans-Antarctic Expedition and was named for Eleanor Honnywill, Assistant Secretary to the expedition in 1955-59, and later Secretary and Editor.
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.
The Lewis Chain is a chain of four rock nunataks on the west side of Gordon Glacier in the Shackleton Range of Antarctica. It was first mapped by the Commonwealth Trans-Antarctic Expedition (CTAE) in 1957, and was photographed by the U.S. Navy in 1967. The chain was named by the UK Antarctic Place-Names Committee for Squadron Leader John H. Lewis, Royal Air Force (RAF), senior pilot of the RAF contingent of the CTAE, 1956–58.
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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