Creswick Gap

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Creswick Gap ( 70°23′S67°44′W / 70.383°S 67.733°W / -70.383; -67.733 Coordinates: 70°23′S67°44′W / 70.383°S 67.733°W / -70.383; -67.733 ), in Antarctica, is a gap between the Creswick Peaks and the Campbell Ridges on the west side of Palmer Land. The gap extends from Chapman Glacier to Meiklejohn Glacier and provides a safe sledging route from George VI Sound via Naess Glacier and Meiklejohn Glacier to the Dyer Plateau of Palmer Land. It was named by the UK Antarctic Place-Names Committee in association with the Creswick Peaks at the south end of the gap.

Geographic coordinate system Coordinate system

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.

Creswick Peaks

The Creswick Peaks, in Antarctica, form an impressive mountain massif with several peaks, the highest at 1,465 metres (4,800 ft), standing at the northeast side of Moore Point between Naess Glacier and Meiklejohn Glacier, and 3 nautical miles (6 km) inland from George VI Sound on the west coast of Palmer Land.

Campbell Ridges

The Campbell Ridges are an irregular complex of ridges between Creswick Gap and Mount Courtauld in Palmer Land. Two north-south ridges are linked by an east-west ridge, on which stand the highest peaks. They were named by the Advisory Committee on Antarctic Names for Lieutenant Commander Bruce H. Campbell, U.S. Navy, Commander of LC-130 aircraft in support of United States Antarctic Research Program field parties on the Lassiter Coast and elsewhere, 1969–70 and 1970–71.

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Sheldon Glacier glacier in Antarctica

Sheldon Glacier is a glacier flowing southeast from Mount Mangin into Ryder Bay, Adelaide Island, Antarctica. Named by the United Kingdom Antarctic Place-Names Committee (UK-APC) in 1977 for Ernest B. Sheldon, British Antarctic Survey (BAS) meteorological observer, Adelaide Station, 1968–69, and Stonington Island, 1969–70; Base Commander, Adelaide Station, 1975–76, and Rothera Station, 1976-77.

Haefeli Glacier glacier in Antarctica

Haefeli Glacier is a glacier, 2 miles (3 km) wide and 6 miles (10 km) long, situated on Pernik Peninsula, Loubet Coast in Graham Land, Antarctica, at the northwest side of Finsterwalder Glacier and flowing south-southwest toward the head of Lallemand Fjord. With Finsterwalder and Klebelsberg Glaciers, its mouth merges with Sharp Glacier where the latter enters the fjord. It was first surveyed in 1946–47 by the Falkland Islands Dependencies Survey and named by them for Robert Haefeli, a Swiss glaciologist.

Willey Glacier is a heavily crevassed glacier north of Creswick Peaks in Palmer Land, flowing west from Creswick Gap into George VI Sound. Named by United Kingdom Antarctic Place-Names Committee (UK-APC) for Lawrence E. Willey, British Antarctic Survey (BAS) geologist at Fossil Bluff and Stonington Island stations, 1966–69 and 1973, and awarded the Polar Medal for services to Antarctic Survey in 1976.

Ashton Glacier is a glacier 9 nautical miles (17 km) long, which flows east-southeast from Mount Thompson to the northwest side of Lehrke Inlet, on the east coast of Palmer Land. The glacier was photographed from the air in December 1940 by the United States Antarctic Service (USAS), and was probably seen by the USAS ground survey party which explored this coast. A joint party consisting of members of the Ronne Antarctic Research Expedition and the Falkland Islands Dependencies Survey (FIDS) charted the glacier in 1947. It was named by the FIDS for L. Ashton, a carpenter with the FIDS at the Port Lockroy and Hope Bay bases in 1944–45 and 1945–46, respectively.

Clifford Glacier is a broad glacier, about 40 nautical miles (70 km) long, flowing in an east-northeast direction to the gap between Mount Tenniel and the Eland Mountains, and then east to Smith Inlet on the east coast of Palmer Land. The upper part of this glacier was charted in 1936 by the British Graham Land Expedition under John Rymill; the seaward side by the United States Antarctic Service survey party which explored along this coast in 1940. During 1947 it was photographed from the air by the Ronne Antarctic Research Expedition under Finn Ronne, who in conjunction with the Falkland Islands Dependencies Survey (FIDS) charted it from the ground. It was named in 1952 by the FIDS for Sir G. Miles Clifford, at that time Governor of the Falkland Islands.

Orion Massif

Orion Massif is a prominent massif located in Palmer Land, Antarctica. It is 14 nautical miles long and consists of a complicated network of peaks, passes, ridges, and cirques. It is located 4 nautical miles east-northeast of Scorpio Peaks, between the upper parts of Meiklejohn and Millett Glaciers, and 5 nautical miles south of Goettel Escarpment.

Kukri Hills

Kukri Hills is a prominent east-west trending range, about 25 nautical miles (46 km) long and over 2,000 metres (6,600 ft) high, forming the divide between Ferrar Glacier on the south and Taylor Glacier and Taylor Valley on the north, in Victoria Land, Antarctica.

Planet Heights is a series of summits running along an ice-free ridge, extending 24 nautical miles (44 km) in a north-south direction between the southernmost extremity of the LeMay Range and George VI Sound in the east part of Alexander Island, Antarctica. Many landforms and nearby features are named in association with this mountain range, some of these include landforms named after astronomers, satellites, planets and other things related to astrology and astrophysics. The mountain range was first mapped from air photos taken by the Ronne Antarctic Research Expedition (RARE), 1947–48, by Searle of the Falkland Islands Dependencies Survey (FIDS) in 1960. Named by the United Kingdom Antarctic Place-Names Committee (UK-APC) from association with the nearby glaciers named for planets of the solar system. The only planet that is not featured in any of these glaciers is the planet Earth, as there are no glaciers named "Earth Glacier" and this glacier does not exist.

Mount Eissinger

Mount Eissinger is a large ridge-like mountain at the north side of Riley Glacier on the west side of Palmer Land. The feature has a snow-topped upper surface, bare rock cliffs along the north side, and an impressive rectangular rock buttress rising in an unbroken, near-vertical sweep from the glacier to 500 metres (1,600 ft) at the west end. It was mapped by the United States Geological Survey (USGS) in 1974, and was named by the Advisory Committee on Antarctic Names for Karlheinz Eissinger, a USGS topographic engineer with the Ellsworth Land Survey party, 1968–69.

Elder Bluff is a prominent and mostly bare rock bluff that forms a portion of the north side of Eielson Peninsula and overlooks Smith Inlet, on the east coast of Palmer Land. It was named by the Advisory Committee on Antarctic Names for Robert B. Elder, Chief of the U.S. Coast Guard Oceanographic Unit on the first International Weddell Sea Oceanographic Expedition on board USCGC Glacier in 1968.

Godfrey Upland is a small remnant plateau with an undulating surface and a mean elevation of 1,500 metres (5,000 ft) in south-central Graham Land, Antarctica. It is bounded by Clarke, Meridian, Lammers and Cole Glaciers. The existence of the feature was known to the United States Antarctic Service, 1939–41, Finn Ronne and Carl R. Eklund having traveled along Meridian and Lammers Glaciers in January 1941. It was photographed from the air by the Ronne Antarctic Research Expedition in 1947 and surveyed from the ground by the Falkland Islands Dependencies Survey in 1958. It was named by the UK Antarctic Place-Names Committee after Thomas Godfrey, an American glassworker and mathematician who, at the same time as John Hadley, independently invented the quadrant, in 1730.

Moore Point is a rocky point surmounted by a small peak, fronting on George VI Sound and marking the north side of the mouth of Meiklejohn Glacier, on the west coast of Palmer Land, Antarctica. It was first surveyed in 1936 by the British Graham Land Expedition under John Rymill, and was named by the UK Antarctic Place-Names Committee in 1954 after James I. Moore, second engineer of the Penola during Rymill's expedition.

Millett Glacier is a heavily crevassed glacier in Antarctica, 13 nautical miles (24 km) long and 7 nautical miles (13 km) wide, flowing west from the Dyer Plateau of Palmer Land to George VI Sound, immediately north of Wade Point. In its lower reaches the north side of this glacier merges with Meiklejohn Glacier. Millett Glacier was first surveyed in 1936 by the British Graham Land Expedition (BGLE) under John Rymill, and was named by the UK Antarctic Place-Names Committee in 1954 for Hugh M. Millett, chief engineer of the Penola during the BGLE.

Meiklejohn Glacier is a glacier, 12 nautical miles (22 km) long and 4 nautical miles (7 km) wide, flowing southwest from the Dyer Plateau of Palmer Land, Antarctica, to George VI Sound, immediately south of Moore Point. In its lower reaches the south side of this glacier merges with Millett Glacier. It was first surveyed in 1936 by the British Graham Land Expedition (BGLE) under John Rymill, and was named by the UK Antarctic Place-Names Committee in 1954 for Ian F. Meiklejohn, a radio operator of the BGLE.

Klebelsberg Glacier glacier in Antarctica

Klebelsberg Glacier is a glacier, 7 nautical miles (13 km) long and 2 nautical miles (4 km) wide, situated at the south side of Finsterwalder Glacier and flowing from Hemimont Plateau northwestward between Armula Peak and Smilyan Bastion on Graham Land, Antarctica, toward the head of Lallemand Fjord. With Finsterwalder Glacier and Haefeli Glacier, its mouth merges with Sharp Glacier where the latter enters the fjord. It was first surveyed from the plateau in 1946–47 by the Falkland Islands Dependencies Survey, and named by them for Raimund von Klebelsberg, an Austrian glaciologist.

Scorpio Peaks is a conspicuous massif with two high conical peaks dominating its western end and with a ridge of lower peaks extending eastward. The feature separates Meiklejohn Glacier and Millett Glacier on the west edge of Palmer Land. Named by United Kingdom Antarctic Place-Names Committee (UK-APC) after the constellation of Scorpio.

Sölch Glacier

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.

Taylor Buttresses is an oval shaped, whale-back shaped hill with its smooth contours broken at the northern end by three rock buttresses which are conspicuous from the north, located near the heads of Riley Glacier and Chapman Glacier in western Palmer Land. Named by United Kingdom Antarctic Place-Names Committee (UK-APC) for Brian J. Taylor, British Antarctic Survey (BAS) geologist at Fossil Bluff station, 1961-63.

References

United States Geological Survey scientific agency of the United States government

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.

Geographic Names Information System geographical database

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.