Elephant Ridge

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Elephant Ridge ( 71°20′S68°19′W / 71.333°S 68.317°W / -71.333; -68.317 Coordinates: 71°20′S68°19′W / 71.333°S 68.317°W / -71.333; -68.317 ) is a sharp curved ridge in Antarctica, orientated generally west–east, and extending for about 0.5 nautical miles (1 km), with the highest point at the center rising to 6,999 metres (22,963 ft). The northern slopes are snow and ice free, and the central point is situated about 0.7 nautical miles (1.3 km) south-southeast of Khufu Peak and 0.9 nautical miles (1.7 km) southwest of Giza Peak. Uranus Glacier forms the southern boundary of the feature. Elephant Ridge is referred to as "Man Pack Hill" in scientific reports in the early 1960s, and is locally known descriptively as "The Elephant". The summit resembles an elephant's head, with the ridge forming the trunk. [1]

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.

Khufu Peak is a peak rising to about 745 m located in Planet Heights, near the center of the Fossil Bluff massif, on the east side of Alexander Island, Antarctica, in which the east face of the peak faces towards George VI Sound and the George VI Ice Shelf. For many years this was known to British Antarctic Survey (BAS) workers by the unofficial descriptive name "Pyramid," a name already in use. To avoid duplication, in 1987 the United Kingdom Antarctic Place-Names Committee (UK-APC) applied a new name after Khufu, the second Pharaoh of the Fourth Dynasty of Egypt, who erected the Great Pyramid of El Giza.

Giza Peak

Giza Peak is a peak rising to about 600 metres (2,000 ft) on the east side of the Fossil Bluff massif, eastern Alexander Island, Antarctica. For many years this peak was known to the British Antarctic Survey (BAS) workers as "Sphinx," a name already in use. To avoid duplication, the UK Antarctic Place-Names Committee in 1987 applied the name Giza Peak to this feature in reference to the site of the colossal statue of the Sphinx at El Giza, Egypt.

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The Prince Charles Mountains are a major group of mountains in Mac. Robertson Land in Antarctica, including the Athos Range, the Porthos Range, and the Aramis Range. The highest peak is Mount Menzies. Other prominent peaks are Mount Izabelle and Mount Stinear. These mountains together with other scattered peaks form an arc about 260 miles long, extending from the vicinity of Mount Starlight in the north to Goodspeed Nunataks in the south.

Explorers Range

Explorers Range is a large mountain range in the Bowers Mountains of Victoria Land, Antarctica, extending from Mount Bruce in the north to Carryer Glacier and McLin Glacier in the south. Named by the New Zealand Antarctic Place-Names Committee (NZ-APC) for the northern party of New Zealand Geological Survey Antarctic Expedition (NZGSAE), 1963–64, whose members carried out a topographical and geological survey of the area. The names of several party members are assigned to features in and about this range. All of the geographical features listed below lie situated on the Pennell Coast, a portion of Antarctica lying between Cape Williams and Cape Adare.

Finsterwalder Glacier glacier in Antarctica

Finsterwalder Glacier is a glacier on the northwest side of Hemimont Plateau, 2 nautical miles wide and 10 nautical miles long, flowing southwest from the central plateau of Graham Land, Antarctica, toward the head of Lallemand Fjord. Its mouth lies between the mouths of Haefeli Glacier and Klebelsberg Glacier, the three glaciers merging 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 Sebastian Finsterwalder and his son, Richard Finsterwalder, German glaciologists.

Blodwen Peak(71°20′S68°22′W) is a peak on the Alexander Island, the largest island of Antarctica.

Copland Peak is a peak 3 nautical miles (6 km) northeast of the Mussorgsky Peaks and about 1.2 miles (2 km) south of Mazza Point near the tip of Derocher Peninsula, in the north central area of Beethoven Peninsula, situated in southwest Alexander Island, Antarctica. It was mapped by the United States Geological Survey from U.S. Navy aerial photographs taken 1967–68 and from Landsat imagery taken 1972–73. In association with names of composers in the area, it was named by the Advisory Committee on Antarctic Names after Aaron Copland, the American composer (1900-90).

Drune Hill is a rounded flat topped mountain rising to about 680 metres (2,230 ft), and located about 0.5 nautical miles (1 km) north of Khufu Peak, separated from it by Khufu Corrie, and about 0.5 nautical miles northeast of Pearce Dome, situated on the east coast of Alexander Island, Antarctica. The name is used by those working in the area, however, the origin of the name remains unknown.

Elsner Ridge is a narrow, southwest-trending ridge, or spur, 6 nautical miles (11 km) long, located 4 nautical miles (7 km) northeast of the south end of the Homerun Range in the Admiralty Mountains of Victoria Land, Antarctica. It was mapped by the United States Geological Survey from surveys and U.S. Navy, aerial photographs, 1960–63, and was named by the Advisory Committee on Antarctic Names for Robert W. Elsner, a United States Antarctic Research Program biologist at McMurdo Station, Hut Point Peninsula, Ross Island, 1967–68, 1968–69 and 1969–70. The ridge lies situated on the Pennell Coast, a portion of Antarctica lying between Cape Williams and Cape Adare.

Eros Glacier is a glacier on the east coast of Alexander Island, Antarctica, 7 nautical miles (13 km) long and 2 nautical miles (4 km) wide at its mouth, flowing southeast from the Planet Heights into George VI Sound immediately north of Fossil Bluff. It was probably first seen on November 23, 1935, by Lincoln Ellsworth, who flew directly over the glacier and obtained photos of features north and south of it. The mouth of the glacier was observed and positioned by the British Graham Land Expedition in 1936 and the Falkland Islands Dependencies Survey (FIDS) in 1948 and 1949. The glacier was mapped in detail from air photos taken by the Ronne Antarctic Research Expedition, 1947–48, by D. Searle of the FIDS in 1960. It was named by the UK Antarctic Place-Names Committee after the minor planet Eros in association with nearby Pluto Glacier and Uranus Glacier.

Pearce Dome is a dome shaped mountain rising to about 789 m that is snow and ice free on the north slopes and is situated about 0.5 nautical miles (0.9 km) west-northwest of Khufu Peak and 0.6 nautical miles (1.1 km) due east of Blodwen Peak, situated on the east coast of Alexander Island overlooking George VI Sound and the George VI Ice Shelf, Antarctica. The feature was referred to descriptively as The Snow Dome in scientific reports in the early 1960s, and referred to as Dome by those working in the area. Named for C.J. Pearce, a Falkland Islands Dependencies Survey Meteorologist who spent the first winter season (1961) at Fossil Bluff along with B.J. Taylor and J.P. Smith.

The Gadsden Peaks are a line of northeast-trending peaks on a ridge, 5 nautical miles (9 km) long. They rise to over 2,500 metres (8,200 ft) and stand 5 nautical miles west-southwest of Lange Peak of the Lyttelton Range, in the Admiralty Mountains of Victoria Land. Antarctica. They were mapped by the United States Geological Survey from surveys and U.S. Navy aerial photographs, 1960–63, and were named by the Advisory Committee on Antarctic Names for Michael Gadsden, a radioscience researcher at McMurdo Station, Hut Point Peninsula, Ross Island, 1965–66 and 1967–68. These peaks lie situated on the Pennell Coast, a portion of Antarctica lying between Cape Williams and Cape Adare.

Morelli Ridge is a ridge, 2.7 nautical miles (5 km) long, that extends north from Hoehn Peak into the upper part of Bartley Glacier, in the Asgard Range of Victoria Land, Antarctica. It was named by the Advisory Committee on Antarctic Names in 1997 after Frank A. Morelli of the Bioscience and Planetology Section at the Jet Propulsion Laboratory of the California Institute of Technology, who studied the surface distribution of microorganisms in soils of the McMurdo Dry Valleys in the 1970–71 field season. Morelli was also a member of the environmental monitoring team for the Dry Valley Drilling Project in 1973–74.

Mount Morris (Antarctica) mountain in Antarctica

Mount Morris is a steep, sharp mountain about 1 nautical mile (2 km) south of Mount Ostenso, in the main ridge of the Sentinel Range of the Ellsworth Mountains in Antarctica. It surmounts Patton Glacier to the eas-northeast.

Mathys Bank is a rock ridge rising to about 750 metres (2,500 ft), located 2.5 nautical miles (5 km) southwest of Mount Etchells in the La Grange Nunataks, Shackleton Range, Antarctica. It was photographed from the air by the U.S. Navy, 1967, and surveyed by the British Antarctic Survey (BAS), 1968–71. It was named by the UK Antarctic Place-Names Committee after Nicholas Mathys, BAS general assistant at Halley Station, 1967–69, who worked in the Shackleton Range in summer 1968–69.

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.

McClary Glacier is a glacier 10 nautical miles (19 km) long and 2 nautical miles (4 km) wide on the west coast of Graham Land, Antarctica. It flows southwest along the north side of Butson Ridge into Marguerite Bay between Cape Calmette and the Debenham Islands. The glacier was first roughly surveyed by the British Graham Land Expedition, 1936–37, and resurveyed by the Falkland Islands Dependencies Survey, 1946–50. It was named by the UK Antarctic Place-Names Committee for George B. McClary, father of Nelson McClary, mate on the Port of Beaumont during the Ronne Antarctic Research Expedition, 1947–48.

Steeple Point is a low ice-covered point on the west coast of Palmer Land, approximately 2 nautical miles (3.7 km) west of Sandau Nunatak of the Steeple Peaks. The point was named by United Kingdom Antarctic Place-Names Committee (UK-APC) in association with the Steeple Peaks.

Stamper Peak is a peak (2,180 m) 10 nautical miles (18 km) east-northeast of Mount Gilruth in the Admiralty Mountains. It rises from the south-central part of the ridge separating Dugdale and Ommanney Glaciers. Mapped by the United States Geological Survey (USGS) from surveys and U.S. Navy air photos, 1960–63. Named by Advisory Committee on Antarctic Names (US-ACAN) for Wilburn E. Stamper, RM2, U.S. Navy, radioman at McMurdo Station, 1967.

Khufu Corrie is a cirque roughly 0.3 nautical miles (0.6 km) across formed between Drune Hill to the north and Khufu Peak to the south on the east coast of Alexander Island, Antarctica. It was referred to as the "Fossil Bluff Glacier" in scientific reports in the early 1960s, Fossil Bluff being nearby, and is sometimes referred to today as "Moraine Corrie" and "Moraine Corrie Valley". The name is derived from Khufu Peak.

Rubble Glacier is an ice filled valley in the Palmer Land region of the Antarctic Peninsula. It is surrounded by Giza Peak and the ridge connecting it to Baily Ridge to the north and Elephant Ridge to the south. Rubble Glacier is referred to as "Man Pack Glacier" in scientific reports of the early 1960s, but is now descriptively referred to as Rubble Glacier or sometimes as "Louis Glacier".

References

PD-icon.svg This article incorporates  public domain material from the United States Geological Survey document "Elephant Ridge" (content from the Geographic Names Information System ).

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.