Moore Ridge

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Moore Ridge ( 73°7′S161°45′E / 73.117°S 161.750°E / -73.117; 161.750 Coordinates: 73°7′S161°45′E / 73.117°S 161.750°E / -73.117; 161.750 ) is the northernmost ridge of the Caudal Hills in Victoria Land, Antarctica. It was mapped by the United States Geological Survey from surveys and U.S. Navy air photos, 1960–64, and was named by the Advisory Committee on Antarctic Names for Bruce F. Moore, a photographer with U.S. Navy Squadron VX-6 at McMurdo Station in 1966. [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.

The Caudal Hills are a group of hills situated within Victoria Land, Antarctica the hills lie between the Sequence Hills and the Lichen Hills on the western margin of upper Rennick Glacier. A series of spurs "tail" out to the north, hence the name "Caudal". They were so named by the northern party of New Zealand Geological Survey Antarctic Expedition, 1962–63. The Caudal Hills lies situated on the Pennell Coast, a portion of Antarctica lying between Cape Williams and Cape Adare.

Victoria Land region of Antarctica

Victoria Land is a region of Antarctica which fronts the western side of the Ross Sea and the Ross Ice Shelf, extending southward from about 70°30'S to 78°00'S, and westward from the Ross Sea to the edge of the Antarctic Plateau. It was discovered by Captain James Clark Ross in January 1841 and named after the UK's Queen Victoria. The rocky promontory of Minna Bluff is often regarded as the southernmost point of Victoria Land, and separates the Scott Coast to the north from the Hillary Coast of the Ross Dependency to the south.

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Neptune Range

The Neptune Range is a mountain range, 112 km (70 mi) long, lying WSW of Forrestal Range in the central part of the Pensacola Mountains in Antarctica. The range is composed of Washington Escarpment with its associated ridges, valleys and peaks, the Iroquois Plateau, and the Schmidt and Williams Hills. It was discovered and photographed on January 13, 1956 on a US Navy transcontinental plane flight from McMurdo Sound to Weddell Sea and return.

Lillie Glacier glacier

Lillie Glacier is a large glacier in Antarctica, about 100 nautical miles (190 km) long and 10 nautical miles (19 km) wide. It lies between the Bowers Mountains on the west and the Concord Mountains and Anare Mountains on the east, flowing to Ob' Bay on the coast and forming the Lillie Glacier Tongue.

The Quartermain Mountains are a group of exposed mountains in Antarctica, about 32 kilometers long, typical of ice-free features of the McMurdo Dry Valleys, Victoria Land, located south of Taylor Glacier and bounded by Finger Mountain, Mount Handsley, Mount Feather and Tabular Mountain; also including Knobhead, Terra Cotta Mountain, New Mountain, Beacon Heights, Pyramid Mountain, Arena Valley, Kennar Valley, Turnabout Valley and the several valleys and ridges within Beacon Valley.

Shoemaker Glacier is a tributary glacier in the Southern Cross Mountains of Antarctica, flowing east along the south side of Daley Hills to Aviator Glacier, in Victoria Land. Mapped by United States Geological Survey (USGS) from surveys and U.S. Navy air photos, 1960-64. Named by Advisory Committee on Antarctic Names (US-ACAN) after Lieutenant Brian H. Shoemaker, U.S. Navy, helicopter pilot with Squadron VX-6 at McMurdo Station, 1967.

Astakhov Glacier glacier in Antarctica

Astakhov Glacier is the glacier next south of Chugunov Glacier in the Explorers Range, Bowers Mountains. It flows northeast from Mount Hager and enters Ob' Bay just west of Platypus Ridge, the glacier is situated in Victoria Land, Antarctica. It was mapped by the United States Geological Survey from surveys and from U.S. Navy air photos, 1960–65, and named by the Advisory Committee on Antarctic Names for Petr Astakhov, Soviet exchange scientist at the U.S. South Pole Station in 1967. The glacier lies on the Pennell Coast, a portion of Antarctica lying between Cape Williams and Cape Adare.

Wood Ridge is a flat-topped, ice-covered ridge, 7 nautical miles (13 km) long, extending in a north-south direction between Campbell and Styx Glaciers in the Southern Cross Mountains, Victoria Land. Mapped by United States Geological Survey (USGS) from surveys and U.S. Navy air photos, 1955-63. Named by Advisory Committee on Antarctic Names (US-ACAN) for Vernon P. Wood, U.S. Navy yeoman, a member of the McMurdo Station winter parties of 1963 and 1967.

The Brawn Rocks are prominent isolated rocks extending over 3 nautical miles (6 km), lying 12 nautical miles (22 km) southwest of the Sequence Hills in Victoria Land, Antarctica. They were mapped by the United States Geological Survey from surveys and from U.S. Navy air photos, 1960–64, and named by the Advisory Committee on Antarctic Names for James E. Brawn, an aviation machinist's mate with U.S. Navy Squadron VX-6 at McMurdo Station, 1966. These large rock formations lie situated on the Pennell Coast, a portion of Antarctica lying between Cape Williams and Cape Adare.

Church Ridge is a southwest-trending ridge, 10 nautical miles (19 km) long, with several peaks over 2,000 metres (6,600 ft) high. The ridge separates the flow of nearby Church Glacier and Leander Glacier in the Admiralty Mountains, a major mountain range lying situated in Victoria Land, Antarctica. The ridge was mapped by the United States Geological Survey from surveys and from U.S. Navy aerial photography, 1960–63, and named by the Advisory Committee on Antarctic Names for Commander A.E. Church, U.S. Navy, assistant chief of staff for civil engineering with the U.S. Naval Support Force, Antarctica, 1967 and 1968. The ridge lies on the Pennell Coast, a portion of Antarctica lying between Cape Williams and Cape Adare.

Wasson Rock is a prominent, mainly ice-free rock situated along the north wall near the head of Priestley Glacier, Victoria Land. Mapped by United States Geological Survey (USGS) from surveys and U.S. Navy air photos, 1960-64. Named by Advisory Committee on Antarctic Names (US-ACAN) for William G. Wasson, aviation electrician's mate with U.S. Navy Squadron VX-6 at McMurdo Station, 1966.

Whitcomb Ridge is a high, ice-covered ridge along the south side of the head of Gair Glacier, standing 6 nautical miles (11 km) southeast of Mount Supernal in the Mountaineer Range of Victoria Land. Mapped by United States Geological Survey (USGS) from surveys and U.S. Navy air photos, 1960-64. Named by Advisory Committee on Antarctic Names (US-ACAN) for Jean P. Whitcomb, radio scientist at McMurdo Station, 1965–66 and 1966-67.

The Daley Hills are a group of high, ice-covered hills along the west side of Aviator Glacier between the mouths of Cosmonette Glacier and Shoemaker Glacier, in Victoria Land. The hills were mapped by the United States Geological Survey from surveys and from U.S. Navy air photos, 1960–64, and named by the Advisory Committee on Antarctic Names for Robert C. Daley, U.S. Navy, flight engineer on Hercules aircraft during U.S. Navy Operation Deepfreeze, 1966, 1967 and 1968.

Mount Stubberud is a mountain, 2,970 m, standing 2 nautical miles (3.7 km) southeast of Beck Peak on a ridge from the north side of Nilsen Plateau, in the Queen Maud Mountains. Mapped by United States Geological Survey (USGS) from surveys and U.S. Navy air photos, 1960-64. Named by Advisory Committee on Antarctic Names (US-ACAN) for Jorgen Stubberud, carpenter on the ship Fram and member of the land party at Framheim on Amundsen's expedition of 1910-12. This naming preserves the spirit of Amundsen's 1911 commemoration of "Mount J. Stubberud," a name applied for an unidentifiable mountain in the general area.

Freyberg Mountains

The Freyberg Mountains are a group of mountains in Victoria Land, Antarctica, bounded by Rennick Glacier, Bowers Mountains, Black Glacier, and Evans Neve. Named for New Zealand's most famous General, Lord Bernard Freyberg, by the Northern Party of New Zealand Geological Survey Antarctic Expedition (NZGSAE), 1963-64. This mountain group includes the Alamein Range. These topographical features all lie situated on the Pennell Coast, a portion of Antarctica lying between Cape Williams and Cape Adare.

Tranter Glacier is a glacier in the north part of Queen Elizabeth Range, draining into Nimrod Glacier between Mount Chivers and Mount Boman. Mapped by the United States Geological Survey (USGS) from tellurometer surveys and Navy air photos, 1960-62. Named by Advisory Committee on Antarctic Names (US-ACAN) for David L. Tranter, United States Antarctic Research Program (USARP) glaciologist at Roosevelt Island, 1962-63.

Douglas Glacier is a glacier that flows east-northeast through the central Werner Mountains in Palmer Land. The glacier merges with Bryan Glacier just north of Mount Broome where it enters New Bedford Inlet. It was mapped by the United States Geological Survey from ground surveys and U.S. Navy air photos, 1961–67, and was named by the Advisory Committee on Antarctic Names for Everett L. Douglas, a biologist at Palmer Station, summer 1967–68.

Mount Pollock is a symmetrical mountain (2,640 m) that rises above the mid-portion of Recoil Glacier just south of Archambault Ridge, in the Deep Freeze Range, Victoria Land. Mapped by United States Geological Survey (USGS) from surveys and US. Navy air photos, 1960–64. Named by Advisory Committee on Antarctic Names (US-ACAN) for Herbert W. Pollock, U.S. Navy, construction electrician at McMurdo Station, 1962 and 1967.

Ellis Ridge is an ice-covered ridge, 10 nautical miles (19 km) long and 1.5 nautical miles (3 km) wide, extending northeast from Jenkins Heights between Dorchuck Glacier and Keys Glacier, on the Walgreen Coast of Marie Byrd Land, Antarctica. It was mapped by the United States Geological Survey (USGS) from surveys and U.S. Navy aerial photographs, 1959–67, and from U.S. Landsat imagery, 1972–73. It was named by the Advisory Committee on Antarctic Names for Melvin Y. Ellis, a USGS cartographer who was a member of the USGS satellite surveying team at South Pole Station, winter party 1974.

Folk Ridge is a ridge just southeast of Moore Ridge and parallel to it in the Caudal Hills of Victoria Land, Antarctica. The ridge was first mapped by the United States Geological Survey from surveys and U.S. Navy air photos, 1960–64, and was named by the Advisory Committee on Antarctic Names for John E. Folk, a biolab technician at McMurdo Station, Hut Point Peninsula, Ross Island, 1965–66. The feature lies situated on the Pennell Coast, a portion of Antarctica lying between Cape Williams and Cape Adare.

Gondola Ridge is a high rocky ridge just south of Mackay Glacier, extending northeast from Mount Suess for about 4 nautical miles (7 km) in Victoria Land, Antarctica. It was charted by the Western Geological Party of the British Antarctic Expedition, 1910–13, who so named it because Mount Suess, to which the ridge is joined, resembles a gondola in shape.

Heth Ridge is a ridge 3 nautical miles (6 km) long, located 4 nautical miles (7 km) south of the Hornblende Bluffs and near the head of Suvorov Glacier, in the Wilson Hills of Antarctica. It was mapped by the United States Geological Survey from surveys and U.S. Navy air photos, 1960–63, and was named by the Advisory Committee on Antarctic Names for Samuel R. Heth, a United States Antarctic Research Program biologist at Hallett Station, 1968–69.

References

PD-icon.svg This article incorporates  public domain material from the United States Geological Survey document "Moore 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.