The Jaren Crags ( 71°45′S6°44′E / 71.750°S 6.733°E Coordinates: 71°45′S6°44′E / 71.750°S 6.733°E ) are a row of rock peaks in the form of a bluff, just west of Storkvarvet Mountain in the Mühlig-Hofmann Mountains of Queen Maud Land, Antarctica. They were plotted from surveys and air photos by the Sixth Norwegian Antarctic Expedition (1956–60) and named Jaren (the edge). [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.
Storkvarvet Mountain is a mountain that is round in plan and has several radial spurs, standing N of Habermehl Peak at the NE end of the Muhlig-Hofmann Mountains, Queen Maud Land.
The Mühlig-Hofmann Mountains is a major group of associated mountain features extending east to west for 100 km (62 mi) between the Gjelsvik Mountains and the Orvin Mountains in Queen Maud Land, East Antarctica. With its summit at 3,148 metres (10,328 ft), the massive Jøkulkyrkja Mountain forms the highest point in the Mühlig-Hofmann Mountains.
Ebbe Glacier is a tributary glacier about 60 nautical miles long, draining northwest from the Homerun Range and the Robinson Heights, and then west-northwest between the Everett Range and the Anare Mountains into Lillie Glacier, Victoria Land, Antarctica. This feature saddles with Tucker Glacier, the latter draining southeast to the Ross Sea. The glacier lies situated on the Pennell Coast, a portion of Antarctica lying between Cape Williams and Cape Adare. Robertson Glacier is a tributary glacier to Ebbe Glacier.
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.
Wohlthat Mountains is a large group of associated mountain features consisting of the Humboldt Mountains, Petermann Ranges, and the Gruber Mountains, located immediately east of the Orvin Mountains in Fimbulheimen in the central Queen Maud Land. Discovered by the Third German Antarctic Expedition (1938–1939), led by Capt. Alfred Ritscher, and named for Councilor of state Helmuth C.H. Wohlthat, who as economist and fiscal officer dealt with the organization of the expedition.
Høgfonna Mountain is a high, flat, snow-topped mountain with sheer rock sides, standing 3 miles (5 km) southeast of Hogskavlen Mountain in the Borg Massif, Queen Maud Land, Antarctica. It was mapped by Norwegian cartographers from surveys and air photos by the Norwegian–British–Swedish Antarctic Expedition (1949–1952), led by John Schjelderup Giæver, and named Høgfonna.
Zenith Glacier is a glacier which lies 1 mile (1.6 km) west of Johnstone Glacier and drains south from the south end of Lanterman Range, Bowers Mountains. So named by the New Zealand Geological Survey Antarctic Expedition (NZGSAE) to northern Victoria Land, 1967–68, because the glacier is an important geological outcrop area with an impressive view from the top of much of the Bowers Mountains.
Isdalen Valley is an ice-filled valley between Aurdalsegga Ridge and Isdalsegga Ridge in the Südliche Petermann Range of the Wohlthat Mountains in Antarctica. It was discovered and plotted from air photos by the Third German Antarctic Expedition in 1938–39. It was replotted from air photos and surveys by the Sixth Norwegian Antarctic Expedition in 1956–60 and named "Isdalen".
Geikie Ridge is a massive mountain ridge, 20 nautical miles (37 km) long and 6 nautical miles (11 km) wide, forming the divide between Dugdale Glacier and Murray Glacier in the Admiralty Mountains of Victoria Land, Antarctica. It was first charted by the British Antarctic Expedition, 1898–1900, under Carsten Borchgrevink, who named the high land between these glaciers "Geikie Land", after Sir Archibald Geikie. The generic "Land" has been changed to "Ridge", since it was not appropriate for so small a feature, but Borchgrevink's intent in naming the whole mass has been respected. This geographical feature lies situated on the Pennell Coast, a portion of Antarctica lying between Cape Williams and Cape Adare.
Anders Peak is a peak 2,135 metres (7,000 ft) high, rising 1 nautical mile (2 km) south of the Gruvletindane Crags of the Holtedahl Peaks, in the Orvin Mountains of Queen Maud Land. It was mapped by Norwegian cartographers from air photos and surveys by the Sixth Norwegian Antarctic Expedition, 1956–60, and named for Anders Vinten-Johansen, a medical officer with the expedition, 1957–58.
The Bain Crags are a number of rock exposures, many of which are banded, in the face of or projecting from the ice cliffs along the south part of the west side of Gillock Island in the Amery Ice Shelf. The feature was visited in January 1969 by J.H.C. Bain, geologist with the Australian National Antarctic Research Expeditions Prince Charles Mountains survey party, after whom it is named.
The Östliche Petermann Range is one of the Petermann Ranges, trending in a north-south direction for 15 nautical miles (28 km) from Per Spur to the Gornyye Inzhenery Rocks, in the Wohlthat Mountains of Queen Maud Land. It was discovered and plotted from air photos by German Antarctic Expedition of 1938–39, and so named by them for its eastern location in the Petermann Ranges.
Nicol Crags is a rock crags rising to about 1,300 m to the south of Arkell Cirque in the Read Mountains, Shackleton Range. Photographed from the air by the U.S. Navy, 1967, and surveyed by British Antarctic Survey (BAS), 1968–71. In association with the names of geologists grouped in this area, named by the United Kingdom Antarctic Place-Names Committee (UK-APC) in 1971 after William Nicol (1770–1851), Scottish natural philosopher who devised the Nicol prism and the preparation of thin rock sections, thus contributing to the techniques of microscopy.
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.
The Gruvletindane Crags are rock crags, rising to 2,255 metres (7,400 ft) and forming the north end of the Kurze Mountains of Queen Maud Land, Antarctica. They were mapped from surveys and air photos by the Sixth Norwegian Antarctic Expedition (1956–60) and named Gruvletindane. The feature is bounded on the western side by a large and prominent glacial moraine.
The Gruvleflesa Knolls are two low rock knolls rising above the Antarctic glacial moraine west of the Gruvletindane Crags, in the Kurze Mountains of Queen Maud Land. They were mapped from surveys and air photos by the Sixth Norwegian Antarctic Expedition (1956–60) and named Gruvleflesa.
Douglas Gap is a glacier-filled gap, 1.5 nautical miles (3 km) wide, between the Hedgpeth Heights and the Quam Heights in the Anare Mountains of Victoria Land, 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 Donald S. Douglas, a United States Antarctic Research Program biologist at Hallett Station, 1959–60 and 1960–61. This mountain pass lies situated on the Pennell Coast, a portion of Antarctica lying between Cape Williams and Cape Adare.
Eureka Glacier is a broad, gently sloping glacier, 18 nautical miles (33 km) long and 17 nautical miles (31 km) wide at its mouth, which flows westward from the west side of Palmer Land into George VI Sound. It is bounded on its north side by the nunataks south of Mount Edgell, on its south side by the Traverse Mountains and Terminus Nunatak, and at its head Prospect Glacier provides a route to the Wordie Ice Shelf. It was first surveyed in 1936 by the British Graham Land Expedition (BGLE) under John Rymill and resurveyed in 1948 by the Falkland Islands Dependencies Survey. The name, from the ancient Greek word eureka, expresses the triumph of discovery and arose because the BGLE sledge party found their way to George VI Sound via this glacier in 1936.
Graveson Glacier is a broad north-flowing tributary to the Lillie Glacier, draining that portion of the Bowers Mountains between the Posey Range and the southern part of Explorers Range, Victoria Land, Antarctica. The geographical feature is fed by several lesser tributaries and enters Lillie Glacier via Flensing Icefall. The glacier was so named by the northern party of the New Zealand Geological Survey Antarctic Expedition, 1963–64, for F. Graveson, a mining engineer who wintered at Scott Base in 1963 and was field assistant on this expedition. The glacier lies situated on the Pennell Coast, a portion of Antarctica lying between Cape Williams and Cape Adare.
Mehaugen Hill is the central hill in the group at the east side of Kamp Glacier in the Sør Rondane Mountains of Antarctica. It was mapped by Norwegian cartographers in 1946 from air photos taken by the Lars Christensen Expedition, 1936–37, and in 1957 from air photos taken by U.S. Navy Operation Highjump, 1946-47, and was named "Mehaugen" by the Norwegians.
Kamp Glacier is a glacier, 8 nautical miles (15 km) long, flowing northwest between the Austkampane Hills on the west and Nordhaugen Hill, Mehaugen Hill and Sørhaugen Hill on the east, in the Sør Rondane Mountains of Antarctica. It was mapped by Norwegian cartographers in 1957 from air photos taken by U.S. Navy Operation Highjump, 1946–47, and named Kampbreen.
Larson Crag is a prominent rocky summit, over 1,600 metres (5,250 ft) high, at the north end of the Staten Island Heights in the Convoy Range, Antarctica. It was mapped by the United States Geological Survey from ground surveys and Navy air photos, and was named by the Advisory Committee on Antarctic Names in 1964 for Commander Wesley Larson, commanding officer of the USS Staten Island (AGB-5) in Antarctic waters, 1959–60.
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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