Marble Hills
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Marble Hills
The Marble Hills () are a group of mainly ice-free hills in West Antarctica. They are located on the west side of Horseshoe Valley, between the Liberty Hills and Independence Hills in the southern part of the Heritage Range, Ellsworth Mountains. The hills were named by the University of Minnesota Ellsworth Mountains Party, 1962–63, because the rocks in these hills are composed of marble Marble is a metamorphic rock composed of recrystallized carbonate minerals, most commonly calcite or Dolomite (mineral), dolomite. Marble is typically not Foliation (geology), foliated (layered), although there are exceptions. In geology, the .... Features Geographical features include: * Beitzel Peak * Craddock Crags * Minaret Peak * Mount Fordell References Hills of Ellsworth Land {{EllsworthLand-geo-stub ...
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West Antarctica
West Antarctica, or Lesser Antarctica, one of the two major regions of Antarctica, is the part of that continent that lies within the Western Hemisphere, and includes the Antarctic Peninsula. It is separated from East Antarctica by the Transantarctic Mountains and is covered by the West Antarctic Ice Sheet. It lies between the Ross Sea (partly covered by the Ross Ice Shelf), and the Weddell Sea (largely covered by the Filchner-Ronne Ice Shelf). It may be considered a giant peninsula, stretching from the South Pole towards the tip of South America. West Antarctica is largely covered by the Antarctic ice sheet, but there have been signs that climate change is having some effect and that this ice sheet may have started to shrink slightly. Over the past 50 years, the west coast of the Antarctic Peninsula has been - and still is - one of the most rapidly warming parts of the planet, and the coasts of the Peninsula are the only parts of West Antarctica that become (in summer) ice-free ...
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Horseshoe Valley (Antarctica)
Horseshoe Valley is a large ice-filled valley in the southern Heritage Range of the Ellsworth Mountains of Antarctica. It is outlined by the semicircular arrangement of the Independence, Marble, Liberty and Enterprise Hills. Approval of the descriptive name was suggested by the University of Minnesota Ellsworth Mountains Party, 1962–63, who reported the name was in wide use by U.S. Navy The United States Navy (USN) is the maritime service branch of the United States Armed Forces and one of the eight uniformed services of the United States. It is the largest and most powerful navy in the world, with the estimated tonnage of ... flyers in the area. References Valleys of Antarctica {{EllsworthLand-geo-stub ...
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Liberty Hills (Antarctica)
The Liberty Hills () are a line of rugged hills and peaks with bare rock eastern slopes, about long, standing northwest of the Marble Hills and forming part of the west wall of Horseshoe Valley, in the Heritage Range, Ellsworth Mountains, Antarctica. The Liberty Hills were mapped by the United States Geological Survey from ground surveys and U.S. Navy air photos, 1961–66. The name was applied by the Advisory Committee on Antarctic Names in association with the name Heritage Range. The remarkable High Nunatak towers east of the Hills. Maps Liberty Hills.Scale 1:250 000 topographic map. Reston, Virginia: US Geological Survey, 1966. Antarctic Digital Database (ADD).Scale 1:250000 topographic map of Antarctica. Scientific Committee on Antarctic Research (SCAR). Since 1993, regularly updated. Features Geographical features include: * Horseshoe Valley * Kelley Peak * Moulder Peak * Mount Rosenthal Mount Rosenthal () is a prominent mountain, 1,840 m, at the north end of Libe ...
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Independence Hills
The Independence Hills () are a line of rugged hills and peaks, long, with mainly bare rock eastern slopes. They lie southeast of the Marble Hills and form the southern segment of the west wall of Horseshoe Valley, in the Heritage Range of Antarctica. The Independence Hills were mapped by the United States Geological Survey from ground surveys and U.S. Navy air photos, 1961–66. The name was applied by the Advisory Committee on Antarctic Names in association with the name "Heritage Range". Features Geographical features include: * Marble Hills * Horseshoe Valley * Morris Cliff * Mount Geissel * Mount Shattuck * Mount Simmons * Patriot Hills Patriot Hills () is a line of rock hills 5 nautical miles (9 km) long, located 3 nautical miles (6 km) east of the north end of Independence Hills in Horseshoe Valley, Heritage Range, Western Antarctica. To the north of Patriot Hills ... * Redpath Peaks References

Hills of Ellsworth Land {{EllsworthLand-geo ...
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Heritage Range
The Heritage Range is a major mountain range, long and wide, situated southward of Minnesota Glacier and forming the southern half of the Ellsworth Mountains in Antarctica. The range is complex, consisting of scattered ridges and peaks of moderate height, escarpments, hills and nunataks, with the various units of relief set off by numerous intervening glaciers. The northern portion of the range was probably first sighted by Lincoln Ellsworth in the course of his trans-Antarctic flight of November 23, 1935. On December 14, 1959, the southern range was seen for the first time in a reconnaissance flight from Byrd Station, made by Edward C. Thiel, J. C. Craddock and E. S. Robinson. The team landed at a glacier on Pipe Peak, in the northwestern part of the range, on December 26.Gerald F. Webers, et al., ''Geology and Paleontology of the Ellsworth Mountains, West Antarctica'' (Geological Society of America, 1992), p. xi During the 1962–63 and 1963–64 seasons, the Un ...
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Ellsworth Mountains
The Ellsworth Mountains are the highest mountain ranges in Antarctica, forming a long and wide chain of mountains in a north to south configuration on the western margin of the Ronne Ice Shelf in Marie Byrd Land. They are bisected by Minnesota Glacier to form the Sentinel Range to the north and the Heritage Range to the south. The former is by far the higher and more spectacular with Mount Vinson () constituting the highest point on the continent.Bockheim, J.G., Schaefer, C.E., 2015. ''Soils of Ellsworth Land, the Ellsworth Mountains''. In: Bockheim, J.G. (Ed.), ''The Soils of Antarctica. World Soils Book Series'', Springer, Switzerland, pp. 169–181. The mountains are located within the Chilean Antarctic territorial claim but outside of the Argentinian and British ones. Discovery The mountains were discovered on November 23, 1935, by Lincoln Ellsworth in the course of a trans-Antarctic flight from Dundee Island to the Ross Ice Shelf. He gave them the descriptive name Sentinel ...
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University Of Minnesota
The University of Minnesota, formally the University of Minnesota, Twin Cities, (UMN Twin Cities, the U of M, or Minnesota) is a public university, public Land-grant university, land-grant research university in the Minneapolis–Saint Paul, Twin Cities of Minneapolis and Saint Paul, Minnesota, United States. The Twin Cities campus comprises locations in Minneapolis and Falcon Heights, Minnesota, Falcon Heights, a suburb of St. Paul, approximately apart. The Twin Cities campus is the oldest and largest in the University of Minnesota system and has the List of United States university campuses by enrollment, ninth-largest main campus student body in the United States, with 52,376 students at the start of the 2021–22 academic year. It is the Flagship#Colleges and universities in the United States, flagship institution of the University of Minnesota System, and is organized into 19 colleges, schools, and other major academic units. The Minnesota Territorial Legislature drafted a ...
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Marble
Marble is a metamorphic rock composed of recrystallized carbonate minerals, most commonly calcite or Dolomite (mineral), dolomite. Marble is typically not Foliation (geology), foliated (layered), although there are exceptions. In geology, the term ''marble'' refers to metamorphosed limestone, but its use in stonemasonry more broadly encompasses unmetamorphosed limestone. Marble is commonly used for Marble sculpture, sculpture and as a building material. Etymology The word "marble" derives from the Ancient Greek (), from (), "crystalline rock, shining stone", perhaps from the verb (), "to flash, sparkle, gleam"; Robert S. P. Beekes, R. S. P. Beekes has suggested that a "Pre-Greek origin is probable". This Stem (linguistics), stem is also the ancestor of the English language, English word "marmoreal," meaning "marble-like." While the English term "marble" resembles the French language, French , most other European languages (with words like "marmoreal") more closely resemb ...
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Beitzel Peak
Beitzel Peak () is a peak, high, rising southeast of Minaret Peak in the Marble Hills, Heritage Range. It was named by the Advisory Committee on Antarctic Names for John E. Beitzel, a geophysicist on the United States Antarctic Research Program South Pole—Queen Maud Land Traverse I and II, 1964–65 and 1965–66. The first ascent is credited to British climbers Dominic Spicer and Rob Jarvis Robert S Jarvis (born 1965) is an English television and film actor. He is best known for his roles as Eddie in ''Hustle'' the long running BBC series, Graham Shand in ''Luther'' and as Russell Posner in ''Emmerdale''. From the Wirral, he is fre ... in late December 2009. References Mountains of Ellsworth Land {{EllsworthLand-geo-stub ...
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Craddock Crags
Craddock Crags () are steep, rugged rock summits that rise to about just east of Beitzel Peak in the Marble Hills, Heritage Range, Ellsworth Mountains. They were named by the Advisory Committee on Antarctic Names (2004) after John P. Craddock, a geologist who was a member of a United States Antarctic Research Program The United States Antarctic Program (or USAP; formerly known as the United States Antarctic Research Program or USARP and the United States Antarctic Service or USAS) is an organization of the United States government which has presence in the A ... 1979–80 Ellsworth Mountains expedition. References * Cliffs of Ellsworth Land {{EllsworthLand-geo-stub ...
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Minaret Peak
Fatima namagari' '' is a distinctive rock peak at the northwest end of the Marble Hills in the Heritage Range, Ellsworth Mountains, Antarctica. It was named by the University of Minnesota Ellsworth Mountains Party of 1962–63 because the peak resembles a minaret. See also * Mountains in Antarctica This is a list of all the Ultra prominent peaks (with topographic prominence greater than 1,500 metres) in Antarctica. Some islands in the South Atlantic have also been included and can be found at the end of the list. Antarctica South Atl ... References Ellsworth Mountains Mountains of Ellsworth Land {{EllsworthLand-geo-stub ...
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Mount Fordell
Mount Fordell () is a mountain, high, marking the south end of the Marble Hills in the Heritage Range, Antarctica. It was named by the Advisory Committee on Antarctic Names for Lieutenant William D. Fordell, U.S. Navy, a co-pilot of LC-47 aircraft, who perished in a plane crash on the Ross Ice Shelf on February 2, 1966. See also * Mountains in Antarctica This is a list of all the Ultra prominent peaks (with topographic prominence greater than 1,500 metres) in Antarctica. Some islands in the South Atlantic have also been included and can be found at the end of the list. Antarctica South Atl ... References Mountains of Ellsworth Land {{EllsworthLand-geo-stub ...
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