Herbert Mountains
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Herbert Mountains
The Herbert Mountains () are a conspicuous group of rock summits on the east side of Gordon Glacier in the Shackleton Range of Antarctica. They were first mapped in 1957 by the Commonwealth Trans-Antarctic Expedition (and named for Sir Edwin S. Herbert, Chairman of the Finance Committee and a Member of the Committee of Management of the expedition, 1955–58. Features Geographical features include: * Bernhardi Heights * Bonney Bowl * Charlesworth Cliffs * Charpentier Pyramid * Geikie Nunatak * Högbom Outcrops * Hollingworth Cliffs * Jamieson Ridge * Kendall Basin * Maclaren Monolith * Mount Absalom * Ramsay Wedge * Schimper Glacier * Shaler Cliffs * Sumgin Buttress * Venetz Peak References

Mountain ranges of Coats Land {{CoatsLand-geo-stub ...
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Gordon Glacier
Gordon Glacier () is an Antarctic glacier of at least in length flowing in a northerly direction beginning in the Crossover Pass, flowing through the Shackleton Range to finally meet the Slessor Glacier. The glacier was first mapped in 1957 by the Commonwealth Trans-Antarctic Expedition, CTAE, and named after George Patrick Pirie-Gordon, 15th Laird of Buthlaw (died 4 April 2011), who was a member of the Committee of Management and treasurer of the CTAE between 1955 and 1958. See also * List of glaciers in the Antarctic * Glaciology References

Glaciers of Coats Land {{CoatsLand-glacier-stub ...
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Jamieson Ridge
Jamieson Ridge () is a narrow ridge long, rising to about at the southwestern end of the Herbert Mountains, in the Shackleton Range, Antarctica. It was photographed from the air by the U.S. Navy, 1967, and surveyed by the British Antarctic Survey, 1968–71. In association with the names of glacial geologists grouped in this area, it was named by the UK Antarctic Place-Names Committee in 1971 after Thomas F. Jamieson, a Scottish geologist whose work on the ice-worn rocks of Scotland developed the true origin of glacial striae in 1862, and who in 1865 originated the theory of isostasy Isostasy (Greek ''ísos'' "equal", ''stásis'' "standstill") or isostatic equilibrium is the state of gravitational equilibrium between Earth's crust (or lithosphere) and mantle such that the crust "floats" at an elevation that depends on its .... References Ridges of Coats Land {{CoatsLand-geo-stub ...
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Sumgin Buttress
Sumgin Buttress () is a prominent elevated rock mass 2.5 nautical miles (4.6 km) southwest of Charpentier Pyramid, rising to about 1,100 m on the west side of Herbert Mountains, Shackleton Range. It was roughly surveyed by the Commonwealth Trans-Antarctic Expedition of 1957 and was photographed from the air by the U.S. Navy in 1967. It was resurveyed by the British Antarctic Survey (BAS) between 1968 and 1971. In association with the names of glacial geologists grouped in this area, it was named by the United Kingdom Antarctic Place-Names Committee The UK Antarctic Place-Names Committee (or UK-APC) is a United Kingdom government committee, part of the Foreign and Commonwealth Office, responsible for recommending names of geographical locations within the British Antarctic Territory (BAT) an ... (UK-APC) in 1971 after (1873–1942), a Russian pioneer in permafrost research. Mountains of Coats Land {{CoatsLand-geo-stub ...
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Shaler Cliffs
Shaler Cliffs () is a rock cliffs 2 miles (3.2 km) east-southeast of Charpentier Pyramid, rising to 1,000 m in the north part of Herbert 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 glacial geologists grouped in this area, named by the United Kingdom Antarctic Place-Names Committee (UK-APC) after Nathaniel S. Shaler (1841-1906), American geologist, joint author with geographer William Morris Davis William Morris Davis (February 12, 1850 – February 5, 1934) was an American geographer, geologist, geomorphologist, and meteorologist, often called the "father of American geography". He was born into a prominent Quaker family in Philadelphia, ... of Glaciers (Boston, 1881) and of papers on glacial geology, 1884–92. Cliffs of Coats Land {{CoatsLand-geo-stub ...
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Schimper Glacier
Schimper Glacier () is a glacier in the east part of Herbert Mountains, Shackleton Range, flowing north-northeast into Slessor Glacier. 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 glacial geologists grouped in the area, named by the United Kingdom Antarctic Place-Names Committee (UK-APC) after Karl Friedrich Schimper (1803–67), German botanist who in 1835 originated the theory of the Ice Age in Europe to account for the distribution of erratic boulders. See also * List of glaciers in the Antarctic * Glaciology Glaciology (; ) is the scientific study of glaciers, or more generally ice and natural phenomena that involve ice. Glaciology is an interdisciplinary Earth science that integrates geophysics, geology, physical geography, geomorphology, climato ... References * Glaciers of Coats Land {{CoatsLand-glacier-stub ...
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Ramsay Wedge
Ramsay Wedge () is a narrow rock spur, 2 nautical miles (3.7 km) long, with talus slopes rising to about 1,200 m, located 2 nautical miles (3.7 km) southwest of Mount Absalom in the southwest portion of the Herbert 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 glacial geologists grouped in this area, named by the United Kingdom Antarctic Place-Names Committee (UK-APC) after Sir Andrew C. Ramsay (1814–91), Scottish geologist who first recognized the glacial origin of rock basins in 1862; Director-General, Geological Survey of Great Britain Great Britain is an island in the North Atlantic Ocean off the northwest coast of continental Europe. With an area of , it is the largest of the British Isles, the largest European island and the ninth-largest island in the world. It is ..., 1871–81. Ridges of Coats Land {{CoatsLand-g ...
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Mount Absalom
Mount Absalom () is the southernmost and highest (1,640 m) mountain of the Herbert Mountains, in the central part of the Shackleton Range. It was first mapped in 1957 by the Commonwealth Trans-Antarctic Expedition and named for Henry W.L. Absalom, a member of the Scientific Committee on the Commonwealth Trans-Antarctic Expedition The Commonwealth Trans-Antarctic Expedition (CTAE) of 1955–1958 was a Commonwealth-sponsored expedition that successfully completed the first overland crossing of Antarctica, via the South Pole. It was the first expedition to reach the South ... of 1955–58. Mountains of Coats Land {{CoatsLand-geo-stub ...
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Maclaren Monolith
Maclaren Monolith () is a peak rising to about on the central ridge of the Herbert Mountains, Shackleton Range, Antarctica. The feature is notable for a monolith forming the summit. It was photographed from the air by the U.S. Navy in 1967, and surveyed by the British Antarctic Survey between 1968 and 1971. In association with the names of glacial geologists grouped in this area, it was named by the UK Antarctic Place-Names Committee The UK Antarctic Place-Names Committee (or UK-APC) is a United Kingdom government committee, part of the Foreign and Commonwealth Office, responsible for recommending names of geographical locations within the British Antarctic Territory (BAT) and ... in 1971 after Charles Maclaren, a Scottish naturalist who in 1842 was the first to recognize the glacial control of sea level. References Mountains of Coats Land {{CoatsLand-geo-stub ...
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Kendall Basin
Kendall Basin () is an ice-free cirque at the northwest end of the Herbert Mountains, in the Shackleton Range, Antarctica. It was photographed from the air by the U.S. Navy, 1967, and surveyed by the British Antarctic Survey, 1968–71. In association with the names of glacial geologists grouped in this area, it was named by the UK Antarctic Place-Names Committee in 1971 after Percy Fry Kendall, an English glacial geologist, Professor of Geology at Leeds University , mottoeng = And knowledge will be increased , established = 1831 – Leeds School of Medicine1874 – Yorkshire College of Science1884 - Yorkshire College1887 – affiliated to the federal Victoria University1904 – University of Leeds , ... in the early 20th century. References Cirques of Coats Land {{CoatsLand-geo-stub ...
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Hollingworth Cliffs
The Hollingworth Cliffs () are a line of cliffs to the south of Mount Absalom in the Herbert Mountains of the Shackleton Range in Antarctica. They were photographed from the air by the U.S. Navy in 1967, and surveyed by the British Antarctic Survey, 1968–71. In association with the names of glacial geologists grouped in this area, they were named by the UK Antarctic Place-Names Committee after Sydney E. Hollingworth, a British geologist who specialized in the Pleistocene geology of northwest England, and was Professor of Geology at University College London , mottoeng = Let all come who by merit deserve the most reward , established = , type = Public research university , endowment = £143 million (2020) , budget = ..., 1946–66. References Cliffs of Coats Land {{CoatsLand-geo-stub ...
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Shackleton Range
The Shackleton Range is a mountain range in Antarctica. Rising at Holmes Summit to , it extends in an east–west direction for about between the Slessor and Recovery glaciers. The range was named after Sir Ernest Shackleton, leader of the British Imperial Trans-Antarctic Expedition (or "Shackleton's Expedition") of 1914–16. Surveys The Commonwealth Trans-Antarctic Expedition (CTAE), which in 1956 saw the range from the air, conducted a ground-level survey of its western part in 1957. The United States Navy photographed the range from the air in 1967. In 1968–69 and 1969–70, the British Antarctic Survey (based at Halley Station) conducted further ground surveys with support from US Navy C-130 Hercules aircraft. Geology The Haskard Group and Turnpike Bluff Group rest unconformably on the Archean-Middle Proterozoic Shackleton Range Metamorphic Complex. The Ordovician-Early Devonian Blaiklock Glacier Group (475 Ma) also unconformably overlies the Shackleton Range Metam ...
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Högbom Outcrops
The Högbom Outcrops () are rocks rising to about at the eastern side of the terminus of Schimper Glacier in the Herbert Mountains of the Shackleton Range, Antarctica. They were photographed from the air by the U.S. Navy, 1967, and surveyed by the British Antarctic Survey, 1968–71. In association with the names of glacial geologists grouped in this area, the feature was named in 1971 by the UK Antarctic Place-Names Committee after Arvid Högbom (1857–1940), a Swedish geologist who made important contributions to the glacial geology of northern Sweden Sweden, formally the Kingdom of Sweden,The United Nations Group of Experts on Geographical Names states that the country's formal name is the Kingdom of SwedenUNGEGN World Geographical Names, Sweden./ref> is a Nordic country located on .... References Rock formations of Antarctica Landforms of Coats Land {{CoatsLand-geo-stub ...
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