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Nimitz Glacier
The Nimitz Glacier is an Antarctic glacier, long and wide, draining the area about west of the Vinson Massif and flowing southeast between the Sentinel Range and Bastien Range to enter Minnesota Glacier, in the central Ellsworth Mountains. Discovered by USN Squadron VX-6 on photographic flights of December 14-December 15, 1959, and mapped by United States Geological Survey from these photos. Named by US-ACAN for Fleet Admiral Chester Nimitz Chester William Nimitz (; February 24, 1885 – February 20, 1966) was a fleet admiral in the United States Navy. He played a major role in the naval history of World War II as Commander in Chief, US Pacific Fleet, and Commander in C ..., USN, who as Chief of Naval Operations at the time of Operation Highjump, 1947–1948, made possible that unprecedentedly large and complex Antarctic expedition. Tributary glaciers * Karasura Glacier * Branscomb Glacier * Cairns Glacier * Tulaczyk Glacier * Zapol Glacier * Donnellan Gla ...
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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 Sent ...
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Karasura Glacier
Karasura Glacier ( bg, ледник Карасура, lednik Karasura, ) is the long and wide glacier on the northeast side of Bastien Range in Ellsworth Mountains, Antarctica. It drains the north slopes of Bergison Peak and the east slopes of Patmos Peak, flows northwards, leaves the range and enters the southeast flowing Nimitz Glacier. The glacier is named after the ancient Roman and medieval settlement of Karasura in Southern Bulgaria. Location Karasura Glacier is centred at . US mapping in 1961 and 1988. See also * List of glaciers in the Antarctic * Glaciology Maps Vinson Massif. Scale 1:250 000 topographic map. Reston, Virginia: US Geological Survey, 1988. Antarctic Digital Database (ADD).Scale 1:250000 topographic map of Antarctica. Scientific Committee on Antarctic Research (SCAR). Since 1993, regularly updated. References Karasura GlacierSCAR A scar (or scar tissue) is an area of fibrous tissue that replaces normal skin after an injury. Scars result ...
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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, climatology, meteorology, hydrology, biology, and ecology. The impact of glaciers on people includes the fields of human geography and anthropology. The discoveries of water ice on the Moon, Mars, Europa and Pluto add an extraterrestrial component to the field, which is referred to as "astroglaciology". Overview A glacier is an extended mass of ice formed from snow falling and accumulating over a long period of time; glaciers move very slowly, either descending from high mountains, as in valley glaciers, or moving outward from centers of accumulation, as in continental glaciers. Areas of study within glaciology include glacial history and the reconstruction of past glaciation. A glaciologist is a person who studies glaciers. A glacia ...
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List Of Glaciers In The Antarctic
There are many glaciers in the Antarctic. This set of lists does not include ice sheets, ice caps or ice fields, such as the Antarctic ice sheet, but includes glacial features that are defined by their flow, rather than general bodies of ice. The lists include outlet glaciers, valley glaciers, cirque glaciers, tidewater glaciers and ice streams. Ice streams are a type of glacier and many of them have "glacier" in their name, e.g. Pine Island Glacier. Ice shelves are listed separately in the List of Antarctic ice shelves. For the purposes of these lists, the Antarctic is defined as any latitude further south than 60° (the continental limit according to the Antarctic Treaty System). List by letters * List of glaciers in the Antarctic: A–H * List of glaciers in the Antarctic: I–Z See also * List of Antarctic and subantarctic islands * List of Antarctic ice rises * List of Antarctic ice shelves * List of Antarctic ice streams * List of glaciers * List of s ...
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Sirma Glacier
Sirma Glacier ( bg, ледник Сирма, lednik Sirma, ) is the long and wide glacier on the west side of Owen Ridge in southern Sentinel Range, Ellsworth Mountains in Antarctica, situated south of Bolgrad Glacier, and flowing west-southwestwards from Mount Southwick, Mount Milton and Mount Inderbitzen to leave the range and join Nimitz Glacier northwest of Modren Peak. The glacier is named after the Bulgarian woman rebel leader Sirma Voyvoda (1773-1858). Location Sirma Glacier is centred at . US mapping in 1961, updated in 1988. 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, c ... Maps Vinson Massif. Scale 1:250 000 topographic map. Reston, Virginia: US Geological Survey, 1988. Antarctic Digital Database (AD ...
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Bender Glacier
Bender Glacier () is a glacier that flows from Mount Atkinson and Mount Craddock southwards between Chaplin Peak and Krusha Peak, and joins Nimitz Glacier just south of Gilbert Spur in the southern Sentinel Range, Ellsworth Mountains in Antarctica. Receiving ice influx from its left tributaries Severinghaus Glacier, Brook Glacier and Bolgrad Glacier. It was named by the Advisory Committee on Antarctic Names (2006) after Professor Michael L. Bender at the Department of Geosciences (Geochemistry), Princeton University (earlier at the Graduate School of Oceanography, University of Rhode Island), whose paleoclimate research from 1984 centered on the glacial-interglacial climate change and the global carbon cycle. Tributary glaciers * Severinghaus Glacier * Brook Glacier * Bolgrad Glacier 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 i ...
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Gildea Glacier
Gildea Glacier is a glacier long and wide flowing southwestward from Craddock Massif between Mount Slaughter and Mount Atkinson into Nimitz Glacier, in the Sentinel Range of the Ellsworth Mountains, Antarctica. The upper portion of the glacier also receives ice from Hammer Col and southern Vinson Massif. It was named by the Advisory Committee on Antarctic Names in 2006 after Damien Gildea, the Australian leader of several Omega Foundation expeditions to the Sentinel Range and Livingston Island in 2000–07. He made an ascent of Mount Craddock from the Bender Glacier in 2005, and directed the preparation of a 1:50,000-scale map of the Vinson Massif area for publication by the Omega Foundation in 2006. 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 ...
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Donnellan Glacier
Donnellan Glacier () is a steep valley glacier fed by highland ice adjacent to Opalchenie Peak and Fukushima Peak on Vinson Plateau, the summit plateau of Vinson Massif, in the Sentinel Range of the Ellsworth Mountains, Antarctica. The glacier flows west-southwestward from Opalchenie Peak along the northwest side of Mount Slaughter into Nimitz Glacier. The glacier was named by the Advisory Committee on Antarctic Names in 2006 after Andrea Donnellan of the Satellite Geodesy and Geodynamics Systems Group at the Jet Propulsion Laboratory, California Institute of Technology, who was involved from the mid-1990s in research projects involving the use of GPS in studies of earth crustal deformation in Southern California and also in Antarctica. 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 in ...
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Zapol Glacier
Zapol Glacier () is a steep valley glacier draining the west slope of Vinson Massif south of Silverstein Peak and Príncipe de Asturias Peak, and descending between Tulaczyk Glacier and Donnellan Glacier in the Sentinel Range, Antarctica. The glacier flows southwestward and leaving the range joins Nimitz Glacier south of Hodges Knoll. It was named by US-ACAN (2006) after Dr. Warren M. Zapol, Department of Anesthesia, Massachusetts General Hospital, whose long-term research near McMurdo Station on diving physiology of Weddell seals (begun mid-1970s) was part of a larger effort to understand how gas is handled in mammals as part of a search to understand SIDS (Sudden Infant Death Syndrome). 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, ...
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Tulaczyk Glacier
Tulaczyk Glacier () is a steep valley glacier draining the west slope of Vinson Massif southwest of Príncipe de Asturias Peak, and descending between Cairns Glacier and Zapol Glacier in the Sentinel Range, Antarctica. The glacier flows southwestward and leaving the range, together with Cairns Glacier joins Nimitz Glacier west of Hodges Knoll and southeast of Klenova Peak. It was named by US-ACAN (2006) after Slawek M. Tulaczyk, Earth Sciences, University of California, Santa Cruz; USAP researcher of West Antarctic ice streams from 1998. 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, c ... Maps Vinson Massif. Scale 1:250 000 topographic map. Reston, Virginia: US Geological Survey, 1988. Antarctic Digital Database (ADD).S ...
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Cairns Glacier
Cairns Glacier () is a glacier on the west slope of Vinson Massif, Sentinel Range in Antarctica, situated between Branscomb Glacier and Tulaczyk Glacier. It flows along the northwest side of Brichebor Peak southwestwards, and leaving the range together with Tulaczyk Glacier joins Nimitz Glacier southeast of Klenova Peak. The feature was named by US-ACAN (2006) after Stephen Douglas Cairns, research zoologist, Department of Invertebrate Zoology, National Museum of Natural History, Smithsonian Institution, 1985–2006; Board of Associated Editors, Antarctic Research Series, American Geophysical Union, 1990–95. 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, c ... Maps Vinson Massif. Scale 1:250 000 topographic map. Res ...
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Branscomb Glacier
The Branscomb Glacier () is an Antarctic glacier, long, flowing west from the north-west side of Vinson Massif (the highest point in Antarctica) into Nimitz Glacier, in the Sentinel Range of the Ellsworth Mountains. Its upper course receives ice influx from both Goodge Col and Jacobsen Valley, while the tributary Roché Glacier joins Branscomb Glacier just northwest of Príncipe de Asturias Peak. The glacier was mapped by the USGS from surveys and USN aerial photographs between 1957 and 1960. It was named by US-ACAN after Lewis M. Branscomb, Chairman of the National Science Board from 1982 to 1984. 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, c ... Maps Vinson Massif. Scale 1:250 000 topographic map. Reston, Vir ...
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