Backdrop Ridge
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Backdrop Ridge
Backdrop Ridge () is an east–west ridge running to the north of The Stage on the north side of Renegar Glacier, Scott Coast, Antarctica. The ridge links the northern ends of the West, Central, and East Aisle Ridges, and was named by a New Zealand Geological Survey GNS Science ( mi, Te Pū Ao), officially registered as the Institute of Geological and Nuclear Sciences Limited, is a New Zealand Crown Research Institute. It focuses on geology, geophysics (including seismology and volcanology), and nuclear sc ... field party, 1977–78, led by D. N. B. Skinner, the name being derived from the ridge's position relative to The Stage. References * Ridges of Victoria Land Scott Coast {{ScottCoast-geo-stub ...
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The Stage (Antarctica)
The Stage is a prominent moraine floored amphitheater (a cirque) between West Aisle Ridge and Central Aisle Ridge on the north side of Renegar Glacier, Scott Coast. The cirque floor, at , is relatively flat. The feature was visited by D. N. B. Skinner, D. N. B. Skinner's New Zealand Geological Survey field party, 1977–78, which suggested the name; viewed from the lower Renegar Glacier the elevated floor of the amphitheater appears to be the ideal stage for some great theater. See also *Backdrop Ridge References

* Cirques of Antarctica Landforms of Victoria Land Scott Coast {{ScottCoast-geo-stub ...
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Renegar Glacier
Koettlitz Glacier is a large Antarctic glacier lying west of Mount Morning and Mount Discovery in the Royal Society Range, flowing from the vicinity of Mount Cocks northeastward between Brown Peninsula and the mainland into the ice shelf of McMurdo Sound. It was discovered by the British National Antarctic Expedition (1901–04) which named it for Dr. Reginald Koettlitz, physician and botanist of the expedition. See also * Bulwark Stream * 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. Th ... References Glaciers of Victoria Land Scott Coast {{ScottCoast-geo-stub ...
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Scott Coast
Scott Coast () is the portion of the coast of Victoria Land, Antarctica between Cape Washington and Minna Bluff. It was named by the New Zealand Antarctic Place-Names Committee in 1961 after Captain Robert Falcon Scott, Royal Navy, leader of the ''Discovery'' Expedition (1901–1904) and the British Antarctic Expedition (1910-1913), who died on the return journey from the South Pole. Much of the early exploration of this coastline was accomplished by Scott and his colleagues, and many of the names in the region were bestowed by him. See also * Blue Glacier Blue Glacier is a large glacier located to the north of Mount Olympus in the Olympic Mountains of Washington. The glacier covers an area of and contains of ice and snow in spite of its low terminus elevation. The glacier length has decreased ... * Dreschhoff Peak * Nostoc Flats * Robbins Hill * Stoner Peak * Thoreson Peak * Weidner Ridge * Mount Band External links Coasts of Victoria Land {{Scot ...
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Antarctica
Antarctica () is Earth's southernmost and least-populated continent. Situated almost entirely south of the Antarctic Circle and surrounded by the Southern Ocean, it contains the geographic South Pole. Antarctica is the fifth-largest continent, being about 40% larger than Europe, and has an area of . Most of Antarctica is covered by the Antarctic ice sheet, with an average thickness of . Antarctica is, on average, the coldest, driest, and windiest of the continents, and it has the highest average elevation. It is mainly a polar desert, with annual precipitation of over along the coast and far less inland. About 70% of the world's freshwater reserves are frozen in Antarctica, which, if melted, would raise global sea levels by almost . Antarctica holds the record for the lowest measured temperature on Earth, . The coastal regions can reach temperatures over in summer. Native species of animals include mites, nematodes, penguins, seals and tardigrades. Where vegetation o ...
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West Aisle Ridge
West Aisle Ridge () in Antarctica is a named from the position of the ridge in a group of three ridges in relation to The Stage ''The Stage'' is a British weekly newspaper and website covering the entertainment industry and particularly theatre. It was founded in 1880. It contains news, reviews, opinion, features, and recruitment advertising, mainly directed at those wh .... Ridges of Victoria Land Scott Coast {{ScottCoast-geo-stub ...
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Central Aisle Ridge
Central Aisle Ridge () is a north–south ridge immediately east of The Stage on the north side of lower Renegar Glacier, Scott Coast. The name is derived from the position of the ridge relative to West Aisle Ridge, East Aisle Ridge, and its proximity to The Stage. It was named by the New Zealand Geographic Board (1994) following work by a New Zealand Geological Survey GNS Science ( mi, Te Pū Ao), officially registered as the Institute of Geological and Nuclear Sciences Limited, is a New Zealand Crown Research Institute. It focuses on geology, geophysics (including seismology and volcanology), and nuclear sc ... party to the area, 1977–78. References * Ridges of Victoria Land Scott Coast {{ScottCoast-geo-stub ...
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East Aisle Ridge
East Aisle Ridge () is a north–south ridge east of Central Aisle Ridge at the junction of the lower Renegar Glacier and Koettlitz Glacier, Scott Coast, Antarctica. The name is derived from the position of the ridge relative to West Aisle Ridge, Central Aisle Ridge, and its proximity to The Stage ''The Stage'' is a British weekly newspaper and website covering the entertainment industry and particularly theatre. It was founded in 1880. It contains news, reviews, opinion, features, and recruitment advertising, mainly directed at those wh .... It was named by the New Zealand Geographic Board in 1994, following work by a New Zealand Geological Survey party to the area in 1977–78. . References Ridges of Victoria Land Scott Coast {{ScottCoast-geo-stub ...
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New Zealand Geological Survey
GNS Science ( mi, Te Pū Ao), officially registered as the Institute of Geological and Nuclear Sciences Limited, is a New Zealand Crown Research Institute. It focuses on geology, geophysics (including seismology and volcanology), and nuclear science (particularly ion-beam technologies, isotope science and carbon dating). GNS Science was known as the Institute of Geological and Nuclear Sciences (IGNS) from 1992 to 2005. Originally part of the New Zealand Government's Department of Scientific and Industrial Research (DSIR), it was established as an independent organisation when the Crown Research Institutes were set up in 1992.
Crown Research Institutes Act 1992.
As well as undertaking basic research, and operating the national geological hazards monitoring network (GeoNet)
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Ridges Of Victoria Land
A ridge or a mountain ridge is a geographical feature consisting of a chain of mountains or hills that form a continuous elevated crest for an extended distance. The sides of the ridge slope away from the narrow top on either side. The lines along the crest formed by the highest points, with the terrain dropping down on either side, are called the ridgelines. Ridges are usually termed hills or mountains as well, depending on size. Smaller ridges, especially those leaving a larger ridge, are often referred to as spurs. Types There are several main types of ridges: ;Dendritic ridge: In typical dissected plateau terrain, the stream drainage valleys will leave intervening ridges. These are by far the most common ridges. These ridges usually represent slightly more erosion resistant rock, but not always – they often remain because there were more joints where the valleys formed or other chance occurrences. This type of ridge is generally somewhat random in orientation, often ...
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