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Mount Harkness
The Gothic Mountains () is a group of mountains, long, in the Queen Maud Mountains of Antarctica, located west of Watson Escarpment and bounded by Scott Glacier, Albanus Glacier, and Griffith Glacier. Exploration and naming The mountains were first visited in December 1934 by the Byrd Antarctic Expedition (ByrdAE) geological party led by Quin Blackburn. The name was proposed by Edmund Stump, leader of a United States Antarctic Research Program (USARP) - Arizona State University geological party which made investigations here in the 1980–81 season. The mountains are composed of granites which have weathered to produce a series of spires and peaks reminiscent of a Gothic cathedral. Location The western Gothic Mountains are just east of Scott Glacier, to the south of the point where the Albanus Glacier joins the Scott Glacier from the east. Peaks in the western section include, from west to east, Grizzly Peak, Mount Zanuck, Zanuck East Peak, Outlook Peak and Mount Danforth ...
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Mountain
A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited summit area, and is usually higher than a hill, typically rising at least above the surrounding land. A few mountains are inselberg, isolated summits, but most occur in mountain ranges. mountain formation, Mountains are formed through tectonic plate, tectonic forces, erosion, or volcanism, which act on time scales of up to tens of millions of years. Once mountain building ceases, mountains are slowly leveled through the action of weathering, through Slump (geology), slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce Alpine climate, colder climates than at sea level at similar latitude. These colder climates strongly affect the Montane ecosystems, ecosystems of mountains: different elevations hav ...
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Mountain Ranges Of Antarctica
A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited summit area, and is usually higher than a hill, typically rising at least above the surrounding land. A few mountains are isolated summits, but most occur in mountain ranges. Mountains are formed through tectonic forces, erosion, or volcanism, which act on time scales of up to tens of millions of years. Once mountain building ceases, mountains are slowly leveled through the action of weathering, through slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce colder climates than at sea level at similar latitude. These colder climates strongly affect the ecosystems of mountains: different elevations have different plants and animals. Because of the less hospitable terrain and climate, mountains te ...
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California Plateau
Watson Escarpment () is a major escarpment in the Queen Maud Mountains, trending northward along the east margin of Scott Glacier, then eastward to Reedy Glacier where it turns southward along the glacier's west side. Somewhat arcuate, the escarpment is nearly long, rises above sea level, and above the adjacent terrain. Discovery and naming The north-central part of the escarpment was observed from a vantage point on Supporting Party Mountain and was partially mapped in December 1929 by the Byrd Antarctic Expedition geological party under Laurence Gould. The escarpment was more closely observed in December 1934 by the Byrd Antarctic Expedition geological party under Quin Blackburn, and was named by Byrd for Thomas J. Watson, American business executive, a patron of this expedition. The escarpment and its related features was mapped in detail by United States Geological Survey (USGS) from surveys and United States Navy air photos, 1960–64. Topology The western end of the ...
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Darryl F
Darryl is a given name, a variant spelling of Darell. Variations of this name include: Daryl, Daryll, Darryll, and Darrel. People Darryl * Darryl Brown (West Indian cricketer) (born 1973) * Darryl Brown (South African cricketer) (born 1983) * Darryl Byrd (born 1960), American former football player * Darryl Cunningham (born 1960), English cartoonist (see also Daryl Cunningham below) * Darryl David (born 1971), a member of the Singapore Parliament * Darryl Dawkins (1957–2015), American National Basketball Association player * Darryl Dikarrna Brown, Australian didgeridoo master * Darryl Drake (1956–2019), American football coach and player * Darryl George (born 1993), Australian baseball player * Darryl Hamilton (1964–2015), American Major League Baseball player * Darryl Hardy (born 1968), American former National Football League player * Darryl Henley (born 1966), American former National Football League player convicted of drug trafficking and attempted mur ...
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Darryl F Zanuck And Oscar In Gentleman's Agreement Trailer
Darryl is a given name, a variant spelling of Darell. Variations of this name include: Daryl, Daryll, Darryll, and Darrel. People Darryl * Darryl Brown (West Indian cricketer) (born 1973) * Darryl Brown (South African cricketer) (born 1983) * Darryl Byrd (born 1960), American former football player * Darryl Cunningham (born 1960), English cartoonist (see also Daryl Cunningham below) * Darryl David (born 1971), a member of the Singapore Parliament * Darryl Dawkins (1957–2015), American National Basketball Association player * Darryl Dikarrna Brown, Australian didgeridoo master * Darryl Drake (1956–2019), American football coach and player * Darryl George (born 1993), Australian baseball player * Darryl Hamilton (1964–2015), American Major League Baseball player * Darryl Hardy (born 1968), American former National Football League player * Darryl Henley (born 1966), American former National Football League player convicted of drug trafficking and attempted murder * D ...
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Granite
Granite ( ) is a coarse-grained (phanerite, phaneritic) intrusive rock, intrusive igneous rock composed mostly of quartz, alkali feldspar, and plagioclase. It forms from magma with a high content of silica and alkali metal oxides that slowly cools and solidifies underground. It is common in the continental crust of Earth, where it is found in igneous intrusions. These range in size from dike (geology), dikes only a few centimeters across to batholiths exposed over hundreds of square kilometers. Granite is typical of a larger family of ''granitic rocks'', or ''granitoids'', that are composed mostly of coarse-grained quartz and feldspars in varying proportions. These rocks are classified by the relative percentages of quartz, alkali feldspar, and plagioclase (the QAPF diagram, QAPF classification), with true granite representing granitic rocks rich in quartz and alkali feldspar. Most granitic rocks also contain mica or amphibole minerals, though a few (known as leucogranites) conta ...
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Queen Maud Mountains
The Queen Maud Mountains () are a major group of mountains, ranges and subordinate features of the Transantarctic Mountains, lying between the Beardmore Glacier, Beardmore and Reedy Glaciers and including the area from the head of the Ross Ice Shelf to the Antarctic Plateau in Antarctica. Captain Roald Amundsen and his South Pole party ascended Axel Heiberg Glacier near the central part of this group in November 1911, naming these mountains for the Norwegian queen Maud of Wales. Exploration and naming Elevations bordering the Beardmore Glacier, at the western extremity of these mountains, were observed by the British expeditions led by Ernest Shackleton (1907–09) and Robert Falcon Scott (1910-13), but the mountains as a whole were mapped by several American expeditions led by Richard Evelyn Byrd (1930s and 1940s), and United States Antarctic Program (USARP) and New Zealand Antarctic Research Program (NZARP) expeditions from the 1950s through the 1970s. Appearance The ''Sailing ...
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Arizona State University
Arizona State University (Arizona State or ASU) is a public university, public research university in Tempe, Arizona, United States. Founded in 1885 as Territorial Normal School by the 13th Arizona Territorial Legislature, the university is one of the List of United States university campuses by enrollment, largest public universities by enrollment in the United States. It was one of about 180 "normal schools" founded in the late 19th century to train teachers for the rapidly growing public common schools. Some closed, but most steadily expanded their role and became state colleges in the early 20th century, then state universities in the late 20th century. One of three universities governed by the Arizona Board of Regents, Arizona State University is a member of the Association of American Universities (AAU) and is Carnegie Classification of Institutions of Higher Education, classified among "R1: Doctoral Universities – Very High Research Activity". ASU has over 183,000 st ...
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