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Ward Valley
Ward Valley () is an ice-free valley that lies between Porter Hills and Xanadu Hills and east of the snout of Ward Glacier in the Denton Hills, Scott Coast, 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 contine .... Named by US-ACAN (1994) in association with Ward Glacier and Ward Lake. References Valleys of Victoria Land Scott Coast {{ScottCoast-geo-stub ...
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Porter Hills
Porter Hills () is a set of hills in Antarctica named after Raymond C. Porter, Electronics Technician, USCG, a crewman of USCGC Glacier, who was killed in an offloading accident at McMurdo Station McMurdo Station is a United States Antarctic research station on the south tip of Ross Island, which is in the New Zealand-claimed Ross Dependency on the shore of McMurdo Sound in Antarctica. It is operated by the United States through the Unit ... on February 8, 1979. Hills of Victoria Land Scott Coast {{ScottCoast-geo-stub ...
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Xanadu Hills
Xanadu Hills () are a ridge of hills lying between Ward Valley and the Alph River in Victoria Land, a region of Antarctica. They were named by the New Zealand Geographic Board in 1994 in connection with the adjacent Alph River, an earlier name inspired by a poem of Samuel Taylor Coleridge, ''Kubla Khan ''Kubla Khan'' () is a poem written by Samuel Taylor Coleridge, completed in 1797 and published in 1816. It is sometimes given the subtitles "A Vision in a Dream" and "A Fragment." According to Coleridge's preface to ''Kubla Khan'', the poem ...''. References Hills of Victoria Land Scott Coast {{ScottCoast-geo-stub ...
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Ward Glacier
Ward Glacier () is a small glacier between Terminus Mountain and Howchin Glacier on the east side of the Royal Society Range in Victoria Land Victoria Land is a region in eastern Antarctica which fronts the western side of the Ross Sea and the Ross Ice Shelf, extending southward from about 70°30'S to 78°00'S, and westward from the Ross Sea to the edge of the Antarctic Plateau. It .... Named by Taylor of the British Antarctic Expedition (1910–13) for L. Ward, a Tasmanian geologist. Glaciers of Scott Coast {{ScottCoast-glacier-stub ...
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Denton Hills
The Denton Hills () are a group of rugged foothills, 24 nautical miles (44 km) long southwest–northeast and 9 nautical miles (17 km) wide, to the east of the Royal Society Range on the Scott Coast, Victoria Land. The feature comprises a series of eastward-trending ridges and valleys circumscribed by Howchin Glacier, Armitage Saddle, Blue Glacier (Antarctica), Blue Glacier, the coast, and Walcott Bay. The highest summits, Mount Kowalczyk at , and Goat Mountain (Antarctica), Goat Mountain at , rise from Hobbs Ridge in the northern part of the foothills. Elevations decrease southward as in Kahiwi Maihao Ridge, high near the center of the group and the Xanadu Hills, high at the southern end. The principal glaciers (Hobbs Glacier (Victoria Land), Hobbs, Blackwelder Glacier, Blackwelder, Salmon Glacier (Antarctica), Salmon, Garwood Glacier, Garwood, Joyce Glacier, Joyce, Rivard Glacier, Rivard, Miers Glacier, Miers, Adams Glacier (Victoria Land), Adams, Ward Glacier, Ward) fl ...
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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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Ward Lake (Antarctica)
Ward Lake () is a small lake, formed at the snout of the Ward Glacier, on the east side of the Royal Society Range in Victoria Land. Named by the Terra Nova Expedition The ''Terra Nova'' Expedition, officially the British Antarctic Expedition, was an expedition to Antarctica which took place between 1910 and 1913. Led by Captain Robert Falcon Scott, the expedition had various scientific and geographical objec ... (1910–13) after Ward Glacier. References Royal Society Range Lakes of Victoria Land Scott Coast {{ScottCoast-geo-stub ...
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Valleys Of Victoria Land
A valley is an elongated low area often running between hills or mountains, which will typically contain a river or stream running from one end to the other. Most valleys are formed by erosion of the land surface by rivers or streams over a very long period. Some valleys are formed through erosion by glacial ice. These glaciers may remain present in valleys in high mountains or polar areas. At lower latitudes and altitudes, these glacially formed valleys may have been created or enlarged during ice ages but now are ice-free and occupied by streams or rivers. In desert areas, valleys may be entirely dry or carry a watercourse only rarely. In areas of limestone bedrock, dry valleys may also result from drainage now taking place underground rather than at the surface. Rift valleys arise principally from earth movements, rather than erosion. Many different types of valleys are described by geographers, using terms that may be global in use or else applied only locally. For ...
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