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Gjelsvik Peak
The Herbert Range is a mountain range in the Queen Maud Mountains of Antarctica, extending from the edge of the polar plateau to the Ross Ice Shelf between the Axel Heiberg and Strom glaciers. Named by the New Zealand Antarctic Place-Names Committee (NZ-APC) for Walter W. Herbert, leader of the Southern Party of the New Zealand GSAE (1961–62) which explored the Axel Heiberg Glacier area. Features Geographical features include: * Axel Heiberg Glacier * Bell Peak * Bigend Saddle * Cohen Glacier * Mount Balchen * Mount Betty * Mount Cohen * Sargent Glacier * Strom Glacier Strom Glacier () is a steep valley glacier flowing northeast from the north side of Mount Fridtjof Nansen to the head of the Ross Ice Shelf, flanked on the northwest by the Duncan Mountains and on the southeast by the Herbert Range. The glacier deri ... * Zigzag Bluff References * East Antarctica Queen Maud Mountains Amundsen Coast {{RossDependency-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountain Range
A mountain range or hill range is a series of mountains or hills arranged in a line and connected by high ground. A mountain system or mountain belt is a group of mountain ranges with similarity in form, structure, and alignment that have arisen from the same cause, usually an orogeny. Mountain ranges are formed by a variety of geological processes, but most of the significant ones on Earth are the result of plate tectonics. Mountain ranges are also found on many planetary mass objects in the Solar System and are likely a feature of most terrestrial planets. Mountain ranges are usually segmented by highlands or mountain passes and valleys. Individual mountains within the same mountain range do not necessarily have the same geologic structure or petrology. They may be a mix of different orogenic expressions and terranes, for example thrust sheets, uplifted blocks, fold mountains, and volcanic landforms resulting in a variety of rock types. Major ranges Most geolo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 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. Despite the name, they are not located within Queen Maud Land. 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. Featu ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Antarctic Plateau
The Antarctic Plateau, Polar Plateau or King Haakon VII Plateau is a large area of East Antarctica which extends over a diameter of about , and includes the region of the geographic South Pole and the Amundsen–Scott South Pole Station. This huge continental plateau is at an average elevation of about . Exploration This plateau was first sighted in 1903 during the ''Discovery'' Expedition to the Antarctic, which was led by Robert Falcon Scott. Ernest Shackleton became the first to cross parts of this plateau in 1909 during his ''Nimrod'' Expedition, which turned back in bad weather when it had reached a point just from the South Pole. Shackleton named this plateau the King Edward VII Plateau in honour of the king of the United Kingdom. In December 1911, while returning from the first journey to the South Pole, the Norwegian explorer Roald Amundsen decided to name this plateau the King Haakon VII Plateau in honour of the newly elected king of Norway. The Antarctic Plateau ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ross Ice Shelf
The Ross Ice Shelf is the largest ice shelf of Antarctica (, an area of roughly and about across: about the size of France). It is several hundred metres thick. The nearly vertical ice front to the open sea is more than long, and between high above the water surface. Ninety percent of the floating ice, however, is below the water surface. Most of Ross Ice Shelf is in the Ross Dependency claimed by New Zealand. It floats in, and covers, a large southern portion of the Ross Sea and the entire Roosevelt Island located in the east of the Ross Sea. The ice shelf is named after Sir James Clark Ross, who discovered it on 28 January 1841. It was originally called "The Barrier", with various adjectives including "Great Ice Barrier", as it prevented sailing further south. Ross mapped the ice front eastward to 160° W. In 1947, the U.S. Board on Geographic Names applied the name "Ross Shelf Ice" to this feature and published it in the original U.S. Antarctic Gazetteer. In Januar ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Axel Heiberg Glacier
The Axel Heiberg Glacier in Antarctica is a valley glacier, long, descending from the high elevations of the Antarctic Plateau into the Ross Ice Shelf (nearly at sea level) between the Herbert Range and Mount Don Pedro Christophersen in the Queen Maud Mountains. This huge glacier was discovered in November 1911 by the Norwegian polar explorer Roald Amundsen, and named by him for Axel Heiberg, a Norwegian businessman and patron of science who contributed to numerous Norwegian polar expeditions. Amundsen used this glacier as his route up onto the polar plateau during his successful expedition to the South Pole. Unlike the big “outlet” glaciers such as the Beardmore, Shackleton and Liv, the Axel Heiberg is in effect an alpine glacier, cut off from the Plateau by a dolerite rim and fed entirely from the uncharacteristically heavy snow falling within its own catchment. It falls over 2,700 m (9,000 ft) in 32 km (20 mi), most of it over 11 km (7 mi). See also * List of glaci ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Strom Glacier
Strom Glacier () is a steep valley glacier flowing northeast from the north side of Mount Fridtjof Nansen to the head of the Ross Ice Shelf, flanked on the northwest by the Duncan Mountains and on the southeast by the Herbert Range. The glacier derives its name from "Strom Camp" near its foot, occupied during December 1929 by the Byrd Antarctic Expedition geological party under Gould. Strom Camp was named by that party for Sverre Strom, first mate of the ship City of New York City, New York, who remained ashore as a member of the winter party and headed the snowmobile party which hauled supplies in support of the two field parties. Glaciers of Amundsen Coast {{RossDependency-glacier-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bell Peak
The Herbert Range is a mountain range in the Queen Maud Mountains of Antarctica, extending from the edge of the polar plateau to the Ross Ice Shelf between the Axel Heiberg and Strom glaciers. Named by the New Zealand Antarctic Place-Names Committee (NZ-APC) for Walter W. Herbert, leader of the Southern Party of the New Zealand GSAE (1961–62) which explored the Axel Heiberg Glacier area. Features Geographical features include: * Axel Heiberg Glacier * Bell Peak * Bigend Saddle * Cohen Glacier * Mount Balchen * Mount Betty * Mount Cohen * Sargent Glacier * Strom Glacier Strom Glacier () is a steep valley glacier flowing northeast from the north side of Mount Fridtjof Nansen to the head of the Ross Ice Shelf, flanked on the northwest by the Duncan Mountains and on the southeast by the Herbert Range. The glacier deri ... * Zigzag Bluff References * East Antarctica Queen Maud Mountains Amundsen Coast {{RossDependency-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bigend Saddle
The Herbert Range is a mountain range in the Queen Maud Mountains of Antarctica, extending from the edge of the polar plateau to the Ross Ice Shelf between the Axel Heiberg and Strom glaciers. Named by the New Zealand Antarctic Place-Names Committee (NZ-APC) for Walter W. Herbert, leader of the Southern Party of the New Zealand GSAE (1961–62) which explored the Axel Heiberg Glacier area. Features Geographical features include: * Axel Heiberg Glacier * Bell Peak * Bigend Saddle * Cohen Glacier * Mount Balchen * Mount Betty * Mount Cohen * Sargent Glacier * Strom Glacier Strom Glacier () is a steep valley glacier flowing northeast from the north side of Mount Fridtjof Nansen to the head of the Ross Ice Shelf, flanked on the northwest by the Duncan Mountains and on the southeast by the Herbert Range. The glacier deri ... * Zigzag Bluff References * East Antarctica Queen Maud Mountains Amundsen Coast {{RossDependency-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cohen Glacier
Strom Glacier () is a steep valley glacier flowing northeast from the north side of Mount Fridtjof Nansen to the head of the Ross Ice Shelf, flanked on the northwest by the Duncan Mountains and on the southeast by the Herbert Range. The glacier derives its name from " Strom Camp" near its foot, occupied during December 1929 by the Byrd Antarctic Expedition geological party under Gould. Strom Camp was named by that party for Sverre Strom, first mate of the ship City of New York New York most commonly refers to: * New York City, the most populous city in the United States, located in the state of New York * New York (state), a state in the northeastern United States New York may also refer to: Film and television * '' ..., who remained ashore as a member of the winter party and headed the snowmobile party which hauled supplies in support of the two field parties. Glaciers of Amundsen Coast {{RossDependency-glacier-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount Balchen
The Herbert Range is a mountain range in the Queen Maud Mountains of Antarctica, extending from the edge of the polar plateau to the Ross Ice Shelf between the Axel Heiberg and Strom glaciers. Named by the New Zealand Antarctic Place-Names Committee (NZ-APC) for Walter W. Herbert, leader of the Southern Party of the New Zealand GSAE (1961–62) which explored the Axel Heiberg Glacier area. Features Geographical features include: * Axel Heiberg Glacier * Bell Peak * Bigend Saddle * Cohen Glacier * Mount Balchen * Mount Betty * Mount Cohen * Sargent Glacier * Strom Glacier Strom Glacier () is a steep valley glacier flowing northeast from the north side of Mount Fridtjof Nansen to the head of the Ross Ice Shelf, flanked on the northwest by the Duncan Mountains and on the southeast by the Herbert Range. The glacier deri ... * Zigzag Bluff References * East Antarctica Queen Maud Mountains Amundsen Coast {{RossDependency-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount Betty
The Herbert Range is a mountain range in the Queen Maud Mountains of Antarctica, extending from the edge of the polar plateau to the Ross Ice Shelf between the Axel Heiberg and Strom glaciers. Named by the New Zealand Antarctic Place-Names Committee (NZ-APC) for Walter W. Herbert, leader of the Southern Party of the New Zealand GSAE (1961–62) which explored the Axel Heiberg Glacier area. Features Geographical features include: * Axel Heiberg Glacier * Bell Peak * Bigend Saddle * Cohen Glacier * Mount Balchen * Mount Betty * Mount Cohen * Sargent Glacier * Strom Glacier Strom Glacier () is a steep valley glacier flowing northeast from the north side of Mount Fridtjof Nansen to the head of the Ross Ice Shelf, flanked on the northwest by the Duncan Mountains and on the southeast by the Herbert Range. The glacier deri ... * Zigzag Bluff References * East Antarctica Queen Maud Mountains Amundsen Coast {{RossDependency-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
