Vahsel Bay
Vahsel Bay (german: Vahselbucht) is a bay about 7 miles wide in the western part of the Luitpold Coast, Antarctica. This bay receives the flow of the Schweitzer Glacier and Lerchenfeld Glacier. It was discovered by the German Antarctic Expedition of 1911–1912, led by Wilhelm Filchner. Upon discovery Filchner named the bay for Captain Richard Vahsel of the expedition ship ''Deutschland'', who died during the course of the expedition, reputedly of Syphilis. Filchner later renamed the bay ''Herzog Ernst Bucht'' after large portions of the surrounding ice broke away forming a much larger bay, but later explorers have retained the name Vahsel Bay. Vahsel Bay was the intended destination of Ernest Shackleton and the crew of the Imperial Trans-Antarctic Expedition. They made it all the way through the Weddell Sea The Weddell Sea is part of the Southern Ocean and contains the Weddell Gyre. Its land boundaries are defined by the bay formed from the coasts of Coats Land and t ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Luitpold Coast
Luitpold Coast (german: Prinzregent-Luitpold-Land) is that portion of the coast of Coats Land extending from the vicinity of Hayes Glacier, at 27°54′W, to 36°W, which is regarded as the eastern limit of the Filchner Ice Shelf. It was discovered by Wilhelm Filchner, leader of the Second German Antarctic Expedition, 1911–12, and named after Luitpold, Prince Regent of Bavaria. Important Bird Area A 500 ha site on fast ice some 50 km north-east of the Filchner Ice Shelf, where icebergs regularly calve from the continental margin, has also been designated an Important Bird Area (IBA) by BirdLife International because it supports a breeding colony of about 6,500 emperor penguins, an estimate based on 2009 satellite imagery. Virgen de las Nieves Refuge Virgen de las Nieves Refuge () is an Argentine Antarctic refuge located on the Filchner-Ronne Ice Shelf on the Luitpold Coast 150 kilometres south of the Belgrano I Base. The refuge is administered by the A ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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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 ve ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Schweitzer Glacier
Schweitzer Glacier (german: Schweitzergeletscher, ) is a glacier which drains west along the north side of Littlewood Nunataks into Vahsel Bay. The Lerchenfeld Glacier, trending west-northwestward, coalesces with the lower portion of this glacier. Discovered by the German Antarctic Expedition, 1911–12, under Wilhelm Filchner. He named it for Major Schweitzer, first president of the German Antarctic Expedition Society. 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 ... References * Glaciers of Coats Land {{CoatsLand-glacier-stub ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Lerchenfeld Glacier
Lerchenfeld Glacier (german: Lerchenfeldgletscher, ) is a glacier flowing in a west-northwesterly direction between Bertrab Nunatak and the Littlewood Nunataks in Antarctica. It coalesces with the southern flank of Schweitzer Glacier before the combined flow discharges into the head of Vahsel Bay. The glacier was discovered by the Second German Antarctic Expedition, 1911–12, under Wilhelm Filchner, who named this feature for Count Hugo von und zu Lerchenfeld-Köfering, a supporter of the expedition. 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 ... References * Glaciers of Coats Land {{CoatsLand-glacier-stub ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Wilhelm Filchner
Wilhelm Filchner (13 September 1877 – 7 May 1957) was a German army officer, scientist and explorer. He conducted several surveys and scientific investigations in China, Tibet and surrounding regions, and led the Second German Antarctic Expedition, 1911–13. As a young military officer, Filchner gained an early reputation for dash and daring, following his travel exploits in Russia and the Pamir Mountains range. After further technical studies, he developed expertise in geography and geophysics, before leading a major scientific survey in Tibet and western China in 1903–05. In 1909 he was appointed to organise and lead the forthcoming German expedition to the Antarctic, with both scientific and geographical objectives involving extensive exploration of the continent's interior. During the expedition his ship became trapped in the Weddell Sea ice, drifting for eight months and preventing Filchner from establishing a land base, thus failing in its main objective. Although import ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Richard Vahsel
Richard Vahsel (9 February 1868 – 8 August 1912) was a German naval officer who served as second officer on the Antarctic ''Gauss'' expedition, under command of Erich von Drygalski. In 1911, Vahsel was controversially appointed as captain of the ''Deutschland'', on Wilhelm Filchner's Second German Antarctic Expedition, 1911–1913. Vahsel and Filchner proved incompatible, and the failure of their relationship fatally undermined the chances of the expedition's success. Vahsel died during the expedition, of heart failure likely aggravated by the effects of syphilis, as ''Deutschland'' was drifting while trapped in the ice in the Weddell Sea. He was buried in the ice on 10 August 1912, as the ship drifted across the Antarctic Circle. Vahsel Bay, at the southern extreme of the Weddell Sea, is named after him, as are the Vahsel Glacier on Heard Island, discovered during Drygalski's expedition, and Cape Vahsel on the south-eastern coast of South Georgia South Georg ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Ernest Shackleton
Sir Ernest Henry Shackleton (15 February 1874 – 5 January 1922) was an Anglo-Irish Antarctic explorer who led three British expeditions to the Antarctic. He was one of the principal figures of the period known as the Heroic Age of Antarctic Exploration. Born in Kilkea, County Kildare, Ireland, Shackleton and his Anglo-Irish family moved to Sydenham in suburban south London when he was ten. Shackleton's first experience of the polar regions was as third officer on Captain Robert Falcon Scott's ''Discovery'' expedition of 1901–1904, from which he was sent home early on health grounds, after he and his companions Scott and Edward Adrian Wilson set a new southern record by marching to latitude 82°S. During the ''Nimrod'' expedition of 1907–1909, he and three companions established a new record Farthest South latitude at 88°S, only 97 geographical miles (112 statute miles or 180 kilometres) from the South Pole, the largest advance to the pole ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Imperial Trans-Antarctic Expedition
The Imperial Trans-Antarctic Expedition of 1914–1917 is considered to be the last major expedition of the Heroic Age of Antarctic Exploration. Conceived by Ernest Shackleton, Sir Ernest Shackleton, the expedition was an attempt to make the first land crossing of the Antarctic continent. After Roald Amundsen's Amundsen's South Pole expedition, South Pole expedition in 1911, this crossing remained, in Shackleton's words, the "one great main object of Antarctic journeyings". Shackleton's expedition failed to accomplish this objective, but became recognized instead as an epic feat of endurance. Shackleton had served in the Antarctic on the Discovery Expedition, ''Discovery'' expedition of 1901–1904, and had led the Nimrod Expedition, ''Nimrod'' expedition of 1907–1909. In this new venture he proposed to sail to the Weddell Sea and to land a shore party near Vahsel Bay, in preparation for a transcontinental march via the South Pole to the Ross Sea. A supporting group, the Ros ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Weddell Sea
The Weddell Sea is part of the Southern Ocean and contains the Weddell Gyre. Its land boundaries are defined by the bay formed from the coasts of Coats Land and the Antarctic Peninsula. The easternmost point is Cape Norvegia at Princess Martha Coast, Queen Maud Land. To the east of Cape Norvegia is the King Haakon VII Sea. Much of the southern part of the sea is covered by a permanent, massive ice shelf field, the Filchner-Ronne Ice Shelf. The sea is contained within the two overlapping Antarctic territorial claims of Argentine Antarctica, the British Antarctic Territory, and also resides partially within the Antarctic Chilean Territory. At its widest the sea is around across, and its area is around . Various ice shelves, including the Filchner-Ronne Ice Shelf, fringe the Weddell sea. Some of the ice shelves on the east side of the Antarctic Peninsula, which formerly covered roughly of the Weddell Sea, had completely disappeared by 2002. The Weddell Sea has been d ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Vahsel Bay
Vahsel Bay (german: Vahselbucht) is a bay about 7 miles wide in the western part of the Luitpold Coast, Antarctica. This bay receives the flow of the Schweitzer Glacier and Lerchenfeld Glacier. It was discovered by the German Antarctic Expedition of 1911–1912, led by Wilhelm Filchner. Upon discovery Filchner named the bay for Captain Richard Vahsel of the expedition ship ''Deutschland'', who died during the course of the expedition, reputedly of Syphilis. Filchner later renamed the bay ''Herzog Ernst Bucht'' after large portions of the surrounding ice broke away forming a much larger bay, but later explorers have retained the name Vahsel Bay. Vahsel Bay was the intended destination of Ernest Shackleton and the crew of the Imperial Trans-Antarctic Expedition. They made it all the way through the Weddell Sea The Weddell Sea is part of the Southern Ocean and contains the Weddell Gyre. Its land boundaries are defined by the bay formed from the coasts of Coats Land and t ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Bays Of Antarctica
A bay is a recessed, coastal body of water that directly connects to a larger main body of water, such as an ocean, a lake, or another bay. A large bay is usually called a gulf, sea, sound, or bight. A cove is a small, circular bay with a narrow entrance. A fjord is an elongated bay formed by glacial action. A bay can be the estuary of a river, such as the Chesapeake Bay, an estuary of the Susquehanna River. Bays may also be nested within each other; for example, James Bay is an arm of Hudson Bay in northeastern Canada. Some large bays, such as the Bay of Bengal and Hudson Bay, have varied marine geology. The land surrounding a bay often reduces the strength of winds and blocks waves. Bays may have as wide a variety of shoreline characteristics as other shorelines. In some cases, bays have beaches, which "are usually characterized by a steep upper foreshore with a broad, flat fronting terrace".Maurice Schwartz, ''Encyclopedia of Coastal Science'' (2006), p. 129. Bays were ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |