Mount Rouge
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Mount Rouge
Mount Rouge () is a prominent mountain between Funk and Cadman Glaciers at the head of Beascochea Bay, on the west side of Graham Land on the Antarctic Peninsula. Discovered and named ''Massif Rouge'' (red mountain) by the French Antarctic Expedition, 1908–10, led by Jean-Baptiste Charcot Jean-Baptiste-Étienne-Auguste Charcot (15 July 1867 – 16 September 1936), born in Neuilly-sur-Seine, was a French scientist, medical doctor and polar scientist. His father was the neurologist Jean-Martin Charcot (1825–1893). Life Jean-Ba .... References Mountains of Graham Land Graham Coast {{GrahamCoast-geo-stub ...
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Funk Glacier
Funk Glacier () is a glacier flowing into the head of Nevsha Cove in Beascochea Bay to the south of Frölich Peak, on the west coast of Graham Land, Antarctica. It was first charted by the French Antarctic Expedition, 1908–10, under Jean-Baptiste Charcot. It was named by the UK Antarctic Place-Names Committee in 1959 for Casimir Funk, an American (formerly Polish) biochemist who, while working at the Lister Institute The Lister Institute of Preventive Medicine, informally known as the Lister Institute, was established as a research institute (the British Institute of Preventive Medicine) in 1891, with bacteriologist Marc Armand Ruffer as its first director, us ... in London in 1912, originated the theory of vitamins. References Poland and the Antarctic Glaciers of Graham Coast {{GrahamCoast-glacier-stub ...
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Cadman Glacier
Cadman Glacier () is a glacier, wide at its mouth and about long, flowing northwestward into the head of the southern arm of Beascochea Bay south of Plas Point on the west side of the Antarctic Peninsula. History The glacier was discovered and roughly surveyed in 1909 by the French Antarctic Expedition under Jean-Baptiste Charcot. It was surveyed in 1935 by the British Graham Land Expedition (BGLE), led by John Rymill, and later named for John Cadman, 1st Baron Cadman of Silverdale, who contributed toward the cost of the BGLE, 1934–37. 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, climato ... References * Glaciers of Graham Coast {{GrahamCoast-glacier-stub ...
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Beascochea Bay
Beascochea Bay () is a bay, long and wide, indenting the Graham Coast of Graham Land, Antarctica, between Kyiv Peninsula and Barison Peninsula, and entered south of Cape Perez. The glaciers Lever, Funk, Cadman, Talev and Butamya feed the bay. It was discovered but incompletely defined by the Belgian Antarctic Expedition, 1897–99; was resighted by the French Antarctic Expedition, 1903–05, and named by Jean-Baptiste Charcot for Commander Beascochea, Argentine Navy. The bay was then more accurately charted by the British Graham Land Expedition, 1934–37. Maps Antarctic Digital Database (ADD).Scale 1:250000 topographic map of Antarctica. Scientific Committee on Antarctic Research (SCAR). Since 1993, regularly upgraded and updated. See also *Bachstrom Point Bachstrom Point () is a headland on the northeast side of Beascochea Bay, southeast of Cape Perez on the southwest coast of Kyiv Peninsula in Graham Land, Antarctica. It was first charted by the British Graham Land E ...
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Graham Land
Graham Land is the portion of the Antarctic Peninsula that lies north of a line joining Cape Jeremy and Cape Agassiz. This description of Graham Land is consistent with the 1964 agreement between the British Antarctic Place-names Committee and the US Advisory Committee on Antarctic Names, in which the name "Antarctic Peninsula" was approved for the major peninsula of Antarctica, and the names Graham Land and Palmer Land for the northern and southern portions, respectively. The line dividing them is roughly 69 degrees south. Graham Land is named after Sir James R. G. Graham, First Lord of the Admiralty at the time of John Biscoe's exploration of the west side of Graham Land in 1832. It is claimed by Argentina (as part of Argentine Antarctica), Britain (as part of the British Antarctic Territory) and Chile (as part of the Chilean Antarctic Territory). Graham Land is the closest part of Antarctica to South America. Thus it is the usual destination for small ships taking paying ...
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Antarctic Peninsula
The Antarctic Peninsula, known as O'Higgins Land in Chile and Tierra de San Martín in Argentina, and originally as Graham Land in the United Kingdom and the Palmer Peninsula in the United States, is the northernmost part of mainland Antarctica. The Antarctic Peninsula is part of the larger peninsula of West Antarctica, protruding from a line between Cape Adams (Weddell Sea) and a point on the mainland south of the Eklund Islands. Beneath the ice sheet that covers it, the Antarctic Peninsula consists of a string of bedrock islands; these are separated by deep channels whose bottoms lie at depths considerably below current sea level. They are joined by a grounded ice sheet. Tierra del Fuego, the southernmost tip of South America, is about away across the Drake Passage. The Antarctic Peninsula is in area and 80% ice-covered. The marine ecosystem around the western continental shelf of the Antarctic Peninsula (WAP) has been subjected to rapid climate change. Over the past 50 ...
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French Antarctic Expedition
The French Antarctic Expedition is any of several French expeditions in Antarctica. First expedition In 1772, Yves-Joseph de Kerguelen-Trémarec and the naturalist Jean Guillaume Bruguière sailed to the Antarctic region in search of the fabled Terra Australis. Kerguelen-Trémarec took possession of various Antarctic territories for France, including what would later be called the Kerguelen Islands. In Kerguelen-Trémarec's report to King Louis XV, he greatly overestimated the value of the Kerguelen Islands. The King sent him on a second expedition to Kerguelen in late 1773. When it became clear that these islands were desolate, useless, and not the Terra Australis, he was sent to prison. Second expedition In 1837, during an 1837–1840 expedition across the deep southern hemisphere, Captain Jules Dumont d'Urville sailed his ship ''Astrolabe'' along a coastal area of Antarctica which he later named Adélie Land, in honor of his wife. During the Antarctic part of this expedi ...
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Jean-Baptiste Charcot
Jean-Baptiste-Étienne-Auguste Charcot (15 July 1867 – 16 September 1936), born in Neuilly-sur-Seine, was a French scientist, medical doctor and polar scientist. His father was the neurologist Jean-Martin Charcot (1825–1893). Life Jean-Baptiste Charcot was appointed leader of the French Antarctic Expedition with the ship ''Français'' exploring the west coast of Graham Land from 1904 until 1907. The expedition reached Adelaide Island in 1905 and took pictures of the Palmer Archipelago and Loubet Coast. From 1908 until 1910, another expedition followed with the ship '' Pourquoi Pas ?'', exploring the Bellingshausen Sea and the Amundsen Sea and discovering Loubet Land, Marguerite Bay, Mount Boland and Charcot Island, which was named after his father, Jean-Martin Charcot. anhere./ref> He named Hugo Island after Victor Hugo, the grandfather of his wife, Jeanne Hugo. Later on, Jean-Baptiste Charcot explored Rockall in 1921 and Eastern Greenland and Svalbard from 1925 until 1 ...
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Mountains Of Graham Land
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 300 metres (1,000 feet) 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 ...
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