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Charcot Land
Charcot Land is a peninsula of Eastern Greenland, part of the Scoresby Sound system. It lies in the Northeast Greenland National Park zone. The area is remote and uninhabited. It was named after French Polar explorer Jean-Baptiste Charcot (1867–1936) during aerial surveys by Lauge Koch as part of the Three-year Expedition to East Greenland. Geography Charcot Land is a mountainous region. It is bound to the south by the Daugaard-Jensen Glacier, beyond which lies Hinksland. To the north lies the F. Graae Glacier and to the east the head of the Nordvestfjord Nordvestfjord, meaning 'Northwest Fjord', ( kl, Kangertertivarmît Kangertivat) is a fjord in King Christian X Land, eastern Greenland. Administratively most of its length lies in the Northeast Greenland National Park area, at the border of Sermer ..., its easternmost point being a headland named Kap Ursus Major. To the west are a number of nunataks and the Greenland ice sheet. Bibliography *A. K. Higgins, Jane A. G ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Daugaard-Jensen Glacier
The Daugaard-Jensen Glacier is a large glacier located on the southeast coast of Greenland. The glacier was first mapped in 1933 by Lauge Koch during aerial surveys made during the 1931–34 Three-year Expedition to East Greenland ''(Treårsekspeditionen)''. It is named in honour of Niels Daugaard-Jensen, who was head of the Greenland department under the Danish Ministry of State and former governor ''(Landsfoged)'' of Northern Greenland. Geography Located in the northwestern side of Hinksland and south of Charcot Land, it drains an area of 50,150 km2 of the Greenland Ice Sheet with a flux (quantity of ice moved from the land to the sea) of 10.5 km3 per year, as measured for 1996. With its terminus in the Nordvestfjord of the Scoresby Sound, it is one of the main producers of icebergs to the north of Iceland. See also *List of glaciers in Greenland This is a list of glaciers in Greenland. Details on the size and flow of some of the major Greenlandic glaciers a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Nordvestfjord
Nordvestfjord, meaning 'Northwest Fjord', ( kl, Kangertertivarmît Kangertivat) is a fjord in King Christian X Land, eastern Greenland. Administratively most of its length lies in the Northeast Greenland National Park area, at the border of Sermersooq municipality. This fjord is part of the Scoresby Sound system. The distance from the head of Nordvestfjord across Hall Bredning to the mouth of Scoresby Sound is , which makes this continuous stretch of water the longest fjord in the world. History The Nordvestfjord fjord was named by Carl Ryder during his Ryder's East Greenland Expedition, 1891–92 expedition because of its approximate northwestern direction.''Catalogue of place names in northern East Greenland''. Geological Survey of Denmark. Ryder, however, was prevented from exploring it because it was already September, new ice was forming, and a very strong wind was blowing from the interior of the fjord. Geography This long and very deep fjord is the northernmost arm of the S ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
NE Greenland National Park
Northeast Greenland National Park ( kl, Kalaallit Nunaanni nuna eqqissisimatitaq, da, Grønlands Nationalpark) is the world's largest national park and the 10th largest protected area (the only larger protected areas all consist mostly of sea). Established in 1974 and expanded to its present size in 1988, it protects of the interior and northeastern coast of Greenland and is bigger than all but 29 of the world's 195 countries. It was the first national park to be created in the Kingdom of Denmark and remains Greenland's only national park. It is the northernmost national park in the world. It is the second largest by area of any second level subdivision of any country in the world trailing only the Qikiqtaaluk Region, Nunavut, Canada. Geography The park shares borders, largely laid out as straight lines, with the Sermersooq municipality in the south and with the Avannaata municipality in the west, partly along the 45° West meridian on the ice cap. The large interior of the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Peninsula
A peninsula (; ) is a landform that extends from a mainland and is surrounded by water on most, but not all of its borders. A peninsula is also sometimes defined as a piece of land bordered by water on three of its sides. Peninsulas exist on all continents. The size of a peninsula can range from tiny to very large. The largest peninsula in the world is the Arabian Peninsula. Peninsulas form due to a variety of causes. Etymology Peninsula derives , which is translated as 'peninsula'. itself was derived , or together, 'almost an island'. The word entered English in the 16th century. Definitions A peninsula is usually defined as a piece of land surrounded on most, but not all sides, but is sometimes instead defined as a piece of land bordered by water on three of its sides. A peninsula may be bordered by more than one body of water, and the body of water does not have to be an ocean or a sea. A piece of land on a very tight river bend or one between two rivers is sometimes s ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Greenland
Greenland ( kl, Kalaallit Nunaat, ; da, Grønland, ) is an island country in North America that is part of the Kingdom of Denmark. It is located between the Arctic and Atlantic oceans, east of the Canadian Arctic Archipelago. Greenland is the world's largest island. It is one of three constituent countries that form the Kingdom of Denmark, along with Denmark and the Faroe Islands; the citizens of these countries are all citizens of Denmark and the European Union. Greenland's capital is Nuuk. Though a part of the continent of North America, Greenland has been politically and culturally associated with Europe (specifically Norway and Denmark, the colonial powers) for more than a millennium, beginning in 986.The Fate of Greenland's Vikings , by Dale Mackenzie Brown, ''Archaeological Institute of America'', ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Scoresby Sound
Scoresby Sound (Danish: ''Scoresby Sund'', Greenlandic: ''Kangertittivaq'') is a large fjord system of the Greenland Sea on the eastern coast of Greenland. It has a tree-like structure, with a main body approximately Scoresby Sund Encyclopædia Britannica on-line long that branches into a system of s covering an area of about . The longest of the fjords extends 340–350 km (210-216 mi) inland from the coastline. The depth is 400–600 m (1,310-1,970 ft) in the main basin, but depths increase to up to in some fjords. It is one of the largest and longest fjord systems in the world.Archaeology, p. 7 On the northern side of the mouth of the Scoresb ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Northeast Greenland National Park
Northeast Greenland National Park ( kl, Kalaallit Nunaanni nuna eqqissisimatitaq, da, Grønlands Nationalpark) is the world's largest national park and the 10th List of largest protected areas in the world, largest protected area (the only larger protected areas all consist mostly of sea). Established in 1974 and expanded to its present size in 1988, it protects of the interior and northeastern coast of Greenland and is bigger than all but List of countries and outlying territories by total area, 29 of the world's 195 countries. It was the first List of national parks of Denmark, national park to be created in the Kingdom of Denmark and remains Greenland's only national park. It is the northernmost national park in the world. It is the second largest by area of any second level subdivision of any country in the world trailing only the Qikiqtaaluk Region, Qikiqtaaluk Region, Nunavut, Canada. Geography The park shares borders, largely laid out as Great Circle, straight lines, with ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lauge Koch
Lauge Koch (5 July 1892 – 5 June 1964) was a Danish geologist and Arctic explorer. Biography Lauge Koch was born in 1892 to Karl and Elisabeth Koch. His development as a scientist was greatly influenced by his father's second cousin Johan Peter Koch - a polar explorer, a member of several Greenland expeditions, including Ludvig Mylius-Erichsen's and Alfred Wegener's (in the latter's expedition (1912-1913) to cross Greenland, he led a sledging party). He received his higher education at the University of Copenhagen, where he began his studies in 1911, in 1920 he received a master's degree, and in 1929 a doctor's degree, having defended a dissertation on the topic "Stratigraphy of Greenland". General He was the renowned leader of 24 Danish government expeditions to Greenland, and the central character in the ''Lauge Koch Controversy'', an international and intra-national conflict. Beginning in December 1935 a bitter conflict arose between Koch and eleven of the most prominent Da ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Three-year Expedition To East Greenland
The Three-year Expedition ( da, Treårsekspeditionen) was an exploratory expedition to East Greenland that lasted from 1931 to 1934 financed by the Carlsberg Foundation and the Danish state. The expedition included aerial surveys. Many geographic features in East Greenland were mapped and named during the expedition. Eskimonaes station was used as a wintering base by the Three-year Expedition to East Greenland. History The expedition was led by Lauge Koch. The other participants were Danish and Swedish geographers, geologists, archaeologists, zoologists and botanists: Paul Gelting, Gunnar Seidenfaden, Thorvald Sørensen, Steen Hasselbach, Helge G. Backlund, Gunnar Thorson, Gunnar Säve-Söderbergh, Helge Larsen, Thyge Johansen, L. Bruhn, H. Heinrich Nielsen and N. V. Petersen. The expedition vessels were ''Godthaab'' and ''Gustav Holm''.Koch, Lauge (1933) The Danish Three-Year Expedition to King Christian X Land. Geographical Review 23 (4): 599-607Full text/ref> The engage ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountainous
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 (topography), 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 Monadnock, 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, ecosys ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hinksland
Hinksland ( da, Hinksland) is a peninsula in eastern Greenland. It is a part of the Northeast Greenland National Park. The peninsula is named after Arthur R. Hinks, Secretary of the Royal Geographical Society, 1915–45. Geography Hinksland is limited to the northwest by the Daugaard-Jensen Glacier, beyond which lies Charcot Land, to the northeast by the Nordvestfjord of the Scoresby Sound and to the south by the Flyver Fjord. To the southwest the peninsula is attached to the mainland. The Renland peninsula lies to the southeast, beyond Th. Sørensen Land and Nathorst Land to the north, across the Nordvestfjord. The highest point of the peninsula is a mountain located in the southern part rising above the Flyver Fjord. Geologically Hinksland is part of the Vestfjord-Hinksland gneiss and schist zone crystalline complex.Harold Williams ed. ''Geology of the Appalachian—Caledonian Orogen in Canada and Greenland'', p. 898 Hinksland is at the southern limit of the eastern coasta ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
