Furdesanden Moraine
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Furdesanden Moraine
Furdesanden Moraine () is a moraine extending in a north–south direction for along the west side of the Conrad Mountains in the Orvin Mountains The Orvin Mountains ( no, Orvinfjella) constitute a major group of mountain ranges, extending for about between the Wohlthat Mountains and the Mühlig-Hofmann Mountains in Queen Maud Land. With its summit at , the massive Sandeggtind Peak forms ... of Queen Maud Land, Antarctica. It was discovered and photographed by the Third German Antarctic Expedition, 1938–39. It was mapped by Norway from air photos and surveys by the Sixth Norwegian Antarctic Expedition, 1956–60, and named Furdesanden (the furrow of sand). References Moraines of Queen Maud Land Princess Astrid Coast {{PrincessAstridCoast-geo-stub ...
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Moraine
A moraine is any accumulation of unconsolidated debris (regolith and rock), sometimes referred to as glacial till, that occurs in both currently and formerly glaciated regions, and that has been previously carried along by a glacier or ice sheet. It may consist of partly rounded particles ranging in size from boulders (in which case it is often referred to as boulder clay) down to gravel and sand, in a groundmass of finely-divided clayey material sometimes called glacial flour. Lateral moraines are those formed at the side of the ice flow, and terminal moraines were formed at the foot, marking the maximum advance of the glacier. Other types of moraine include ground moraines (till-covered areas forming sheets on flat or irregular topography) and medial moraines (moraines formed where two glaciers meet). Etymology The word ''moraine'' is borrowed from French , which in turn is derived from the Savoyard Italian ("mound of earth"). ''Morena'' in this case was derived from Provenà ...
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Conrad Mountains
The Conrad Mountains (german: Conradgebirge, no, Conradfjella) are a narrow chain of mountains, long, located between the Gagarin Mountains and Mount Dallmann in Queen Maud Land, Antarctica. The Conrad Mountains are a mountain range, subrange of the Orvin Mountains. With its Summit (topography), summit at , the massive Sandeggtind Peak forms the highest point in the Conrad Mountains. Discovery and naming The Conrad Mountains were discovered by the Third German Antarctic Expedition (1938–1939), led by Captain Alfred Ritscher, and named for Rear Admiral Heinrich Friedrich (Fritz) Conrad (18 April 1883 – 1 January 1944), director of the meteorological division of the former Marineleitung (German Admiralty). They were surveyed by the Sixth Norwegian Antarctic Expedition, 1956-1960. See also * Henry Moraine * List of mountains of Queen Maud Land References External links Scientific Committee on Antarctic Research (SCAR)
{{Antarctica topics Mountain ranges of Queen Maud La ...
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Orvin Mountains
The Orvin Mountains ( no, Orvinfjella) constitute a major group of mountain ranges, extending for about between the Wohlthat Mountains and the Mühlig-Hofmann Mountains in Queen Maud Land. With its summit at , the massive Sandeggtind Peak forms the highest point in the Conrad Mountains, a subrange of the Orvin Mountains. Discovery and naming First photographed from the air and roughly plotted by the Third German Antarctic Expedition (1938-1939), led by Capt. Alfred Ritscher. Mapped by Norwegian cartographers from surveys and air photos by the Sixth Norwegian Antarctic Expedition (1956–60) and named for Anders K. Orvin, director of the Norwegian Polar Institute from 1958 to 1959. Constituent ranges Constituent ranges of Orvin Mountains, listed from east to west: * Shcherbakov Range * Mount Dallmann * Conrad Mountains * Gagarin Mountains * Kurze Mountains * Drygalski Mountains * Filchner Mountains See also * List of mountains of Queen Maud Land This list of mountain ...
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Queen Maud Land
Queen Maud Land ( no, Dronning Maud Land) is a roughly region of Antarctica claimed by Norway as a dependent territory. It borders the claimed British Antarctic Territory 20° west and the Australian Antarctic Territory 45° east. In addition, a small unclaimed area from 1939 was annexed in June 2015. Positioned in East Antarctica, it makes out about one-fifth of the continent, and is named after the Norwegian queen Maud of Wales (1869–1938). In 1930, the Norwegian Hjalmar Riiser-Larsen was the first person known to have set foot in the territory. On 14 January 1939, the territory was claimed by Norway. On 23 June 1961, Queen Maud Land became part of the Antarctic Treaty System, making it a demilitarised zone. It is one of two Antarctic claims made by Norway, the other being Peter I Island. They are administered by the Polar Affairs Department of the Norwegian Ministry of Justice and Public Security in Oslo. Most of the territory is covered by the east Antarctic ic ...
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Third German Antarctic Expedition
New Swabia (Norwegian and german: Neuschwabenland) was a disputed Antarctic claim by Nazi Germany within the Norwegian territorial claim of Queen Maud Land and is now a cartographic name sometimes given to an area of Antarctica between 20°E and 10°W in Queen Maud Land. New Swabia was explored by Germany in early 1939 and named after that expedition's ship, , itself named after the German region of Swabia.McGonigal, David, Antarctica', frances lincoln ltd, 2009, , p. 367 Background Like many other countries, Germany sent expeditions to the Antarctic region in the late 19th and early 20th centuries, most of which were scientific. The late 19th century expeditions to the Southern Ocean, South Georgia, the Kerguelen Islands, and the Crozet Islands were astronomical, meteorological, and hydrological, mostly in close collaboration with scientific teams from other countries. As the 19th century ended, Germany began to focus on Antarctica. The first German expedition to Antarctica ...
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Sixth Norwegian Antarctic Expedition
The sixth Norwegian Antarctic Expedition (''Den norske antarktisekspedisjonen'') was a scientific expedition to Queen Maud Land in Antarctica. The expedition was based at Norway Station () which was located on the Fimbul Ice Shelf bordering the coast of Queen Maud Land. The expedition carried out survey work and scientific studies over a period of three-four years (1956–1960). The expedition was intended as part of Norway's participation in the International Geophysical Year, 1957-58. The crew set sail from Oslo on board two whaling ships, the ''Polarsirkel'' and ''Polarbjørn'', on 10 November 1956. The expedition was led by Sigurd Gunnarson Helle, a geodesist at Norsk Polarinstitutt. It included a total crew of fourteen researchers which was reduced to nine during the third year. Among their activities were topological mapping of the region. In 1960, King Olav V of Norway instituted the Antarctic Medal The Antarctic Medal is a civil decoration of Norway. Established by ...
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Moraines Of Queen Maud Land
A moraine is any accumulation of unconsolidated debris (regolith and rock), sometimes referred to as glacial till, that occurs in both currently and formerly glaciated regions, and that has been previously carried along by a glacier or ice sheet. It may consist of partly rounded particles ranging in size from boulders (in which case it is often referred to as boulder clay) down to gravel and sand, in a groundmass of finely-divided clayey material sometimes called glacial flour. Lateral moraines are those formed at the side of the ice flow, and terminal moraines were formed at the foot, marking the maximum advance of the glacier. Other types of moraine include ground moraines (till-covered areas forming sheets on flat or irregular topography) and medial moraines (moraines formed where two glaciers meet). Etymology The word ''moraine'' is borrowed from French , which in turn is derived from the Savoyard Italian ("mound of earth"). ''Morena'' in this case was derived from Provenà ...
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