Mount Dallmann
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Mount Dallmann
Mount Dallmann is a bold mountain, high, east of the northern portion of the Conrad Mountains, in the Orvin Mountains of Queen Maud Land, Antarctica. It was discovered by the Third German Antarctic Expedition (1938–1939), led by Captain Alfred Ritscher, and named for Eduard Dallmann, a German whaling captain who explored along the west coast of the Antarctic Peninsula in 1873–1874. Dallmann was the first person to navigate under the German flag in Antarctic waters. See also * List of mountains of Queen Maud Land This list of mountains of Queen Maud Land contains mountains with a registered elevation of higher than 2000 metres (6561 feet) above sea level. The availability of accurate data for this region is limited, making the list both incomplete and inac ... * Slabotnen Cirque References External links Scientific Committee on Antarctic Research (SCAR)* {{DEFAULTSORT:Dallmann, Mount Mountains of Queen Maud Land Orvin Mountains ...
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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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East Antarctica
East Antarctica, also called Greater Antarctica, constitutes the majority (two-thirds) of the Antarctic continent, lying on the Indian Ocean side of the continent, separated from West Antarctica by the Transantarctic Mountains. It lies almost entirely within the Eastern Hemisphere and its name has been accepted for more than a century. It is generally higher than West Antarctica and includes the Gamburtsev Mountain Range in the center. The geographic South Pole is located within East Antarctica. Apart from small areas of the coast, East Antarctica is permanently covered by ice and it has relatively low biodiversity, with only a small number of species of terrestrial plants, animals, algae, and lichens. The coasts are the breeding ground for various seabirds and penguins, and the leopard seal, Weddell seal, elephant seal, crabeater seal and Ross seal breed on the surrounding pack ice in summer. Location and description Almost completely covered in thick, permanent ice, East A ...
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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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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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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 ...
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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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Alfred Ritscher
Alfred Ritscher (23 May 1879 in Bad Lauterberg – 30 March 1963 in Hamburg) was a German polar explorer. A ''Kapitän zur See'' in the ''Kriegsmarine'', he led the third German Antarctic Expedition in 1938–39, which mapped the New Swabia (german: Neuschwabenland) territories of Queen Maud Land. Ritscher PeakUSGS Geographic Names Information SystemUSGS GNIS: Ritscher Peak/ref> and Ritscher UplandUSGS Geographic Names Information SystemUSGS GNIS: Ritscher Upland/ref> there are named for him. Biography In 1897 Alfred Ritscher made his first trip as a cabin boy on the Bremen ship "Emily". In 1903 he passed his helmsman exams and earned his master's certificate in 1907. At the beginning of 1912, Ritscher gained a place in the newly created Seehandbuchwerk of the Navy Office. Ritscher was skipper of the "German Arctic Expedition" of 1912–1913, under the command of Herbert Schröder-Stranz, which departed from Tromsø in the motor vessel ''Herzog Ernst'' for a preliminary rec ...
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Eduard Dallmann
Eduard Dallmann (11 March 1830 â€“ 23 December 1896) was a German whaler, trader, and Polar explorer. Dallmann was born in Blumenthal, at-the-time a village just to the north of Bremen. He began his adventures as a young sailor at the age of 15. In 1866, he became captain of the Hawaii-registered ship ''W.C. Talbot'' and undertook trading trips through the Bering and Chukchi Seas to locations in Alaska and Chukotka. He was the first European to set foot on Wrangel Island. From 1867 to 1870, he commanded the ''Count Bismarck'' on a whaling cruise to the Pacific tropics and the Bering and Chukchi seas.''Friend'', of Honolulu, December 1, 1869, Vol. 19, No. 12, p. 104. From 1872 to 1874, when whales became more of a rarity in Arctic waters, Dallmann was commissioned to explore the Antarctic seas on the sailing-steamer ''Grönland''. The operation was moderately successful from a whaling point-of-view, but more importantly, Dallmann made many discoveries around Antarctica†...
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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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List Of Mountains Of Queen Maud Land
This list of mountains of Queen Maud Land contains mountains with a registered elevation of higher than 2000 metres (6561 feet) above sea level. The availability of accurate data for this region is limited, making the list both incomplete and inaccurate. Prominence data is generally not available, and the list includes rock formations such as mountain peaks, ridges, nunataks, cliffs and crags. Ice domes are not included in the list. With an elevation of ,s Jøkulkyrkja Mountain is the highest mountain of Queen Maud Land. According to the United States Geological Survey (USGS) database Geographic Names Information System (GNIS) and other sources, several summits in the Sør Rondane Mountains are registered with higher elevation, including Isachsen Mountain (3,425 metres), Devold Peak (3,280 meters), Kjelbotn Peak (3,210 meters), Bond Peaks (3,180 meters) and Mount Widerøe (3,180 meters). According to Belgian sources and Norwegian topographic maps, the highest elevation of Sør ...
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Slabotnen Cirque
Slabotnen Cirque () is a cirque formed between the east slopes of Mount Dallmann and the Shcherbakov Range, in the Orvin Mountains of 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 addit .... It was discovered and photographed by the German Antarctic Expedition, 1938–39. It was mapped by Norway from air photos and surveys by Norwegian Antarctic Expedition, 1956–60, and named Slabotnen (the sloping cirque). Cirques of Queen Maud Land Princess Astrid Coast {{PrincessAstridCoast-geo-stub ...
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Mountains Of Queen Maud 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 ...
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