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Gneiskopf Peak
Gneiskopf Peak () is a peak high rising southwest of Mount Neustruyev at the southern end of the Südliche Petermann Range, in the Wohlthat Mountains of Queen Maud Land, Antarctica. It was discovered and given the descriptive name Gneiskopf (gneiss peak) by the Third German Antarctic Expedition (1938–1939), led by Captain Alfred Ritscher. 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 ... References External links Scientific Committee on Antarctic Research (SCAR) {{Antarctica topics Mountains of Queen Maud Land Princess Astrid Coast ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount Neustruyev
Mount Neustruyev (also known as Gora Neustruyeva) is a peak in East Antarctica, 2,900 m, standing 5 mi NNE of Gneiskopf Peak in Südliche Petermann Range, Wohlthat Mountains, Queen Maud Land. Discovery and naming Mount Neustruyev was discovered and plotted from air photos by the Third German Antarctic Expedition (1938–1939), led by Capt. Alfred Ritscher. Mapped from air photos and surveys by Sixth Norwegian Antarctic Expedition, 1956–60; remapped by Soviet Antarctic Expedition, 1960–61, and named after the Soviet geographer S.S. Neustruyev (1874–1928). 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 ... References External links United States Geological Survey, Geographic Names Information System (GNIS)Scientific Commit ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Südliche Petermann Range
Südliche Petermann Range (german: Südliche Petermannkette, also known as Söre Petermannkjeda, and Gory Otto Grotevolya) is one of the Petermann Ranges, trending NE-SW for from Svarthausane Crags to Gneiskopf Peak, in the Wohlthat Mountains, Queen Maud Land. Mount Neustruyev (also known as Gora Neustruyeva) is a 2,900 meter peak standing NNE of Gneiskopf Peak. Discovery and naming Südliche Petermann Range was discovered and plotted from air photos by the Third German Antarctic Expedition (1938-1939), led by Capt. Alfred Ritscher, which gave directional names to the eastern, middle and western units of the Petermann Ranges. This range was named Sore Petermannkjeda by Sixth Norwegian Antarctic Expedition, 1956–60, because of its southern position in association with other units in the Petermann Ranges. A German form of this name has been recommended by US-ACAN to agree with spellings adopted for the aforementioned ranges. Features * Aurdalsegga Ridge * Bystrov Rock * G ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Wohlthat Mountains
Wohlthat Mountains (german: Wohlthatmassiv) is a large group of associated mountain features consisting of the Humboldt Mountains, Petermann Ranges, and the Gruber Mountains, located immediately east of the Orvin Mountains in Fimbulheimen in the central Queen Maud Land. Discovered by the Third German Antarctic Expedition (1938–1939), led by Capt. Alfred Ritscher, and named for Councilor of state Helmuth C.H. Wohlthat, who as economist and fiscal officer dealt with the organization of the expedition. The area was reconnoitered and aerially photographed by the 5th Indian Antarctic Expedition (Nov 1985-Mar 1986) with a three-month temporary summer camp established there. The area was revisited by later Indian Antarctic expeditions. Astor Rocks The Astor Rocks () are two small rock outcrops lying southeast of Mount Ramenskiy in the southeast extremity of the Wohlthat Mountains. They were plotted from air photos and from surveys by the Sixth Norwegian Antarctic Expedition (NorAE) ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Gneiss
Gneiss ( ) is a common and widely distributed type of metamorphic rock. It is formed by high-temperature and high-pressure metamorphic processes acting on formations composed of igneous or sedimentary rocks. Gneiss forms at higher temperatures and pressures than schist. Gneiss nearly always shows a banded texture characterized by alternating darker and lighter colored bands and without a distinct cleavage. Gneisses are common in the ancient crust of continental shields. Some of the oldest rocks on Earth are gneisses, such as the Acasta Gneiss. Description Orthogneiss from the Czech Republic In traditional English and North American usage, a gneiss is a coarse-grained metamorphic rock showing compositional banding (gneissic banding) but poorly developed schistosity and indistinct cleavage. In other words, it is a metamorphic rock composed of mineral grains easily seen with the unaided eye, which form obvious compositional layers, but which has only a weak tendency to fracture ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
