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Sætet
Sætet, also known as Saetet Cirque, is a large cirque in the north side of Jutulsessen, in the Gjelsvik Mountains, Queen Maud Land, Antarctica. Photographed from the air by the Third German Antarctic Expedition (1938–39). Mapped by Norwegian cartographers from surveys and air photos by the Norwegian-British-Swedish Antarctic Expedition (NBSAE) (1949–1952), led by John Schjelderup Giæver John Schjelderup Giæver (31 December 1901 – 9 November 1970) was a Norwegian author and polar researcher. Jónsbú Station in NE Greenland was named after him. Personal life He was born in Tromsø in Troms, Norway. He was the son of lawy ... and air photos by the Norwegian expedition (1958–59) and named Sætet, meaning "the seat". References Cirques of Queen Maud Land Princess Martha Coast {{PrincessMarthaCoast-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Jutulsessen
Jutulsessen is a nunatak in the Gjelsvik Mountains in Queen Maud Land, Antarctica. It is located in Princess Martha Coast, from the King Haakon VII Sea. Jutulsessen is the site of the Norwegian research station Troll (research station), Troll and the affiliated Troll Satellite Station, which has two radomes on top of the mountain. Troll Airfield is located in the vicinity. Geography Jutulsessen is a nunatak mountain with a peak above mean sea level. It is located north of Terningskarvet Mountain, Terningskarvet, also in the Gjelsvik Mountains of Queen Maud Land. Jutulsessen is located in the eastern part of Princess Martha Coast in Queen Maud Land, which Norway claims as a dependent territory.Kyvik (2008): 153 The main ice-free area of the Jutulsessen massif is about 10 km long by 5 km across. The base is located above mean sea level and is completely surrounded by the Antarctic ice sheet. Jutulsessen is from the coast of King Haakon VII Sea. The mountain area is h ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Norwegian Polar Institute
The Norwegian Polar Institute (NPI; no, Norsk Polarinstitutt) is Norway's central governmental institution for scientific research, mapping and environmental monitoring in the Arctic and the Antarctic. The NPI is a directorate under Norway's Ministry of Climate and Environment. The institute advises Norwegian authorities on matters concerning polar environmental management and is the official environmental management body for Norwegian activities in Antarctica. Activities The institute's activities are focused on environmental research and management in the polar regions. The NPI's researchers investigate biodiversity, climate and environmental toxins in the Arctic and Antarctic, and in this context the institute equips and organizes large-scale expeditions to both polar regions. The institute contributes to national and international climate work, and is an active contact point for the international scientific community. The institute collects and analyses data on the environm ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cirque
A (; from the Latin word ') is an amphitheatre-like valley formed by glacial erosion. Alternative names for this landform are corrie (from Scottish Gaelic , meaning a pot or cauldron) and (; ). A cirque may also be a similarly shaped landform arising from fluvial erosion. The concave shape of a glacial cirque is open on the downhill side, while the cupped section is generally steep. Cliff-like slopes, down which ice and glaciated debris combine and converge, form the three or more higher sides. The floor of the cirque ends up bowl-shaped, as it is the complex convergence zone of combining ice flows from multiple directions and their accompanying rock burdens. Hence, it experiences somewhat greater erosion forces and is most often overdeepened below the level of the cirque's low-side outlet (stage) and its down-slope (backstage) valley. If the cirque is subject to seasonal melting, the floor of the cirque most often forms a tarn (small lake) behind a dam, which marks the down ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Gjelsvik Mountains
The Gjelsvik Mountains are a group of mountains about long, between the Sverdrup Mountains and the Mühlig-Hofmann Mountains in Queen Maud Land, East Antarctica. With its summit at , the massive Risemedet Mountain forms the highest point in these mountains, also marking their eastern end. Discovery and naming The Gjelsvik Mountains were first photographed from the air and roughly plotted by the Third German Antarctic Expedition (1938–39). They were mapped in detail by Norwegian cartographers from surveys and air photos by the Norwegian–British–Swedish Antarctic Expedition (1949–52) and from air photos by the Norwegian expedition (1958–59). They were named for Tore Gjelsvik, Director of the Norwegian Polar Institute. Features * Bakhallet Slope * Brugda Ridge * Bundermann Range * Jutulsessen * Mayr Ridge * Nupskammen Ridge * Terningskarvet Mountain * Von Essen Mountain See also * Gygra Peak * List of mountains of Queen Maud Land This list of mountains ... [...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] |
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 ... [...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] |
John Schjelderup Giæver
John Schjelderup Giæver (31 December 1901 – 9 November 1970) was a Norwegian author and polar researcher. Jónsbú Station in NE Greenland was named after him. Personal life He was born in Tromsø in Troms, Norway. He was the son of lawyer John Schjelderup Giæver (1864–1914) and his wife Thyra Høegh (1879–1954). He was the great-great-great-grandson of Jens Holmboe. John Schjelderup Giæver married Oddbjørg Jacobsen in March 1940 and they had a son in April the same year. However, the marriage was dissolved. Giæver married Anna Margrethe Gløersen in 1948; this time they had a daughter, born 1954. Career He took his secondary education in Trondheim in 1920, and then moved back to Tromsø. He started a newspaper career, as sub-editor of '' Tromsø Stiftstidende'' from 1921 to 1922. He was editor-in-chief in ''Vesteraalens Avis'' from 1922 to 1928 and ''Tromsø Stiftstidende'' from 1928 to 1929. He lived as a trapper in north-eastern Greenland from 1929 to ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cirques Of Queen Maud Land
A (; from the Latin word ') is an amphitheatre-like valley formed by glacial erosion. Alternative names for this landform are corrie (from Scottish Gaelic , meaning a pot or cauldron) and (; ). A cirque may also be a similarly shaped landform arising from fluvial erosion. The concave shape of a glacial cirque is open on the downhill side, while the cupped section is generally steep. Cliff-like slopes, down which ice and glaciated debris combine and converge, form the three or more higher sides. The floor of the cirque ends up bowl-shaped, as it is the complex convergence zone of combining ice flows from multiple directions and their accompanying rock burdens. Hence, it experiences somewhat greater erosion forces and is most often overdeepened below the level of the cirque's low-side outlet (stage) and its down-slope (backstage) valley. If the cirque is subject to seasonal melting, the floor of the cirque most often forms a tarn (small lake) behind a dam, which marks the down ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
