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Larsen Cliffs
The Larsen Cliffs () are steep rock and ice cliffs which form a part of the east face of Jøkulkyrkja Mountain, in the Mühlig-Hofmann Mountains of Queen Maud Land, Antarctica. They were plotted from surveys and air photos by the Sixth Norwegian Antarctic Expedition The sixth Norwegian Antarctic Expedition (''Den norske antarktisekspedisjonen'') was a scientific expedition to Queen Maud's Land in Antarctica. The expedition was based at Norway Station () which was located on the Fimbul Ice Shelf bordering th ... (1956–60) and named for Per Larsen, a steward with the expedition (1956–57). References External links https://data.aad.gov.au/aadc/gaz/display_name.cfm?gaz_id=127815 Gazetteer Cliffs of Queen Maud Land Princess Astrid Coast {{PrincessAstridCoast-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Jøkulkyrkja Mountain
Jøkulkyrkja Mountain ("the Glacier Church"), also known as Massiv Yakova Gakkelya, is a broad, ice-topped mountain with several radial rock spurs, standing east of Lunde Glacier in the Mühlig-Hofmann Mountains of Queen Maud Land, East Antarctica. At elevation, it is the highest mountain in Queen Maud Land, and also the highest rock elevation within the claims of Norway. However, Dome F is also located in Queen Maud Land, and rises to about . The mountain is located on the Princess Astrid Coast of the Norwegian Antarctic Territory. Håhellerskarvet ("shark cave mountain"), , is located to the southwest; the two peaks are separated by the 25-mile-long Lunde Glacier, which flows to the northwest. Discovery and naming Jøkulkyrkja Mountain was plotted from surveys and air photos by the Sixth Norwegian Antarctic Expedition (1956–60) and named ''Jøkulkyrkja''. The first element is ''jøkul'' m 'small glacier', the last element is the finite form of ''kyrkje'' f 'church'. (Like ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mühlig-Hofmann Mountains
The Mühlig-Hofmann Mountains () is a major group of associated mountain features extending east to west for between the Gjelsvik Mountains and the Orvin Mountains in Queen Maud Land, East Antarctica. With its summit at , the massive Jøkulkyrkja Mountain forms the highest point in the Mühlig-Hofmann Mountains. Discovery and naming The Mühlig-Hofmann Mountains were discovered by the Third German Antarctic Expedition (1938-1939), led by Capt. Alfred Ritscher, and named for the division director of the German Air Ministry. They were remapped by the Norwegian Antarctic Expedition, 1956-1960. Features Glaciers * Austreskorve Glacier ** Kvitholten Hill * Flogeken Glacier * Langflog Glacier * Lunde Glacier * Skålebreen ** Skålebrehalsen Terrace * Sloket Glacier * Tønnesen Glacier * Vestreskorve Glacier ** Hamarglovene Crevasses Mountains and ranges * Ahlstad Hills * Breplogen Mountain ** Høgsenga Crags ** Småkovane Cirques * Buddenbrock Range * Cumulus Moun ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Queen Maud Land
Queen Maud Land () is a roughly region of Antarctica Territorial claims in Antarctica, claimed by Norway as a dependent territory. It borders the claimed British Antarctic Territory 20th meridian west, 20° west, specifically the Caird Coast, Coats Land on the West, and the Australian Antarctic Territory 45th meridian east, 45° east, specifically Enderby Land on the 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 Maud of Wales, Queen Maud (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 dependencies of Norway, two Antarctic claims made by Norway, the other being Peter I Island. They are adm ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sixth Norwegian Antarctic Expedition
The sixth Norwegian Antarctic Expedition (''Den norske antarktisekspedisjonen'') was a scientific expedition to Queen Maud's 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 for 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 Oslo ( or ; ) is the capital and most populous city of Norway. It constitutes both a county and a municipality. The municipality of Oslo had a population of in 2022, while the city's greater urban area had a population of 1,064,235 in 2022 ... 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 researche ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Per Larsen
Per Larsen (born 31 May 1962) is a Danish weightlifter. He competed in the men's middle heavyweight event at the 1988 Summer Olympics The 1988 Summer Olympics (), officially the Games of the XXIV Olympiad () and officially branded as Seoul 1988 (), were an international multi-sport event held from 17 September to 2 October 1988 in Seoul, South Korea. 159 nations were represe .... References 1962 births Living people Danish male weightlifters Olympic weightlifters for Denmark Weightlifters at the 1988 Summer Olympics Sportspeople from Aalborg 20th-century Danish sportsmen {{Denmark-weightlifting-bio-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cliffs Of Queen Maud Land
In geography and geology, a cliff or rock face is an area of rock which has a general angle defined by the vertical, or nearly vertical. Cliffs are formed by the processes of weathering and erosion, with the effect of gravity. Cliffs are common on coasts, in mountainous areas, escarpments and along rivers. Cliffs are usually composed of rock that is resistant to weathering and erosion. The sedimentary rocks that are most likely to form cliffs include sandstone, limestone, chalk, and dolomite. Igneous rocks such as granite and basalt also often form cliffs. An escarpment (or scarp) is a type of cliff formed by the movement of a geologic fault, a landslide, or sometimes by rock slides or falling rocks which change the differential erosion of the rock layers. Most cliffs have some form of scree slope at their base. In arid areas or under high cliffs, they are generally exposed jumbles of fallen rock. In areas of higher moisture, a soil slope may obscure the talus. Many cliffs ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
