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Liljequist Heights
The Liljequist Heights () are the heights about south of the Grunehogna Peaks, in the Ahlmann Ridge of Queen Maud Land, Antarctica. They were mapped by Norwegian cartographers from surveys and air photos by the Norwegian–British–Swedish Antarctic Expedition (NBSAE) (1949–52) and air photos by the Norwegian expedition (1958–59). The heights are named for Gösta Hjalmar Liljequist, a Swedish meteorologist with the NBSAE. Preikestolen Ridge is a ridge in the western part of Liljequist Heights. It was first mapped by Norwegian cartographers from surveys and air photos by the NBSAE of 1949–1952, led by John Schjelderup Giæver and air photos by the Norwegian expedition (1958–59) and named ''Preikestolen'' ("the pulpit A pulpit is a raised stand for preachers in a Christian church. The origin of the word is the Latin ''pulpitum'' (platform or staging). The traditional pulpit is raised well above the surrounding floor for audibility and visibility, access ..."). ...
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Grunehogna Peaks
The Grunehogna Peaks () are a group of peaks north of the Liljequist Heights, in the south part of Ahlmann Ridge in Queen Maud Land, Antarctica. They were photographed from the air by the Third German Antarctic Expedition (1938–39). They were mapped by Norwegian cartographers from surveys and air photos by the Norwegian–British–Swedish Antarctic Expedition (1949–52) and the Norwegian expedition (1958–59) and named Grunehogna. The summer research station Sarie Marais was erected at Grunehogna for geological, geophysical, and surveying programs in the 1982/1983 summer by the South African National Antarctic Programme The South African National Antarctic Programme (or SANAP) is the South African government's programme for research in the Antarctic and Subantarctic. Three research stations fall under this programme: the Antarctica research station SANAE IV, an ... and decommissioned in the 2001/2002 summer season. References Mountains of Queen Maud Land Princess Mar ...
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Ahlmann Ridge
Ahlmann Ridge, also known as Ahlmannryggen, is a broad, mainly ice-covered ridge, about long, surmounted by scattered, low peaks. It rises between Schytt Glacier and Jutulstraumen Glacier and extends from Borg Massif northward to Fimbul Ice Shelf in Queen Maud Land. The area was first photographed from aircraft of the Third German Antarctic Expedition (1938–39) and peaks in this vicinity were roughly plotted. The Stein Nunataks and Witte Peaks, named by the German Antarctic Expedition, appear to coincide with the northeast part of the Ahlmann Ridge. The feature was mapped in detail from surveys and air photos by the Norwegian-British-Swedish Antarctic Expedition (NBSAE) (1949–1952) and air photos by the Norwegian expedition (1958–59). Named for Hans Wilhelmsson Ahlmann, chairman of the Swedish committee for the NBSAE. Istindhalsen Saddle is an ice saddle between Istind Peak and the Grunehogna Peaks on the Ahlmann Ridge. Like the ridge, it was mapped by the NBSAE and th ...
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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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Norwegian–British–Swedish Antarctic Expedition
The Norwegian–British–Swedish Antarctic Expedition (also known as NBSX or NBSAE) (1949–1952) was the first Antarctica expedition involving an international team of scientists. The team members came from Norway, Sweden and the British Commonwealth of Nations. History The Norwegian–British–Swedish Antarctic Expedition was the first expedition to Antarctica involving an international team of scientists. The expedition was led by John Schjelderup Giæver, a Norwegian author and polar researcher. The expedition had the goal of establishing whether climatic fluctuations observed in the Arctic were also occurring in the Antarctic. A base known as Maudheim was established on the Quar Ice Shelf along the coast of Queen Maud Land in February 1950. This expedition laid the groundwork for the following Australian expeditions to Antarctic from 1954 to the early 1960s. Transportation The expedition was transported aboard a 600-ton sealer named that was powered by a German U-boat dies ...
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Gösta Hjalmar Liljequist
Gösta Hjalmar Liljequist (1914–1995) was a Swedish meteorologist. In Sweden, radio broadcast weather forecasts begun in 1926, and, starting in 1941, Liljequist was one of the recurrent meteorologists appearing in Swedish radio for many years. Following his debut, his peculiar dialect caused mass protests which, together with an attack published by the humorist Kar de Mumma in the paper Svenska Dagbladet ''Svenska Dagbladet'' (, "The Swedish Daily News"), abbreviated SvD, is a daily newspaper published in Stockholm, Sweden. History and profile The first issue of ''Svenska Dagbladet'' appeared on 18 December 1884. During the beginning of the ..., caused broadcast forecasts to be taken over by Swedish public service radio during the war. After the war, Liljequist took part in the Norwegian-British-Swedish Antarctic Expedition (NBSAE) (1949-1952). During the expedition he became the first to observe a rare type of halo, an optical phenomenon subsequently named Lilj ...
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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 192 ...
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Pulpit
A pulpit is a raised stand for preachers in a Christian church. The origin of the word is the Latin ''pulpitum'' (platform or staging). The traditional pulpit is raised well above the surrounding floor for audibility and visibility, accessed by steps, with sides coming to about waist height. From the late medieval period onwards, pulpits have often had a canopy known as the sounding board, ''tester'' or ''abat-voix'' above and sometimes also behind the speaker, normally in wood. Though sometimes highly decorated, this is not purely decorative, but can have a useful acoustic effect in projecting the preacher's voice to the congregation below. Most pulpits have one or more book-stands for the preacher to rest his or her bible, notes or texts upon. The pulpit is generally reserved for clergy. This is mandated in the regulations of the Catholic Church, and several others (though not always strictly observed). Even in Welsh Nonconformism, this was felt appropriate, and in som ...
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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 and ...
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