Skeidskar Gap
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Skeidskar Gap
Skeidskar Gap () is a narrow gap in the ridge along the southeast side of Skarskvervet Glacier, in the Humboldt 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 .... Discovered and photographed by the German Antarctic Expedition, 1938–39. Mapped by Norway from air photos and surveys by Norwegian Antarctic Expedition, 1956–60, and named Skeidskar. Mountain passes of Queen Maud Land Humboldt Mountains (Antarctica) {{PrincessAstridCoast-geo-stub ...
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Skarskvervet Glacier
Livdebotnen Cirque () is a cirque formed in the northeast side of Mount Flånuten and the west side of Botnfjellet Mountain, in the Humboldt Mountains of Queen Maud Land, Antarctica. Exploration and naming Livdebotnen Cirque was discovered and photographed by the German Antarctic Expedition (1938–1939) (GerAE). It was mapped by Norway from air photos and surveys by the Sixth Norwegian Antarctic Expedition The sixth Norwegian Antarctic Expedition (''Den norske antarktisekspedisjonen'') was a scientific expedition to Queen Maud Land in Antarctica. The expedition was based at Norway Station () which was located on the Fimbul Ice Shelf bordering the coa ..., 1956–60 (NorAE), and named Livdebotnen (the shelter cirque). Features Features in and around the Livdebotnen Cirque include: Botnfjellet Mountain . A mountain, high, forming the northeast and east walls of Livdebotnen Cirque. Discovered and photographed by the GerAE, 1938-39. Mapped by Norway from air photos and su ...
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Humboldt Mountains (Antarctica)
The Humboldt Mountains are a group of mountains immediately west of the Petermann Ranges, forming the westernmost portion of the Wohlthat Mountains in Queen Maud Land, Antarctica. History The mountains were discovered and mapped by the Third German Antarctic Expedition (1938–1939), led by Alfred Ritscher, who named them for Alexander von Humboldt, famed German naturalist and geographer of the first half of the nineteenth century. Historic monument A plaque was erected at India Point () in the Humboldt Mountains in memory of three scientists of the Geological Survey of India, as well as a communications technician from the Indian Navy, all of whom were members of the ninth Indian Expedition to Antarctica, who died in an accident at the site on 8 January 1990. The plaque has been designated a Historic Site or Monument (HSM 78), following a proposal by India to the Antarctic Treaty Consultative Meeting. Geological features Mount Skarshovden Mount Skarshovden () is a rounded m ...
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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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New Swabia
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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Sixth Norwegian Antarctic Expedition
The sixth Norwegian Antarctic Expedition (''Den norske antarktisekspedisjonen'') was a scientific expedition to Queen Maud 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 over a period of 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 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 researchers which was reduced to nine during the third year. Among their activities were topological mapping of the region. In 1960, King Olav V of Norway instituted the Antarctic Medal The Antarctic Medal is a civil decoration of Norway. Established by ...
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Mountain Passes 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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