Steinskaret Gap

	Steinskaret Gap Steinskaret Gap is an ice-filled gap in the central Kurze Mountains The Kurze Mountains (german: Kurzegebirge) are a range of mainly bare rock peaks, ridges and mountains about long and wide in the Orvin Mountains of Queen Maud Land, Antarctica. The feature stands between the Drygalski Mountains on the west a ..., just south of Steinskaregga Ridge. Mapped from surveys and air photos by Norwegian Antarctic Expedition (1956–60) and named Steinskaret (the stone gap). Mountain passes of Queen Maud Land Princess Astrid Coast {{PrincessAstridCoast-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu]
picture info	Kurze Mountains The Kurze Mountains (german: Kurzegebirge) are a range of mainly bare rock peaks, ridges and mountains about long and wide in the Orvin Mountains of Queen Maud Land, Antarctica. The feature stands between the Drygalski Mountains on the west and the Gagarin Mountains and Conrad Mountains on the east. The Kurze Mountains were discovered and plotted from aerial photographs taken by the Third German Antarctic Expedition under Alfred Ritscher, 1938–39, who named them for the director of the Naval Division of the former Marineleitung ( German Admiralty). They were remapped by the Norsk Polarinstitutt from surveys and aerial photos taken 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, and given the name "Holtedahlfjella." Th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu]
	Steinskaregga Ridge Steinskaregga Ridge () is a bare rock ridge just north of Steinskaret Gap in the Kurze Mountains The Kurze Mountains (german: Kurzegebirge) are a range of mainly bare rock peaks, ridges and mountains about long and wide in the Orvin Mountains of Queen Maud Land, Antarctica. The feature stands between the Drygalski Mountains on the west a ... of Queen Maud Land. Mapped from surveys and air photos by Norwegian Antarctic Expedition (1956–60) and named Steinskaregga (the stone gap ridge). Ridges of Queen Maud Land Princess Astrid Coast {{PrincessAstridCoast-geo-stub ... [...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 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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu]
picture info	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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu]