|
Skorvehallet Slope
Skorvehallet Slope () is a snow-covered slope with numerous rock outcrops, lying just west of the Gagarin Mountains in the Orvin Mountains, 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 .... Mapped by Norwegian cartographers from air photos and surveys by Norwegian Antarctic Expedition, 1956–60, and named Skorvehallet. Ice slopes of Queen Maud Land Princess Astrid Coast {{PrincessAstridCoast-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Gagarin Mountains
The Gagarin Mountains (russian: Khrebet Yuriya Gagarina; no, Kurzefjella) are a linear group of mountains, trending in a north–south direction for between the Kurze Mountains and the Conrad Mountains of the Orvin Mountains in Queen Maud Land, East Antarctica. Discovery and naming The Gagarin Mountains were mapped by cartographers of the Norwegian Polar Institute, using aerial photographs and surveys taken by the Sixth Norwegian Antarctic Expedition in 1956–60. They were remapped from surveys and air photos by the Soviet Antarctic Expedition, 1960–61, and named for Soviet astronaut Yuri Gagarin. See also * List of mountains of Queen Maud Land This list of mountains of Queen Maud Land contains mountains with a registered elevation of higher than 2000 metres (6561 feet) above sea level. The availability of accurate data for this region is limited, making the list both incomplete and inac ... References External links Scientific Committee on Antarctic Research (SCAR) ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Orvin Mountains
The Orvin Mountains ( no, Orvinfjella) constitute a major group of mountain ranges, extending for about between the Wohlthat Mountains and the Mühlig-Hofmann Mountains in Queen Maud Land. With its summit at , the massive Sandeggtind Peak forms the highest point in the Conrad Mountains, a subrange of the Orvin Mountains. Discovery and naming First photographed from the air and roughly plotted by the Third German Antarctic Expedition (1938-1939), led by Capt. Alfred Ritscher. Mapped by Norwegian cartographers from surveys and air photos by the Sixth Norwegian Antarctic Expedition (1956–60) and named for Anders K. Orvin, director of the Norwegian Polar Institute from 1958 to 1959. Constituent ranges Constituent ranges of Orvin Mountains, listed from east to west: * Shcherbakov Range * Mount Dallmann * Conrad Mountains * Gagarin Mountains * Kurze Mountains * Drygalski Mountains * Filchner Mountains See also * List of mountains of Queen Maud Land This list of mountain ... [...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] |
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] |
Ice Slopes Of Queen Maud Land
Ice is water frozen into a solid state, typically forming at or below temperatures of 0 degrees Celsius or Depending on the presence of impurities such as particles of soil or bubbles of air, it can appear transparent or a more or less opaque bluish-white color. In the Solar System, ice is abundant and occurs naturally from as close to the Sun as Mercury to as far away as the Oort cloud objects. Beyond the Solar System, it occurs as interstellar ice. It is abundant on Earth's surfaceparticularly in the polar regions and above the snow lineand, as a common form of precipitation and deposition, plays a key role in Earth's water cycle and climate. It falls as snowflakes and hail or occurs as frost, icicles or ice spikes and aggregates from snow as glaciers and ice sheets. Ice exhibits at least eighteen phases ( packing geometries), depending on temperature and pressure. When water is cooled rapidly (quenching), up to three types of amorphous ice can form depending on it ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
