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Cape Norvegia
Cape Norvegia is a prominent cape on Princess Martha Coast of Queen Maud Land. It marks the northeast extremity of Riiser-Larsen Ice Shelf in East Antarctica, and the border point of Weddell Sea and King Haakon VII Sea. It was discovered by Commander Hjalmar Riiser-Larsen in February 1930 while on an airplane flight from the Norvegia, the ship in which the expedition ''The Expedition'' is the live album by the American metal band Kamelot, released in October 2000 through Noise Records. The last three tracks are rare studio recordings: "We Three Kings" (instrumental) and "One Day" are additional material fro ... was made. The cape was named by Riiser-Larsen for the ship. References Headlands of Queen Maud Land Princess Martha Coast {{PrincessMarthaCoast-geo-stub ...
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Princess Martha Coast
Princess Martha Coast ( no, Kronprinsesse Märtha Kyst) is that portion of the coast of Queen Maud Land lying between 05° E and the terminus of Stancomb-Wills Glacier, at 20° W. The entire coastline is bounded by ice shelves with ice cliffs high. Princess Martha Coast was the first portion of Antarctic mainland discovered by a human, Fabian von Bellingshausen and Mikhail Lazarev in 1820. The name "Crown Princess Martha Land" was originally applied by Capt. Hjalmar Riiser-Larsen to that section of the coast in the vicinity of Cape Norvegia which he discovered from the ''Norvegia'' and roughly charted from the air during February 1930. On January 19, 1939, Nazi Germany reached the Martha Coast which was a part of the German Antarctic Expedition. It is named in honour of Crown Princess Märtha of Norway. Troll A troll is a being in Nordic folklore, including Norse mythology. In Old Norse sources, beings described as trolls dwell in isolated areas of rocks, mountains, ...
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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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Riiser-Larsen Ice Shelf
Riiser-Larsen Ice Shelf is an ice shelf about 250 miles (400 km) long on the coast of Queen Maud Land, Antarctica, extending from Cape Norvegia in the north to Lyddan Island and Stancomb-Wills Glacier in the south. Discovery and naming Parts of the ice shelf were sighted by William Speirs Bruce in 1904, Ernest Shackleton in 1915, and Hjalmar Riiser-Larsen in 1930. Most of it was photographed from the air in 1951-52 by the Norwegian-British-Swedish Antarctic Expedition (NBSAE) and delineated from these photos. Additional delineation of the southern and landward margins of the feature was accomplished from aerial photos taken, by the USN's Operation Deep Freeze from 1967 to 1969. The feature was named by Norway for Captain Hjalmar Riiser-Larsen, who explored the area in the late 1920s and early 1930s. Important Bird Area A 477 ha site on fast ice, on the northern coast of the ice shelf some 90 km south-west of Seal Bay and 140 km north-east of Cape Ve ...
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East Antarctica
East Antarctica, also called Greater Antarctica, constitutes the majority (two-thirds) of the Antarctic continent, lying on the Indian Ocean side of the continent, separated from West Antarctica by the Transantarctic Mountains. It lies almost entirely within the Eastern Hemisphere and its name has been accepted for more than a century. It is generally higher than West Antarctica and includes the Gamburtsev Mountain Range in the center. The geographic South Pole is located within East Antarctica. Apart from small areas of the coast, East Antarctica is permanently covered by ice and it has relatively low biodiversity, with only a small number of species of terrestrial plants, animals, algae, and lichens. The coasts are the breeding ground for various seabirds and penguins, and the leopard seal, Weddell seal, elephant seal, crabeater seal and Ross seal breed on the surrounding pack ice in summer. Location and description Almost completely covered in thick, permanent ice ...
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Weddell Sea
The Weddell Sea is part of the Southern Ocean and contains the Weddell Gyre. Its land boundaries are defined by the bay formed from the coasts of Coats Land and the Antarctic Peninsula. The easternmost point is Cape Norvegia at Princess Martha Coast, Queen Maud Land. To the east of Cape Norvegia is the King Haakon VII Sea. Much of the southern part of the sea is covered by a permanent, massive ice shelf field, the Filchner-Ronne Ice Shelf. The sea is contained within the two overlapping Antarctic territorial claims of Argentine Antarctica, the British Antarctic Territory, and also resides partially within the Antarctic Chilean Territory. At its widest the sea is around across, and its area is around . Various ice shelves, including the Filchner-Ronne Ice Shelf, fringe the Weddell sea. Some of the ice shelves on the east side of the Antarctic Peninsula, which formerly covered roughly of the Weddell Sea, had completely disappeared by 2002. The Weddell Sea has been d ...
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King Haakon VII Sea
King Haakon VII Sea ( no, King Haakon VII Hav) is a proposed name for part of the Southern Ocean on the coast of East Antarctica. Geography The International Hydrographic Organization (IHO), often recognized as the authority for worldwide water body names, does not include this sea name. The IHO 2002 draft was never approved by the IHO (or any other organization), and the 1953 IHO document (which does not contain the name) remains currently in force. Most leading geographic authorities and atlases do not use the name, including the 2014 10th edition World Atlas from the National Geographic Society. By a narrow proposed definition, this sea would be between the Weddell Sea and a proposed Lazarev Sea name, and thus stretch only along Princess Martha Coast from Cape Norvegia at 12°18′W, the easternmost point of the Weddell Sea, to Fimbul Ice Shelf close to the Prime Meridian at 0°0′, which is proposed as the western border of Lazarev Sea. From the Norwegian point of ...
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Hjalmar Riiser-Larsen
Hjalmar Riiser-Larsen (7 June 1890 – 3 June 1965) was a Norwegian aviation pioneer, military officer, polar explorer and businessman. Among his achievements, he is generally regarded a founder of the Royal Norwegian Air Force. Background Riiser-Larsen was born in Kristiania, Norway. In 1909, aged nineteen, he joined the Norwegian Naval Academy. In 1915 he became a 1st lieutenant in the newly formed Royal Norwegian Navy Air Service (RNoNAS). After World War I, he served as the acting head of the RNoNAS's factory until a more senior officer was appointed. In 1921, he joined the Aviation Council, then part of the Norwegian Ministry of Defence, as a secretary. This gave him the opportunity to study the fledgling military and civil aviation infrastructure for which the council was responsible. He also became a frequent pilot on the air routes used by the new aviation companies. Polar exploration Flying over the North Pole Riiser-Larsen's years of polar exploration began ...
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Headlands Of Queen Maud Land
A headland, also known as a head, is a coastal landform, a point of land usually high and often with a sheer drop, that extends into a body of water. It is a type of promontory. A headland of considerable size often is called a cape.Whittow, John (1984). ''Dictionary of Physical Geography''. London: Penguin, 1984, pp. 80, 246. . Headlands are characterised by high, breaking waves, rocky shores, intense erosion, and steep sea cliff. Headlands and bays are often found on the same coastline. A bay is flanked by land on three sides, whereas a headland is flanked by water on three sides. Headlands and bays form on discordant coastlines, where bands of rock of alternating resistance run perpendicular to the coast. Bays form when weak (less resistant) rocks (such as sands and clays) are eroded, leaving bands of stronger (more resistant) rocks (such as chalk, limestone, and granite) forming a headland, or peninsula. Through the deposition of sediment within the bay and the erosion of th ...
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