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Nibelungen Valley
The Inland Forts () are a line of peaks extending between Northwest Mountain and Saint Pauls Mountain, in the Asgard Range of Victoria Land, Antarctica. Taylor Glacier lies to the south. The peaks were discovered and so named by the British National Antarctic Expedition, 1901–04. Peaks * Mattox Bastion * Sutherland Peak * Wolak Peak The Inland Forts () are a line of peaks extending between Northwest Mountain and Saint Pauls Mountain, in the Asgard Range of Victoria Land, Antarctica. Taylor Glacier lies to the south. The peaks were discovered and so named by the British Nationa ... References Further reading * James G. Bockheim, editorThe Soils of Antarctica p. 133 US Antarctic Program Continuation: Environmental Impact Statement p. 36 * David R. Marchant, George H. Denton, David E. Sugden and Carl C. Swisher, IIIMiocene Glacial Stratigraphy and Landscape Evolution of the Western Asgard Range, Antarctica Asgard Range Mountain ranges of Victoria Land McMur ...
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Northwest Mountain
The Inland Forts () are a line of peaks extending between Northwest Mountain and Saint Pauls Mountain, in the Asgard Range of Victoria Land, Antarctica. Taylor Glacier lies to the south. The peaks were discovered and so named by the British National Antarctic Expedition, 1901–04. Peaks * Mattox Bastion * Sutherland Peak * Wolak Peak References Further reading * James G. Bockheim, editorThe Soils of Antarctica p. 133 US Antarctic Program Continuation: Environmental Impact Statement p. 36 * David R. Marchant, George H. Denton, David E. Sugden and Carl C. Swisher, IIIMiocene Glacial Stratigraphy and Landscape Evolution of the Western Asgard Range, Antarctica
Asgard Range Mountain ranges of Victoria Land McMurdo Dry Valleys {{McMurdoDryValleys-geo-stub ...
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Saint Pauls Mountain
The Inland Forts () are a line of peaks extending between Northwest Mountain and Saint Pauls Mountain, in the Asgard Range of Victoria Land, Antarctica. Taylor Glacier lies to the south. The peaks were discovered and so named by the British National Antarctic Expedition The ''Discovery'' Expedition of 1901–1904, known officially as the British National Antarctic Expedition, was the first official British exploration of the Antarctic regions since the voyage of James Clark Ross sixty years earlier (1839–18 ..., 1901–04. Peaks * Mattox Bastion * Sutherland Peak * Wolak Peak References Further reading * James G. Bockheim, editorThe Soils of Antarctica p. 133 US Antarctic Program Continuation: Environmental Impact Statement p. 36 * David R. Marchant, George H. Denton, David E. Sugden and Carl C. Swisher, IIIMiocene Glacial Stratigraphy and Landscape Evolution of the Western Asgard Range, Antarctica Asgard Range Mountain ranges of Victoria Land McM ...
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Asgard Range
The Asgard Range is a mountain range in Victoria Land, Antarctica. It divides Wright Valley from Taylor Glacier and Taylor Valley, and was named by the Victoria University of Wellington Antarctic Expedition (1958–59) after Asgard, the home of the Norse gods. Geography The Asgard Range contains numerous named features such as peaks, valleys, and glaciers, and even some sub-ranges. Many are named after Norse gods and mythological figures, in keeping with the name of the range itself. Mountains * Ball Peak * Mount Beowulf * Bromley Peak * Brunhilde Peak * Mount Carnes * Mount Darby * Mount Feola * Mount Freya * Mount Holm-Hansen * Mount Grendal * Mount Hall * Harp Hill * Harris Peak * Hetha Peak * Hind Turret * Hoehn Peak * Hoffman Peak * Idun Peak * Mount Irvine * Mount Jord * Mount Knox * Mount Loke * Lyons Cone * Matterhorn * Mattox Bastion * Mount Newall * Obelisk Mountain * Mount Odin * Oliver Peak * Panorama Peak * Perk Summit * Ponder Peak * Mount ...
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Victoria Land
Victoria Land is a region in eastern Antarctica which fronts the western side of the Ross Sea and the Ross Ice Shelf, extending southward from about 70°30'S to 78°00'S, and westward from the Ross Sea to the edge of the Antarctic Plateau. It was discovered by Captain James Clark Ross in January 1841 and named after Queen Victoria. The rocky promontory of Minna Bluff is often regarded as the southernmost point of Victoria Land, and separates the Scott Coast to the north from the Hillary Coast of the Ross Dependency to the south. The region includes ranges of the Transantarctic Mountains and the McMurdo Dry Valleys (the highest point being Mount Abbott in the Northern Foothills), and the flatlands known as the Labyrinth. The Mount Melbourne is an active volcano in Victoria Land. Early explorers of Victoria Land include James Clark Ross and Douglas Mawson. In 1979, scientists discovered a group of 309 meteorites in Antarctica, some of which were found near the Allan Hills in ...
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Taylor Glacier
__NOTOC__ The Taylor Glacier is an Antarctic glacier about long, flowing from the plateau of Victoria Land into the western end of Taylor Valley, north of the Kukri Hills, south of the Asgard Range. The middle part of the glacier is bounded on the north by the Inland Forts and on the south by Beacon Valley. History The glacier was discovered by the British National Antarctic Expedition (1901–04) and at that time thought to be a part of Ferrar Glacier. The Western Journey Party of the British Antarctic Expedition of 1910 determined that the upper and lower portions of what was then known as Ferrar Glacier are apposed, i.e., joined in Siamese-twin fashion north of Knobhead. With this discovery Robert Falcon Scott named the upper portion for Thomas Griffith Taylor, geologist and leader of the Western Journey Party. Glaciology Research The Taylor Glacier has been the focus of a measurement and modeling effort carried out by researchers from the University of California, B ...
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British National Antarctic Expedition
The ''Discovery'' Expedition of 1901–1904, known officially as the British National Antarctic Expedition, was the first official British exploration of the Antarctic regions since the voyage of James Clark Ross sixty years earlier (1839–1843). Organized on a large scale under a joint committee of the Royal Society and the Royal Geographical Society (RGS), the new expedition carried out scientific research and geographical exploration in what was then largely an untouched continent. It launched the Antarctic careers of many who would become leading figures in the Heroic Age of Antarctic Exploration, including Robert Falcon Scott who led the expedition, Ernest Shackleton, Edward Wilson, Frank Wild, Tom Crean and William Lashly. Its scientific results covered extensive ground in biology, zoology, geology, meteorology and magnetism. The expedition discovered the existence of the only snow-free Antarctic valleys, which contains the longest river of Antarctica. Further ach ...
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Mattox Bastion
The Inland Forts () are a line of peaks extending between Northwest Mountain and Saint Pauls Mountain, in the Asgard Range of Victoria Land, Antarctica. Taylor Glacier lies to the south. The peaks were discovered and so named by the British National Antarctic Expedition The ''Discovery'' Expedition of 1901–1904, known officially as the British National Antarctic Expedition, was the first official British exploration of the Antarctic regions since the voyage of James Clark Ross sixty years earlier (1839–18 ..., 1901–04. Peaks * Mattox Bastion * Sutherland Peak * Wolak Peak References Further reading * James G. Bockheim, editorThe Soils of Antarctica p. 133 US Antarctic Program Continuation: Environmental Impact Statement p. 36 * David R. Marchant, George H. Denton, David E. Sugden and Carl C. Swisher, IIIMiocene Glacial Stratigraphy and Landscape Evolution of the Western Asgard Range, Antarctica Asgard Range Mountain ranges of Victoria Land McMu ...
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Sutherland Peak
The Inland Forts () are a line of peaks extending between Northwest Mountain and Saint Pauls Mountain, in the Asgard Range of Victoria Land, Antarctica. Taylor Glacier lies to the south. The peaks were discovered and so named by the British National Antarctic Expedition, 1901–04. Peaks * Mattox Bastion The Inland Forts () are a line of peaks extending between Northwest Mountain and Saint Pauls Mountain, in the Asgard Range of Victoria Land, Antarctica. Taylor Glacier lies to the south. The peaks were discovered and so named by the British Nationa ... * Sutherland Peak * Wolak Peak References Further reading * James G. Bockheim, editorThe Soils of Antarctica p. 133 US Antarctic Program Continuation: Environmental Impact Statement p. 36 * David R. Marchant, George H. Denton, David E. Sugden and Carl C. Swisher, IIIMiocene Glacial Stratigraphy and Landscape Evolution of the Western Asgard Range, Antarctica Asgard Range Mountain ranges of Victoria Land McMur ...
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Wolak Peak
The Inland Forts () are a line of peaks extending between Northwest Mountain and Saint Pauls Mountain, in the Asgard Range of Victoria Land, Antarctica. Taylor Glacier lies to the south. The peaks were discovered and so named by the British National Antarctic Expedition, 1901–04. Peaks * Mattox Bastion * Sutherland Peak The Inland Forts () are a line of peaks extending between Northwest Mountain and Saint Pauls Mountain, in the Asgard Range of Victoria Land, Antarctica. Taylor Glacier lies to the south. The peaks were discovered and so named by the British Nationa ... * Wolak Peak References Further reading * James G. Bockheim, editorThe Soils of Antarctica p. 133 US Antarctic Program Continuation: Environmental Impact Statement p. 36 * David R. Marchant, George H. Denton, David E. Sugden and Carl C. Swisher, IIIMiocene Glacial Stratigraphy and Landscape Evolution of the Western Asgard Range, Antarctica Asgard Range Mountain ranges of Victoria Land McMurd ...
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Mountain Ranges Of Victoria 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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