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Pinnacle Gap
Pinnacle Gap () is a gap between Pain and Tobin Mesas in the Mesa Range of Victoria Land. The feature was traversed and so named by the northern party of New Zealand Geological Survey Antarctic Expedition The New Zealand Geological Survey Antarctic Expedition (NZGSAE) describes a series of scientific explorations of the continent Antarctica. The expeditions were notably active throughout the 1950s and 1960s. Features named by the expeditions 195 ... (NZGSAE), 1962–63, because it is readily identified by the high rock pinnacle ( Mount Ballou) on the north ridge overlooking the gap. Mountain passes of Victoria Land Pennell Coast {{VictoriaLand-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tobin Mesas
Tobin may refer to: Name *Tobin (surname) *Tobin (given name) Places in the United States * Tobin, California * Tobin Bridge, near Boston, Massachusetts * Tobin Range, a mountain range in Nevada * Tobin Township, Perry County, Indiana * Tobin, Wisconsin * Breitmeyer-Tobin Building, in Detroit, Michigan Fictional characters * Princess Tobin, a character in Melanie Rawn's ''Dragon Prince'' series of fantasy novels * Prince Tobin, the main character in ''The Bone Doll's Twin'' by Lynn Flewelling * Mitch Tobin, protagonist of five mystery novels by Donald Westlake * Tobin, a supporting character in the Fire Emblem franchise, who appears in '' Fire Emblem: Gaiden'' and its remake, '' Fire Emblem Echoes: Shadows of Valentia''. * Beef Tobin and his kids from the animated sitcom, ''The Great North'' * A character from the TV series ''The Walking Dead'' Other uses * Tobin tax, a currency exchange tax first proposed by James Tobin * Tobin's q, an economic measure developed by James Tobin ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mesa Range
The Mesa Range () is a range of flat-topped mesas comprising the Sheehan, Pain, Tobin and Gair Mesas, situated at the head of the Rennick Glacier in Victoria Land, Antarctica. it was given this descriptive name by the northern party of the New Zealand Geological Survey Antarctic Expedition of 1962–63. Features * Biretta Peak * Campbell Glacier * Exposure Hill * Gair Mesa * Haban Spur * Mericle Rock * Mills Valley * Monument Nunataks * Mount Ballou * Mount Fazio * Mount Masley * Pain Mesa * Pinnacle Gap * Scarab Peak Scarab Peak () is a prominent peak, 3,160 m, located 2 nautical miles (3.7 km) northeast of Mount Frustum in the southeast end of Tobin Mesa, the Mesa Range, Victoria Land. Named by the northern party of the New Zealand Geological S ... * Sheehan Mesa * Siders Bluff * Tobin Mesa * Veto Gap * Watchtower Hill References Mountain ranges of Victoria Land Pennell Coast {{VictoriaLand-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 A meteorite is a solid piece of debris from an ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
New Zealand Geological Survey Antarctic Expedition
The New Zealand Geological Survey Antarctic Expedition (NZGSAE) describes a series of scientific explorations of the continent Antarctica. The expeditions were notably active throughout the 1950s and 1960s. Features named by the expeditions 1957–1958 expedition The 1957–1958 expedition went to the Ross Dependency and named the Borchgrevink Glacier. Other features named include: * Carter Ridge * Felsite Island * Halfway Nunatak * Hedgehog Island * Moraine Ridge 1958–1959 expedition * Cadwalader Beach * Cape Hodgson * Carter Ridge * Isolation Point * Mountaineer Range * Mount Aurora * Mount Hayward * Mount Henderson (White Island) * Mount Bird. 1960–1961 expedition * Deverall Island * Lonewolf Nunataks 1961–1962 expedition * Aurora Heights * The Boil * Ford Spur * Graphite Peak * Half Century Nunatak * Half Dome Nunatak * Hump Passage * Last Cache Nunatak * Lookout Dome * Montgomerie Glacier * Mount Fyfe * Mount Macdonald * Snowshoe ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount Ballou
Mount Ballou () is a pinnacle-type mountain (2,900 m) which forms the south end of Pain Mesa and the north side of the entrance to Pinnacle Gap in the Mesa Range, Victoria Land, Antarctica. The mountain was first mapped by the United States Geological Survey (USGS) from surveys and U.S. Navy air photos, 1960–64. Named by Advisory Committee on Antarctic Names (US-ACAN) for Commander Justin G. Ballou, U.S. Navy, officer in charge of the Detachment A winter party at McMurdo Station, 1966. The mountain lies on the Pennell Coast, a portion of Antarctica lying between Cape Williams Cape Williams () is an ice-covered cape in Antarctica. It is the termination of Buell Peninsula at the east side of the terminus of Lillie Glacier at the lower ends of George Glacier and Zykov Glacier. The peninsula is 15 nautical miles (28 ... and Cape Adare. Mountains of Victoria Land Pennell Coast {{VictoriaLand-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountain Passes 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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
