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Mount Finley
Mount Finley () is a prominent mountain, high, on the ridge which extends south from Mount Wade, located south-southwest of Mount Oliver in the Queen Maud Mountains. Mount Finley was named by Rear Admiral Byrd for John H. Finley, President of the American Geographical Society at the time of the Byrd Antarctic Expedition 1928-30. Nearby features Mount Finley is in the northeast of a massif that is bounded by the Yeats Glacier to the north and the McGregor Glacier to the south, both tributaries of the Shackleton Glacier to the west. Other features of the massif, from west to east, are Lockhart Ridge, Pendant Ridge, Simplicity Hill, Crilly Hill, Keel Hill and Bynam Peak. Lockhart Ridge . A conspicuous ridge about long, extending west along the south side of Yeats Glacier and terminating at Shackleton Glacier. Named by the Texas Tech Shackleton Glacier Expedition The Texas Tech Shackleton Glacier Expedition took place first from 1962/63 and then again from 1964/65. The expediti ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Queen Maud Mountains
The Queen Maud Mountains () are a major group of mountains, ranges and subordinate features of the Transantarctic Mountains, lying between the Beardmore Glacier, Beardmore and Reedy Glaciers and including the area from the head of the Ross Ice Shelf to the Antarctic Plateau in Antarctica. Captain Roald Amundsen and his South Pole party ascended Axel Heiberg Glacier near the central part of this group in November 1911, naming these mountains for the Norwegian queen Maud of Wales. Exploration and naming Elevations bordering the Beardmore Glacier, at the western extremity of these mountains, were observed by the British expeditions led by Ernest Shackleton (1907–09) and Robert Falcon Scott (1910-13), but the mountains as a whole were mapped by several American expeditions led by Richard Evelyn Byrd (1930s and 1940s), and United States Antarctic Program (USARP) and New Zealand Antarctic Research Program (NZARP) expeditions from the 1950s through the 1970s. Appearance The ''Sailing ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount Wade
The Prince Olav Mountains () is a mountain group in the Queen Maud Mountains in Antarctica stretching from Shackleton Glacier to Liv Glacier at the head of the Ross Ice Shelf. Discovery and naming The Prince Olav Mountains were discovered in 1911 by Roald Amundsen on the way to the South Pole, and named by him for the then Crown Prince Olav of Norway. Main peaks This range includes the following high mountains and peaks: Location The Prince Olav Mountains extend in a generally northwest – southeast direction between the Shackleton Glacier to the west and the Liv Glacier to the east. The Gabbro Hills and Lillie Range are to the northeast. In the northwest the mountains include the Waldron Spurs, including Nilsen Peak and Mount Orndorff, the Longhorn Spurs, including Cape Surprise, Garden Spur and Olds Peak, and Cathedral Peaks including Mount Kenney, McCuistion Glacier and Lubbock Rudge, all to the west of Barrett Glacier. The Dick Glacier runs west to the Shackleton ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Yeats Glacier
Shackleton Glacier () is a major Antarctic glacier, over long and from wide, descending from the Antarctic Plateau from the vicinity of Roberts Massif and flowing north through the Queen Maud Mountains to enter the Ross Ice Shelf between Mount Speed and Waldron Spurs. Discovered by the United States Antarctic Service (USAS) (1939–41) and named by the Advisory Committee on Antarctic Names (US-ACAN) for Sir Ernest Shackleton, British Antarctic explorer. Course The Shackleton Glacier originates in the East Antarctic Ice Sheet and flows northeast between Dismal Buttress to the northwest and Roberts Massif to the southeast. It is joined from the right (east) by Zaneveld Glacier, which also originates in the ice sheet. Further north it is joined from the right by the Logie Glacier, which flows west through the Cumulus Hills. Flowing north, the Shackleton Glacier is joined from the left (west) by the Gallup Glacier and the Baldwin Glacier and from the right (east) by McGregor ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Texas Tech Shackleton Glacier Expedition
The Texas Tech Shackleton Glacier Expedition took place first from 1962/63 and then again from 1964/65. The expedition, led by F. Alton Wade, was sponsored by Texas Technological College (now Texas Tech University). It explored areas of Antarctica. Exploration Areas explored during and named by the expedition include: * Matador Mountain– Named in honor of the Texas Tech student body, which was originally known as the Matadors. * Red Raider Rampart– Named in honor of the Texas Tech student body, which is now known as the Red Raiders. *Shanklin Glacier– Named in honor of CWO David M. Shanklin, USA, of the U.S. Army Aviation Detachment which supported the expedition. * Ringed Nunatak, named for the ring of moraine that completely surrounds the nunatak. * Shenk Peak– Named in honor of John C. Shenk, who was a Texas Tech graduate student and member of the expedition. *Simplicity Hill– Named because of the ease with which they were able to approach the feature, and because of t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountains Of The Ross Dependency
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 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 Alpine climate, colder climates than at sea level at similar latitude. These colder climates strongly affect the Montane ecosystems, ecosystems of mountains: different elevations have different plants and animals. Because of the less hospitabl ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Dufek Coast
The Dufek Coast is that portion of the coast along the southwest margin of the Ross Ice Shelf between Airdrop Peak on the east side of the Beardmore Glacier and Morris Peak on the east side of Liv Glacier. It was named by the New Zealand Antarctic Place-Names Committee in 1961 after Rear Admiral George J. Dufek, United States Navy, who served under Rear Admiral Richard E. Byrd with the United States Antarctic Service, 1939–41, and as commander of the Eastern Task Force of U.S. Navy Operation Highjump, 1946–47. He was Commander of U.S. Naval Support Force Antarctica, 1954–59, a period in which the following American science stations were established: McMurdo Station, Little America V, Byrd Station, South Pole Station, Wilkes Station, Hallett Station and Ellsworth Station. United States Navy ships, aircraft, and personnel under his command provided broad logistical support to research and survey operations, including aerial photographic missions to virtually all sectors of Antar ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
