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Vertigo Bluff
Vertigo Bluff () is a prominent rock bluff (1,950 m) located 4 nautical miles (7 km) south of Asquith Bluff on the west side of Lennox-King Glacier. Rock samples were collected at the bluff by John Gunner and Henry Brecher of the Ohio State University Geological Expedition Ohio () is a state in the Midwestern region of the United States. Of the fifty U.S. states, it is the 34th-largest by area, and with a population of nearly 11.8 million, is the seventh-most populous and tenth-most densely populated. The sta ..., 1969–70. The name suggested by Gunner reflects the precipitous nature of the bluff face. Cliffs of the Ross Dependency Shackleton Coast {{ShackletonCoast-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Asquith Bluff
Lennox-King Glacier is a large valley glacier, about long, draining Bowden Névé and flowing northeast between the Holland Range and the Queen Alexandra Range of Antarctica to enter Richards Inlet, Ross Ice Shelf. It was named by the 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 ... (1959–60) for Lieutenant Commander James Lennox-King, Royal New Zealand Navy, leader at Scott Base, 1960. See also * Vertigo Bluff References Glaciers of the Ross Dependency Shackleton Coast {{ShackletonCoast-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lennox-King Glacier
Lennox-King Glacier is a large valley glacier, about long, draining Bowden Névé and flowing northeast between the Holland Range and the Queen Alexandra Range of Antarctica to enter Richards Inlet, Ross Ice Shelf. It was named by the New Zealand Geological Survey Antarctic Expedition (1959–60) for Lieutenant Commander James Lennox-King, Royal New Zealand Navy, leader at Scott Base, 1960. See also *Vertigo Bluff Vertigo Bluff () is a prominent rock bluff (1,950 m) located 4 nautical miles (7 km) south of Asquith Bluff on the west side of Lennox-King Glacier Lennox-King Glacier is a large valley glacier, about long, draining Bowden Névé and flowin ... References Glaciers of the Ross Dependency Shackleton Coast {{ShackletonCoast-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
John Gunner (geologist)
John Hugh Gunner (17 May 1884 — 9 August 1918) was an English first-class cricketer and British Army officer. The son of the cricketer Charles Gunner, he was born at Bishops Waltham in May 1884. He was educated at Marlborough College, where he played for a captained the college cricket team. From there he matriculated to Trinity College, Oxford. He represented Trinity College at cricket, but did not progress to play for Oxford University Cricket Club, but did gain a half blue in field hockey. After graduating from Oxford, Gunner became a solicitor and joined the family firm, Gunner & Sons Solicitors, the fifth generation of the family to do so. Gunner was commissioned into the Hampshire Yeomanry as a second lieutenant in May 1905. Gunner played first-class cricket for Hampshire, making his debut against the touring West Indians at Southampton in 1906. He made five further first-class appearances for Hampshire, with three matches in 1906 and two in 1907. He scored 65 runs ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Henry Brecher
Brecher Glacier () is a broad glacier long in the north Churchill Mountains that flows north between the Rundle Peaks and Mandarich Massif into Byrd Glacier. It was named after Henry H. Brecher of the Byrd Polar Research Center, Ohio State University The Ohio State University, commonly called Ohio State or OSU, is a public land-grant research university in Columbus, Ohio. A member of the University System of Ohio, it has been ranked by major institutional rankings among the best publ ...; he conducted Antarctic glaciological investigations for over 30 years, 1960–95, including determinations of surface velocities and elevations on Byrd Glacier. References Glaciers of Oates Land {{OatesLand-glacier-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ohio State University Geological Expedition
Ohio () is a state in the Midwestern region of the United States. Of the fifty U.S. states, it is the 34th-largest by area, and with a population of nearly 11.8 million, is the seventh-most populous and tenth-most densely populated. The state's capital and largest city is Columbus, with the Columbus metro area, Greater Cincinnati, and Greater Cleveland being the largest metropolitan areas. Ohio is bordered by Lake Erie to the north, Pennsylvania to the east, West Virginia to the southeast, Kentucky to the southwest, Indiana to the west, and Michigan to the northwest. Ohio is historically known as the "Buckeye State" after its Ohio buckeye trees, and Ohioans are also known as "Buckeyes". Its state flag is the only non-rectangular flag of all the U.S. states. Ohio takes its name from the Ohio River, which in turn originated from the Seneca word ''ohiːyo'', meaning "good river", "great river", or "large creek". The state arose from the lands west of the Appalachian Moun ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cliffs Of The Ross Dependency
In geography and geology, a cliff is an area of rock which has a general angle defined by the vertical, or nearly vertical. Cliffs are formed by the processes of weathering and erosion, with the effect of gravity. Cliffs are common on coasts, in mountainous areas, escarpments and along rivers. Cliffs are usually composed of rock that is resistant to weathering and erosion. The sedimentary rocks that are most likely to form cliffs include sandstone, limestone, chalk, and dolomite. Igneous rocks such as granite and basalt also often form cliffs. An escarpment (or scarp) is a type of cliff formed by the movement of a geologic fault, a landslide, or sometimes by rock slides or falling rocks which change the differential erosion of the rock layers. Most cliffs have some form of scree slope at their base. In arid areas or under high cliffs, they are generally exposed jumbles of fallen rock. In areas of higher moisture, a soil slope may obscure the talus. Many cliffs also featur ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
