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Matador Mountain
Matador Mountain () is a prominent, ice-free mountain, high, standing at the south side of the mouth of Gallup Glacier, Antarctica, where the latter enters Shackleton Glacier. It was named by F. Alton Wade, leader of the Texas Tech Shackleton Glacier Expedition (1962–63), as "Matador" is a former name of Texas Tech University's (formerly Texas Technological College Texas Tech University (Texas Tech, Tech, or TTU) is a public research university in Lubbock, Texas. Established on , and called Texas Technological College until 1969, it is the main institution of the five-institution Texas Tech University Sy ...) athletic teams, and all three members of the party were affiliated with the college. References Mountains of the Ross Dependency Dufek Coast {{DufekCoast-geo-stub ...
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Mountain
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 (topography), 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 Monadnock, isolated summits, but most occur in mountain ranges. Mountain formation, Mountains are formed through Tectonic plate, 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 Slump (geology), 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, ecosys ...
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Gallup Glacier
Gallup Glacier () is a broad glacier, about long, flowing east between Mount Rosenwald and Mount Black to enter Shackleton Glacier, Antarctica, just north of Matador Mountain. It was named by the Advisory Committee on Antarctic Names after Commander F.S. Gallup, Jr., U.S. Navy, Commanding Officer of Squadron VX-6 during Operation Deep Freeze 1965. See also * List of glaciers in the Antarctic * Glaciology Glaciology (; ) is the scientific study of glaciers, or more generally ice and natural phenomena that involve ice. Glaciology is an interdisciplinary Earth science that integrates geophysics, geology, physical geography, geomorphology, c ... References Glaciers of Dufek Coast {{DufekCoast-glacier-stub ...
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Shackleton Glacier
Shackleton Glacier is a major Antarctica, Antarctic glacier, over long and from 8 to 16 km (5 to 10 mi) wide, descending from the polar 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. The Roberts Zealand GSAE (1961–62), who named it for A.R. Roberts, leader at Scott Massif is a remarkable snow-free massif exceeding 2,700 metres (8,860 ft) and about 155 km2 (60 sq mi) in area. It was by the Southern Party of New United States Antarctic Program, USAS (1939–41) and named by US-SCAN for Sir Ernest Shackleton, Anglo-Irish people, Anglo-Irish Antarctic explorer. See also * List of glaciers in the Antarctic * Mount Greenlee References

* * Queen Maud Mountains Glaciers of Dufek Coast {{DufekCoast-glacier-stub ...
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Franklin Alton Wade
Franklin Alton Wade (1903-1978) was an American geologist. One of his chief scientific interests was the geology of Antarctica, to which he traveled several times, including twice with the explorer Admiral Richard E. Byrd. Early life Wade was born in Akron, Ohio in 1903. He received Bachelor of Science and Master of Arts degrees at the same ceremony in 1926, from Kenyon College in Ohio. After working for a short time as an industrial chemist, he enrolled in a PhD programme at Johns Hopkins University. Career Antarctic expeditions and research Wade was a member of the second Antarctic expedition led by the Admiral Richard E. Byrd in 1933. While there, he was part of a 77-day sled journey into Marie Byrd Land. The field work on this expedition was later the foundation of his doctoral dissertation. Wade was then selected by Byrd to take the role of chief scientist for his third Antarctic expedition. On this expedition he took two students with him, a practice he would contin ...
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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 Shenk Peak is a 2,540 m high Summit (topography), peak standing just southeast of Mount Kenyon between Gillespie Glacier and LaPrade Valley in the Cumulus Hills. It was named by the Texas Tech Shackleton Glacier Expe ...
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Texas Tech University
Texas Tech University (Texas Tech, Tech, or TTU) is a public research university in Lubbock, Texas. Established on , and called Texas Technological College until 1969, it is the main institution of the five-institution Texas Tech University System. The university's student enrollment is the sixth-largest in Texas as of the Fall 2020 semester. As of fall 2020, there were 40,322 students (33,269 undergraduate and 7,053 graduate) enrolled at Texas Tech. With over 25% of its undergraduate student population identifying as Hispanic, Texas Tech University is a designated Hispanic-serving institution (HSI). The university offers degrees in more than 150 courses of study through 13 colleges and hosts 60 research centers and institutes. Texas Tech University has awarded over 200,000 degrees since 1927, including over 40,000 graduate and professional degrees. Texas Tech is classified among "R1: Doctoral Universities – Very high research activity." Research projects in the areas o ...
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History Of Texas Tech University
The history of Texas Tech University dates back to the early 1880s, but the university was not established until 1923. Establishment The call to open a college in West Texas began shortly after the arrival of settlers in the area in the 1880s. In 1917, the Texas legislature passed a bill creating a branch of Texas A&M to be located in Abilene. However, the bill was repealed two years later during the next session after it was discovered that Governor James E. Ferguson had falsely reported the site committee's choice of location. After new legislation passed in the state house and senate in 1921, Governor Pat Neff vetoed it, citing hard financial times in West Texas. Furious about Neff's veto, some in West Texas went so far as to recommend that West Texas secede from the state. In 1923, the legislature decided that, rather than a branch campus, an entirely new university would better serve the needs of the region. On February 10, 1923, Neff signed the legislation creating Texas ...
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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 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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