Cathedral Peaks
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Cathedral Peaks
The Cathedral Peaks () form a rugged mountain mass surmounted by several conspicuous peaks, located north of Lubbock Ridge and extending for about along the eastern margin of Shackleton Glacier. From the glacier the peaks resemble the spires and turrets of a cathedral. They were named by F. Alton Wade, who worked in this area as leader of the Texas Tech 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 Sys ... Shackleton Glacier Party, 1962–63. References Mountains of the Ross Dependency Dufek Coast {{DufekCoast-geo-stub ...
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Lubbock Ridge
The Prince Olav Mountains is a mountain range of the Queen Maud Mountains in Antarctica stretching from Shackleton Glacier to Liv Glacier at the head of the Ross Ice Shelf. 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. Key mountains This range includes the following mountains and peaks: Allaire Peak Allaire Peak is a rock peak standing northwest of Mount Hall, between the Gough and Le Couteur Glaciers. Named by Advisory Committee on Antarctic Names (US-ACAN) for Captain C.J. Allaire, USA, on the Staff of the Commander, U.S. Naval Support Force, Antarctica, during U.S. Navy Operation Deep Freeze 1963. Mount Campbell Mount Campbell is a prominent peak standing southeast of Mount Wade. Discovered and photographed by the USAS (1939–41), and surveyed by A.P. Crary (1957–58). Named by Crary for Joel Campbell of the U.S. Coast and Geodetic Survey, Antarctic Project Leader for geomagnetic oper ...
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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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Cathedral
A cathedral is a church that contains the '' cathedra'' () of a bishop, thus serving as the central church of a diocese, conference, or episcopate. Churches with the function of "cathedral" are usually specific to those Christian denominations with an episcopal hierarchy, such as the Catholic, Eastern Orthodox, Anglican, and some Lutheran churches.New Standard Encyclopedia, 1998 by Standard Educational Corporation, Chicago, Illinois; page B-262c Church buildings embodying the functions of a cathedral first appeared in Italy, Gaul, Spain, and North Africa in the 4th century, but cathedrals did not become universal within the Western Catholic Church until the 12th century, by which time they had developed architectural forms, institutional structures, and legal identities distinct from parish churches, monastic churches, and episcopal residences. The cathedral is more important in the hierarchy than the church because it is from the cathedral that the bishop governs the area unde ...
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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
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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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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