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Bowie Crevasse Field
Bowie Crevasse Field is a large crevasse field at a break in slope on the Minnesota Glacier between the southeast end of the Bastien Range and Anderson Massif in the Ellsworth Mountains of Antarctica. It was named by the University of Minnesota The University of Minnesota, formally the University of Minnesota, Twin Cities, (UMN Twin Cities, the U of M, or Minnesota) is a public university, public Land-grant university, land-grant research university in the Minneapolis–Saint Paul, Tw ... Ellsworth Mountains Party, 1962–63, for Glenn E. Bowie, geophysicist with the party. References * Crevasse fields of Antarctica Bodies of ice of Ellsworth Land {{EllsworthLand-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Crevasse
A crevasse is a deep crack, that forms in a glacier or ice sheet that can be a few inches across to over 40 feet. Crevasses form as a result of the movement and resulting stress associated with the shear stress generated when two semi-rigid pieces above a plastic substrate have different rates of movement. The resulting intensity of the shear stress causes a breakage along the faces. Description Crevasses often have vertical or near-vertical walls, which can then melt and create seracs, arches, and other ice formations. These walls sometimes expose layers that represent the glacier's stratigraphy. Crevasse size often depends upon the amount of liquid water present in the glacier. A crevasse may be as deep as 45 metres and as wide as 20 metres. by |
Minnesota Glacier
Minnesota Glacier () is a broad glacier, about long and wide, flowing east through the Ellsworth Mountains in Antarctica, separating the Sentinel Range and the Heritage Range. It is nourished by ice from the plateau west of the mountains and by Nimitz Glacier and Splettstoesser Glacier, and merges into the larger Rutford Ice Stream at the eastern margin of the Ellsworth Mountains. The glacier was named by the Advisory Committee on Antarctic Names for the University of Minnesota, Twin Cities, which sent research parties to the Ellsworth Mountains in 1961–62, 1962–63 and 1963–64. Tributary glaciers * Splettstoesser Glacier * Gowan Glacier * Webster Glacier * Nimitz Glacier * Wessbecher Glacier * Hudman Glacier * Carey Glacier 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 integ ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bastien Range
The Bastien Range () is an Antarctic mountain range of moderate height which extends in a NW-SE direction for about , flanking the SW side of Nimitz Glacier and the Sentinel Range, in the Ellsworth Mountains. Named by US-ACAN for Thomas W. Bastien, geologist, leader of the helicopter supported University of Minnesota Geological Party to these mountains, 1963–64. Bastien was also a member of a party to the Ellsworth Mountains in 1961–62. Features Geographical features include: * Bergison Peak * Bowie Crevasse Field * Camp Hills * Ereta Peak * Hodges Knoll * Karasura Glacier * Klenova Peak * Mount Fisek * Mount Klayn * Nimitz Glacier * O'Neal Nunataks * Patmos Peak * Wild Knoll Wild Knoll ( bg, могила Уайлд, mogila Uajld, ) is the peak rising to 1773 m [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Anderson Massif
The Anderson Massif is a prominent ice-covered massif about across and rising to a height of , located at the junction of Splettstoesser Glacier and Minnesota Glacier in the Heritage Range of the Ellsworth Mountains, Antarctica. It was named by the Advisory Committee on Antarctic Names for John J. Anderson, a geologist who was field leader of the University of Minnesota Ellsworth Mountains Party, 1961–62. See also * Mountains in Antarctica Geographical features include: * Bowie Crevasse Field * Grimes Glacier * Huggler Peak * Minnesota Glacier * Rullman Peak * Siefker Ridge * Splettstoesser Glacier Splettstoesser Glacier () is a glacier, long, draining from the plateau just south of Founders Escarpment and flowing east-northeast through the Heritage Range to the south of Founders Peaks and Anderson Massif to enter the Minnesota Glacier. ... References Mountains of Ellsworth Land {{EllsworthLand-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ellsworth Mountains
The Ellsworth Mountains are the highest mountain ranges in Antarctica, forming a long and wide chain of mountains in a north to south configuration on the western margin of the Ronne Ice Shelf in Marie Byrd Land. They are bisected by Minnesota Glacier to form the Sentinel Range to the north and the Heritage Range to the south. The former is by far the higher and more spectacular with Mount Vinson () constituting the highest point on the continent.Bockheim, J.G., Schaefer, C.E., 2015. ''Soils of Ellsworth Land, the Ellsworth Mountains''. In: Bockheim, J.G. (Ed.), ''The Soils of Antarctica. World Soils Book Series'', Springer, Switzerland, pp. 169–181. The mountains are located within the Chilean Antarctic territorial claim but outside of the Argentinian and British ones. Discovery The mountains were discovered on November 23, 1935, by Lincoln Ellsworth in the course of a trans-Antarctic flight from Dundee Island to the Ross Ice Shelf. He gave them the descriptive name Sentinel ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
University Of Minnesota
The University of Minnesota, formally the University of Minnesota, Twin Cities, (UMN Twin Cities, the U of M, or Minnesota) is a public university, public Land-grant university, land-grant research university in the Minneapolis–Saint Paul, Twin Cities of Minneapolis and Saint Paul, Minnesota, United States. The Twin Cities campus comprises locations in Minneapolis and Falcon Heights, Minnesota, Falcon Heights, a suburb of St. Paul, approximately apart. The Twin Cities campus is the oldest and largest in the University of Minnesota system and has the List of United States university campuses by enrollment, ninth-largest main campus student body in the United States, with 52,376 students at the start of the 2021–22 academic year. It is the Flagship#Colleges and universities in the United States, flagship institution of the University of Minnesota System, and is organized into 19 colleges, schools, and other major academic units. The Minnesota Territorial Legislature drafted a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Crevasse Fields Of Antarctica
A crevasse is a deep crack, that forms in a glacier or ice sheet that can be a few inches across to over 40 feet. Crevasses form as a result of the movement and resulting stress associated with the shear stress generated when two semi-rigid pieces above a plastic substrate have different rates of movement. The resulting intensity of the shear stress causes a breakage along the faces. Description Crevasses often have vertical or near-vertical walls, which can then melt and create seracs, arches, and other ice formations. These walls sometimes expose layers that represent the glacier's stratigraphy. Crevasse size often depends upon the amount of liquid water present in the glacier. A crevasse may be as deep as 45 metres and as wide as 20 metres. by |
