Mount Strybing
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Mount Strybing
Mount Strybing () is a mountain (3,200 m) standing on Owen Ridge 3 nautical miles (6 km) southeast of Mount Craddock in the south part of Sentinel Range, Ellsworth Mountains. It is linked to Mount Craddock by Karnare Col, and surmounts Saltzman Glacier to the northeast, Brook Glacier to the southwest, and Severinghaus Glacier to the west-northwest. The peak was first mapped by the United States Geological Survey (USGS) from surveys and U.S. Navy air photos from 1957 to 1959. It was named by the Advisory Committee on Antarctic Names (US-ACAN) for M/Sgt. Henry Strybing, a United States Marine Corps The United States Marine Corps (USMC), also referred to as the United States Marines, is the maritime land force service branch of the United States Armed Forces responsible for conducting expeditionary and amphibious operations through combi ... (USMC) navigator on reconnaissance flights of R4D aircraft to this region in the 1957–58 season. The R4D aircraft, named "Charg ...
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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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Owen Ridge
Owen Ridge () is a very high and rugged mountain ridge, 22 nautical miles (41 km) long, which forms the southwesternmost element of the Sentinel Range, Ellsworth Mountains. It extends south-southeast from Karnare Col and includes Mount Strybing (3,200 m), Mount Southwick and Lishness Peak, ending up in Bowers Corner. Mapped by United States Geological Survey (USGS) from surveys and U.S. Navy aerial photography, 1957–60. Named by Advisory Committee on Antarctic Names (US-ACAN) (1974) for Thomas B. Owen, Assistant Director of National and International Programs, National Science Foundation. Maps Vinson Massif. Scale 1:250 000 topographic map. Reston, Virginia: US Geological Survey, 1988. Antarctic Digital Database (ADD).Scale 1:250000 topographic map of Antarctica. Scientific Committee on Antarctic Research (SCAR). Since 1993, regularly updated. Features Geographical features include: * Arsela Peak * Bolgrad Glacier * Bowers Corner * Brook Glacier * Karnare Col * Kasil ...
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Mount Craddock
Mount Craddock is a large, bold mountain forming the south extremity of Craddock Massif in Sentinel Range, the ninth highest mountain in Antarctica. It is linked by Karnare Col to Mount Strybing in the southern Sentinel Range. The ninth-highest mountain in Antarctica was first climbed in January 1992. The name Mount Craddock was originally recommended by the Advisory Committee on Antarctic Names (US-ACAN) in 1965 for the present-day Craddock Massif but subsequent maps limited Mount Craddock to the massif's southernmost peak, a position that became established over years. To avoid confusion and to fix the position of the name, US-ACAN redefined Mount Craddock in 2006 to apply to the southernmost peak described above.USGS GNIS The mountain was named by US-ACAN for J. Campbell Craddock (1930–2006), leader of a University of Minnesota expedition (1962–63) that made geological investigations and cartographic surveys in the Sentinel and Heritage Ranges of the Ellsworth Mountain ...
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Sentinel Range
The Sentinel Range is a major mountain range situated northward of Minnesota Glacier and forming the northern half of the Ellsworth Mountains in Antarctica. The range trends NNW-SSE for about and is 24 to 48 km (15 to 30 mi) wide. Many peaks rise over and Vinson Massif (4892 m) in the southern part of the range is the highest elevation on the continent.Sentinel Range.
SCAR Composite Antarctic Gazetteer.
Sentinel Range comprises a main ridge (featuring Vinson Massif in its southern portion) and a number of distinct heights, ridges and mountains on its east side, including (south to north) ,
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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 ...
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Karnare Col
Karnare Col ( bg, седловина Кърнаре, ) is the narrow rocky col of elevation Reference Elevation Model of Antarctica.
Polar Geospatial Center. University of Minnesota, 2019
between the southeast slopes of and the northeast ridge of , linking to

Saltzman Glacier
Saltzman Glacier () is a glacier that drains the north slopes of Mount Allen, the east slopes of Mount Strybing and Karnare Col, and the southeast slopes of Mount Craddock, and flows eastwards between Mount Osborne and Moyher Ridge into Thomas Glacier in southern Sentinel Range, Ellsworth Mountains in Antarctica. Named by US-ACAN (2006) after Eric S. Saltzman, Department of Earth System Science, University of California, Irvine; USAP investigator of Antarctic ice core records of oceanic emissions; chair, 2006, U.S. National Ice Core Working Group for use of Antarctic ice cores for research purposes. 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, climato ... Maps Vinson Massif. Scale 1:250 000 topographic map. Reston, Virgi ...
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Brook Glacier
Brook Glacier () is a glacier that flows westward between Mount Strybing, Mount Allen and Krusha Peak on the west side of Owen Ridge in southern Sentinel Range, Ellsworth Mountains in Antarctica, and joins Bender Glacier east of Chaplin Peak. It was named by the Advisory Committee on Antarctic Names (2006) after Edward J. Brook, Professor of Geosciences, Oregon State University; U.S. Antarctic Project investigator of Antarctic paleoclimate in numerous field seasons from 1988; Chair, U.S. National Ice Core Working Group for use of Antarctic ice cores for research purposes, 2004–05. See also * List of glaciers in the Antarctic * Glaciology Maps Vinson Massif. Scale 1:250 000 topographic map. Reston, Virginia: US Geological Survey, 1988. Antarctic Digital Database (ADD).Scale 1:250000 topographic map of Antarctica. Scientific Committee on Antarctic Research (SCAR). Since 1993, regularly updated. References * External links Brook Glacier.SCAR Composite Antarctic Gazetteer ...
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Severinghaus Glacier
Severinghaus Glacier () is a glacier flowing southwestward from Karnare Col along the north side of Mount Strybing and the south side of Mount Craddock into Bender Glacier in southern Sentinel Range, Ellsworth Mountains in Antarctica. Named by the US-ACAN (2006) after Jeffrey P. Severinghaus, University of Rhode Island Graduate School of Oceanography; USAP researcher from 1996 on the history of the atmosphere, including greenhouse gases, and history of climate changes, using the ice core record. 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, climato ... Maps Vinson Massif. Scale 1:250 000 topographic map. Reston, Virginia: US Geological Survey, 1988. Antarctic Digital Database (ADD).Scale 1:250000 topographic map of Antarctic ...
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United States Geological Survey
The United States Geological Survey (USGS), formerly simply known as the Geological Survey, is a scientific agency of the United States government. The scientists of the USGS study the landscape of the United States, its natural resources, and the natural hazards that threaten it. The organization's work spans the disciplines of biology, geography, geology, and hydrology. The USGS is a fact-finding research organization with no regulatory responsibility. The agency was founded on March 3, 1879. The USGS is a bureau of the United States Department of the Interior; it is that department's sole scientific agency. The USGS employs approximately 8,670 people and is headquartered in Reston, Virginia. The USGS also has major offices near Lakewood, Colorado, at the Denver Federal Center, and Menlo Park, California. The current motto of the USGS, in use since August 1997, is "science for a changing world". The agency's previous slogan, adopted on the occasion of its hundredt ...
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