Vanderford Valley
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Vanderford Valley
Vanderford Valley (Other English names: Vanderford Strath, Vanderford Submarine Valley Hungarian '' Vanderford-selfvölgy'') () is an undersea valley, named in association with the Vanderford Glacier Vanderford Glacier () is a glacier about 8 km (5 mi) wide flowing northwest into the southeast side of Vincennes Bay, slightly south of the Windmill Islands. It was named by the Advisory Committee on Antarctic Names (US-ACAN) for Ben ..., which reaches a depth of 2287 m (7,503 ft). This may be the deepest glacier-carved valley in the world. External linksGlacial geomorphology Valleys of Antarctica Landforms of Wilkes Land {{WilkesLand-geo-stub ...
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Undersea Valley
The underwater environment is the region below the surface of, and immersed in, liquid water in a natural or artificial feature (called a body of water), such as an ocean, sea, lake, pond, reservoir, river, canal, or aquifer. Some characteristics of the underwater environment are universal, but many depend on the local situation. Liquid water has been present on Earth for most of the history of the planet. The underwater environment is thought to be the place of the origin of life on Earth, and it remains the ecological region most critical to the support of life and the natural habitat of the majority of living organisms. Several branches of science are dedicated to the study of this environment or specific parts or aspects of it. A number of human activities are conducted in the more accessible parts of the underwater environment. These include research, underwater diving for work or recreation, and underwater warfare with submarines. It is hostile to humans in m ...
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Vanderford Glacier
Vanderford Glacier () is a glacier about 8 km (5 mi) wide flowing northwest into the southeast side of Vincennes Bay, slightly south of the Windmill Islands. It was named by the Advisory Committee on Antarctic Names (US-ACAN) for Benjamin Vanderford, pilot of the sloop of war Vincennes of the United States Exploring Expedition under Captain Wilkes, 1838–42. The glacier was mapped from aerial photographs taken by U.S. Navy Operation Highjump, 1946–47. 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 ... * Vanderford Valley References * Glaciers of Wilkes Land {{WilkesLand-glacier-stub ...
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Valleys Of Antarctica
A valley is an elongated low area often running between hills or mountains, which will typically contain a river or stream running from one end to the other. Most valleys are formed by erosion of the land surface by rivers or streams over a very long period. Some valleys are formed through erosion by glacial ice. These glaciers may remain present in valleys in high mountains or polar areas. At lower latitudes and altitudes, these glacially formed valleys may have been created or enlarged during ice ages but now are ice-free and occupied by streams or rivers. In desert areas, valleys may be entirely dry or carry a watercourse only rarely. In areas of limestone bedrock, dry valleys may also result from drainage now taking place underground rather than at the surface. Rift valleys arise principally from earth movements, rather than erosion. Many different types of valleys are described by geographers, using terms that may be global in use or else applied only locally. ...
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