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Sørsdal Glacier () is a heavily
Sørsdal Glacier () is a heavily 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 pie ...
d glacier on the Ingrid Christensen Coast
The Ingrid Christensen Coast is that portion of the coast of Antarctica lying between Jennings Promontory, in 72°33′E, and the western end of the West Ice Shelf in 81°24′E. It is located in the western half of Princess Elizabeth Land, just e ...
of Princess Elizabeth Land
Princess Elizabeth Land is the sector of Antarctica between longitude 73° east and Cape Penck (at 87°43' east). The sector is claimed by Australia as part of the Australian Antarctic Territory, although this claim is not widely recognized.
Ge ...
in Antarctica
Antarctica () is Earth's southernmost and least-populated continent. Situated almost entirely south of the Antarctic Circle and surrounded by the Southern Ocean, it contains the geographic South Pole. Antarctica is the fifth-largest contine ...
, long, flowing westward along the south side of Krok Fjord and the Vestfold Hills
The Vestfold Hills are rounded, rocky, coastal hills, in extent, on the north side of Sorsdal Glacier on the Ingrid Christensen Coast of Princess Elizabeth Land, Antarctica. The hills are subdivided by three west-trending peninsulas bounded by na ...
and terminating in a prominent glacier tongue at Prydz Bay
Prydz Bay is a deep embayment of Antarctica between the Lars Christensen Coast and Ingrid Christensen Coast. The Bay is at the downstream end of a giant glacial drainage system that originates in the East Antarctic interior. The Lambert Glacie ...
. Discovered in February 1935 by a Norwegian expedition under Captain Klarius Mikkelsen and named for Lief Sørsdal, a Norwegian dentist and a member of the party from the whaling ship ''Thorshavn'' that landed at the northern end of the Vestfold Hills.
The Sørsdal Glacier Tongue () is the prominent seaward extension of Sørsdal Glacier into Prydz Bay
Prydz Bay is a deep embayment of Antarctica between the Lars Christensen Coast and Ingrid Christensen Coast. The Bay is at the downstream end of a giant glacial drainage system that originates in the East Antarctic interior. The Lambert Glacie ...
.
See also
*List of glaciers in the Antarctic
There are many glaciers in the Antarctic. This set of lists does not include ice sheets, ice caps or ice fields, such as the Antarctic ice sheet, but includes glacial features that are defined by their flow, rather than general bodies of ice. Th ...
* 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 ...
References
* Glaciers of Ingrid Christensen Coast {{Antarctica-glacier-stub