Socks Glacier is a small
glacier
A glacier (; ) is a persistent body of dense ice that is constantly moving under its own weight. A glacier forms where the accumulation of snow exceeds its ablation over many years, often centuries. It acquires distinguishing features, such as ...
descending the east slopes of
Queen Alexandra Range
The Queen Alexandra Range is a major mountain range of the Transantarctic Mountains System, located in the Ross Dependency region of Antarctica.
It is about long, bordering the entire western side of Beardmore Glacier from the Polar Plateau to ...
just north of
Owen Hills to enter the west side of
Beardmore Glacier.
Gazetteer of the Antarctic : names approved by the United States Board on Geographic Names
retrieved 1 August 2012 Discovered by the British Antarctic Expedition (1907–09) and named for one of the ponies taken with the South Pole Party. Socks, the last pony
A pony is a type of small horse ('' Equus ferus caballus''). Depending on the context, a pony may be a horse that is under an approximate or exact height at the withers, or a small horse with a specific conformation and temperament. Compared ...
to survive the journey, fell into a 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 ...
on 7 December 1908, on Beardmore Glacier near Socks Glacier.
See also
* List of glaciers in the Antarctic
References
Glaciers of the Ross Dependency
Shackleton Coast
{{ShackletonCoast-geo-stub