Shinnan Glacier (, ''Shinnan Hyoga'') is a
glacier
A glacier (; or ) is a persistent body of dense ice, a form of rock, that is constantly moving downhill under its own weight. A glacier forms where the accumulation of snow exceeds its ablation over many years, often centuries. It acquires ...
which flows northwest to the coast just east of
Shinnan Rocks and marks the division between
Queen Maud Land
Queen Maud Land () is a roughly region of Antarctica Territorial claims in Antarctica, claimed by Norway as a dependent territory. It borders the claimed British Antarctic Territory 20th meridian west, 20° west, specifically the Caird Coast, ...
and
Enderby Land
Enderby Land is a projecting landmass of Antarctica. Its shore extends from Shinnan Glacier at about to William Scoresby Bay at , approximately of the earth's longitude (planets), longitude. It was first documented in western and eastern liter ...
. Mapped from surveys and air photos by
Japanese Antarctic Research Expedition (JARE), 1957–62, and named Shinnan Hyōga (new south glacier).
See also
*
Kakure Rocks, rocky exposures along the east wall of Shinnan Glacier
*
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 ...
*
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, clim ...
References
Glaciers of Queen Maud Land
Prince Olav Coast
{{QueenMaudLand-glacier-stub