Koski Glacier
Koski Glacier (85°17′S 167°15′E) is an east-flowing glacier, 7 nautical miles (13 km) long, draining the east-central portion of the Dominion Range icecap, Antarctica. The glacier lies close north of Vandament Glacier, whose flow it parallels, and terminates at Mill Glacier just southeast of Browns Butte. It was named by the Advisory Committee on Antarctic Names for Raymond J. Koski, a United States Antarctic Research Program engineer on several traverses originating at the South Pole Station 1962–63, 1963–64 and 1964–65.[1]
References
- "Koski Glacier". Geographic Names Information System. United States Geological Survey. Retrieved 2013-05-16.
Types |
| ||||||
---|---|---|---|---|---|---|---|
Anatomy |
| ||||||
Processes | |||||||
Measurements | |||||||
Volcanic relations | |||||||
Landforms |
| ||||||
|
This article is issued from Wikipedia. The text is licensed under Creative Commons - Attribution - Sharealike. Additional terms may apply for the media files.