Marsh Glacier
From Wikipedia, the free encyclopedia
The Marsh Glacier (82°52′S 158°30′E / 82.867°S 158.500°E / -82.867; 158.500Coordinates: 
WikiMiniAtlas82°52′S 158°30′E / 82.867°S 158.500°E / -82.867; 158.500) is a glacier about 110 km (70 mi) long, flowing north from the Antarctic polar plateau between the Miller Range and Queen Elizabeth Range into Nimrod Glacier. Seen by a New Zealand party of the CTAE (1956–58) and named for G.W. Marsh, a member of the party.
See also[]
- List of glaciers in the Antarctic
References[]
Portal:
Geography
Geography
Glaciers | |||||||
|---|---|---|---|---|---|---|---|
| Types |
| ||||||
| Anatomy |
| ||||||
| Processes |
| ||||||
| Measurements |
| ||||||
| Volcanic relations | |||||||
| Landforms |
| ||||||
| |||||||
Glaciers in the Antarctic | |
|---|---|
|
Glaciers of the Ross Dependency | |
|---|---|
| King Edward VII Land |
|
| Ross Dependency |
|
 | This article about a glacier in Shackleton Coast is a stub. You can help Wikipedia by . |
- v
- t
Retrieved from ""
Categories:
- Glaciers of Shackleton Coast
- Ross Dependency glacier stubs
- Shackleton Coast geography stubs
Hidden categories:
- Coordinates on Wikidata
- All stub articles