Crevasse Valley Glacier [SEP] continent
Crevasse Valley Glacier
Crevasse Valley Glacier () is a broad glacier about long, flowing west-southwest between the Chester Mountains and the Saunders Mountain to the Sulzberger Ice Shelf in Marie Byrd Land, Antarctica. It was discovered by a sledging party of the Byrd Antarctic Expedition, which visited this area in November–December 1934, and so named because of its extensively crevassed surface.
See also.
- List of glaciers in the Antarctic
- Glaciology
on offer at the pass. Descend to Khalting side is steep, initially scree and then ice, and might require rappelling. At the base of the descent, a 1–2-metre-wide crevasse runs end to end, and there are a couple of snow bridges. After descend, it is a long roped walk through crevasse infested Khatling glacier. At Khatling Glacier Camp site, there is a small patch of stones, but camping on glacier ice is also possible. Camp site also offers amazing views of virgin unknown pass and valley