Bermel Escarpment
The Bermel Escarpment is a snow and rock escarpment, 15 nautical miles (28 km) long, extending from the base of the Ford Massif to King Peak, in the Thiel Mountains. The escarpment drops 300 to 400 metres (1,000 to 1,300 ft) from the polar plateau to the ice surface north of these mountains. At its base sits Drake Nunatak. It was named by the Advisory Committee on Antarctic Names after , a cartographer with the United States Geological Survey (USGS). Bermel was co-leader (with ) of the USGS Thiel Mountains party which surveyed the mountains in 1960–61, and also leader of USGS Topo East and Topo West, 1962–63, in which geodetic control was extended from the area of Cape Hallett to the Wilson Hills (Topo West), and from the foot of Beardmore Glacier through the Horlick Mountains (Topo East).[1]
See also[]
Further reading[]
- Gunter Faure, Teresa M. Mensing, The Transantarctic Mountains: Rocks, Ice, Meteorites and Water, P 228
References[]
- ^ "Bermel Escarpment". Geographic Names Information System. United States Geological Survey. Retrieved 2011-06-09.
This article incorporates public domain material from the United States Geological Survey document: "Bermel Escarpment". (content from the Geographic Names Information System)
Coordinates: 85°17′S 89°30′W / 85.283°S 89.500°W
- Escarpments of Antarctica
- Ellsworth Land geography stubs