Black Ridge (Antarctica)
Black Ridge (74°24′S 163°36′E) is a prominent rock ridge in the Deep Freeze Range of Victoria Land, 7 nautical miles (13 km) long and rising to 1,500 metres (5,000 ft), forming a divide between Priestley Glacier and Corner Glacier. It was first explored by the Northern Party of the British Antarctic Expedition, 1910–13, and so named by them because of its appearance.[1]
Further reading
- R. G. Adamson, Granitic rocks of the Campbell—Priestley divide, Northern Victoria Land, Antarctica,New Zealand Journal of Geology and Geophysics, 14:3, 486–503, DOI: 10.1080/00288306.1971.10421943
- PETER OBERHOLZER, CARLO BARONI, JOERG M. SCHAEFER, GIUSEPPE OROMBELLI, SUSAN IVY OCHS, PETER W. KUBIK, HEINRICH BAUR and RAINER WIELER, Limited Pliocene/Pleistocene glaciation in Deep Freeze Range ,northern Victoria Land, Antarctica, derived from in situcosmogenic nuclides, Antarctic Science 15 (4): 493–502 (2003) DOI: 10.1017/S0954102003001603
References
This article incorporates public domain material from "Black Ridge (Antarctica)". Geographic Names Information System. United States Geological Survey.
This article is issued from Wikipedia. The text is licensed under Creative Commons - Attribution - Sharealike. Additional terms may apply for the media files.