Vortex Island
Vortex Island (Lua error in Module:Coordinates at line 489: attempt to index field 'wikibase' (a nil value).) is an island 0.5 nautical miles (0.9 km) long and 245 m high, lying in the northeast part of Prince Gustav Channel about 2 nautical miles (3.7 km) west-southwest of Corry Island, close south of Trinity Peninsula. Islands in this area were first seen by a party under J. Gunnar Andersson of the Swedish Antarctic Expedition, 1901–04. Vortex Island was first charted by the Falkland Islands Dependencies Survey (FIDS) in August 1945. The FIDS survey party was forced to lie idle there by a whirlwind snowstorm, thus suggesting the name.[1]
Geology
[edit | edit source]Vortex Island is composed of Pleistocene volcanic rocks of the James Ross Island Volcanic Group, consisting of a tuya or moberg, which is a volcano erupted under an icecap. Yellow layers are palagonite weathering of steeply dipping ash layers, whereas black layers are basalt flows and pillow basalts.[2][3]
See also
[edit | edit source]References
[edit | edit source]- ^
This article incorporates public domain material from Lua error in Module:Citation/CS1/Configuration at line 2172: attempt to index field '?' (a nil value). Lua error in Module:EditAtWikidata at line 29: attempt to index field 'wikibase' (a nil value).
- ^ Joseph Holliday, Geology Professor, El Camino College
- ^ Lua error in Module:Citation/CS1/Configuration at line 2172: attempt to index field '?' (a nil value).
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