Edge Rewrite
// HTMLRewriter · presentation

This page was redesigned at the edge.

Cloudflare fetched the original article and streamed it through HTMLRewriter to apply an entirely new visual system without rebuilding the source page.

// request.cf · coarse context

A page that knows where it met you.

Only coarse request metadata is shown. This demo does not display or persist visitor IP addresses.

Country
US
Cloudflare location
CMH
Connection
HTTP/2
Language
Not provided

Ray ID: a22e1637cf97cc36

Jump to content

Vortex Island

Vortex Island (63°44′S 57°38′W / 63.733°S 57.633°W / -63.733; -57.633) 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]

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]

References

[edit]
  1. Public Domain This article incorporates public domain material from "Vortex Island". Geographic Names Information System. United States Geological Survey.  Edit this at Wikidata
  2. Joseph Holliday, Geology Professor, El Camino College
  3. "Geological Map of James Ross Island" (PDF). Retrieved 23 March 2020.