Edge Rewrite
everything Source code View original
// 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: a260af36290fbdc9

Jump to content

Confluence Cone

From Wikipedia, the free encyclopedia

Confluence Cone (68°56′S 66°40′W / 68.933°S 66.667°W / -68.933; -66.667) is a small but conspicuous nunatak 4 nautical miles (7 km) southeast of Sickle Mountain, near the west coast of the Antarctic Peninsula. It was photographed from the air by the Ronne Antarctic Research Expedition in 1947. It was surveyed from the ground by the Falkland Islands Dependencies Survey in 1958, and so named by the UK Antarctic Place-Names Committee because of its position at the confluence of several glaciers which merge with Hariot Glacier to flow into the Wordie Ice Shelf.[1]

References

[edit]
  1. ↑ "Confluence Cone". Geographic Names Information System. United States Geological Survey, United States Department of the Interior. Retrieved 2011-11-21.

Public Domain This article incorporates public domain material from "Confluence Cone". Geographic Names Information System. United States Geological Survey.


Retrieved from "https://en.wikipedia.org/w/index.php?title=Confluence_Cone&oldid=1234103455"