Forlidas Pond

From Wikipedia, the free encyclopedia

Forlidas Pond is a round frozen pond, 100 metres (110 yd) in diameter, lying in a morainal valley east of the north end of Forlidas Ridge, Dufek Massif, Queen Elizabeth Land, Antarctica. The only pond in the northern Pensacola Mountains, it is of much interest to biologists. The pond was discovered and briefly investigated in December 1957 by a United States – International Geophysical Year party from Ellsworth Station. The name is in association with Forlidas Ridge and was suggested by Arthur B. Ford of the United States Geological Survey following geological work in the area, 1978–79.[1]

Antarctic Specially Protected Area

Forlidas Pond, with Davis Valley some 500 m away, and other adjacent ice-free valleys, forms one of the most southerly ‘dry valley’ systems on the continent and has exceptional scientific value for the interpretation of past glacial events and climate in this part of Antarctica. The site is protected under the Antarctic Treaty System as Antarctic Specially Protected Area (ASPA) No.119.[2]

References

  1. ↑ "Forlidas Pond". Geographic Names Information System, U.S. Geological Survey. Retrieved 2012-04-01. 
  2. ↑ "Davis Valley and Forlidas Pond, Dufek Massif". Management Plan for Antarctic Specially Protected Area No. 119: Measure 2, Annex D. Antarctic Treaty Secretariat. 2005. Retrieved 2013-01-24. 

 This article incorporates public domain material from the United States Geological Survey document "Forlidas Pond" (content from the Geographic Names Information System).

Coordinates: 82°27′S 51°21′W / 82.450°S 51.350°W / -82.450; -51.350


This article is issued from Wikipedia. The text is available under the Creative Commons Attribution/Share Alike; additional terms may apply for the media files.