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Blood Falls 01 Medium Res photolibrary.usap.gov
 

 

 

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Description
English: Blood Falls seeps from the end of the Taylor Glacier into Lake Bonney. The tent at left provides a sense of scale for just how big the phenomenon is. The phenomenon is due to leaks from a reservoir of ancient saltwater buried under the glacier. Ferrous ions dissolved in the water oxidize on contact with the atmosphere, and precipitate as insoluble reddish ferric salts.
Français : Coulée ferreuse à travers le glacier du lac Bonney.
Date 26 November 2006(2006-11-26)
Source usap.gov
Transferred from en.wikipedia to Commons by User:João Sousa
Author Peter Rejcek
Permission
(Reusing this file)

US Antarctic Program, National Science Foundation

Licensing

Public domain This work is in the public domain in the United States because it is a work of the United States Federal Government under the terms of Title 17, Chapter 1, Section 105 of the US Code. See Copyright.

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The original description page is/was here. All following user names refer to en.wikipedia.

  • 2009-04-17 18:47 Shinkolobwe 2968×1740× (3948891 bytes) High resolution version. Blood Falls seeps from the end of the Taylor Glacier into Lake Bonney. The tent at left provides a sense of scale for just how big the phenomenon is. Scientists believe a buried saltwater reservoir is partly responsible for the
  • 2009-04-17 18:38 Shinkolobwe 450×264× (47624 bytes) N:\USERS\PDCANNIE\Presentations\Interesting Figures\Biology{{Information | Description = Blood Falls seeps from the end of the Taylor Glacier into Lake Bonney. The tent at left provides a sense of scale for just how big the phenomenon is. Scientists be


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EXIF data:
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Date and time original image was generated 2006:11:26 16:28:11
Date and time image was made digital data 2006:11:26 16:28:11
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