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Blood Falls, Antarctica Blood Falls is an outflow of an iron oxide-tainted plume of saltwater, occurring at the tongue of the Taylor Glacier onto the ice-covered surface of West Lake Bonney in the Taylor Valley of the McMurdo Dry Valleys in Victoria Land, East Antarctica. The concentration of rust originates from a rare microbial colony that was sealed off for around 2 million years.
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Posted by Nova on February 11, 2011 at 9:13 am
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