S13-51-2341
Flight 41C; 23N, 38.5E, 7 April 1984
Photographs of the Red Sea frequently provide images of surface debris that
appears similar to that observed on Persian Gulf and Gulf of Oman waters.
The material lacks the iridescent colors of petroleum slicks, however, indicating
the natural (biological) origin of the slicks. The Red Sea has a great population
of plankton, such that at times the sea surface is reddish colored; thence the name
of the sea. The massive plankton blooms produce such quantities of natural debris
that wave action causes it to form into concentrated broad areas, as in the view
photographed from the Challenger in April 1984.
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