Lost City Expedition 2005

Lost City Expedition 2005. Serpentinized peridotites are the most dominant rock type recovered during past expeditions on the south wall of the Atlantis Massif and form the basement of the Lost City hydrothermal vent field. This outcrop has partially deformed rocks that occur at the top of the massif. The arm of the submersible Alvin is shown on the right.

Photo Category: Ocean exploration

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Author: NOAA

License: Public Domain Mark 1.0 (Public domain)

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Added On	16th October 2015
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