A high-temperature hydrothermal vent field discovered on Puy des Folles Seamount on the Mid-Atlantic Ridge, at approximately 2,000 meters (6,562 feet) in depth, during the In Search of Hydrothermal Lost Cities expedition.
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High-temperature Hydrothermal Vent Field
A high-temperature hydrothermal vent field discovered on Puy des Folles Seamount on the Mid-Atlantic Ridge, at approximately 2,000 meters (6,562 feet) in depth, during the In Search of Hydrothermal Lost Cities expedition.
Credit

Image courtesy of Schmidt Ocean Institute.

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Related Expedition
In Search of Hydrothermal Lost Cities: Searching for Serpentinization-Driven Hydrothermal Activity on Oceanic Core Complexes of the Mid-Atlantic Ridge