Ocean Science for Everyone

Hydrothermal Vents and Volcanoes

Learn About Vents and Volcanoes

Most of the active volcanoes on Earth are located underwater. Most commonly occurring along tectonic spreading centers, submarine eruptions release molten rock from below the seafloor. On the other hand, hydrothermal vents are the result of sea water percolating down through fissures in the ocean crust near spreading centers or subduction zones. The cold seawater is heated by hot magma, and reemerges to form the vents. Despite being in areas with no light for sunlight-driven food production, extinct, and even mildly active, volcanoes and vent sites often support diverse communities of animals that have adapted to produce food using chemical energy, via a process known as chemosynthesis.

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Hydrothermal Vents and Volcanoes

Rocky Ridge
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A rocky ridge of mainly intact fragmented pillow flows heavily covered in corals and sponges (and a photobombing False Boarfish), seen during the second Voyage to the Ridge 2022 expedition.

Small Volcanic Pillow Mound
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Remotely operated vehicle Deep Discoverer images an outcrop that may have been a small volcanic pillow mound with elongate pillow lobes during the second Voyage to the Ridge 2022 expedition. The mound provided habitat for a variety of organisms, including corals and sponges.

High-Temperature Hydrothermal Vent Field
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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. Image courtesy of Schmidt Ocean Institute.

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