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Hydrothermal vents in oceans are closely associated with regions of
Mid-oceanic ridges
Intersection of continental plates
Areas of sea floor spreading
All of the above
Hydrothermal vents are globally distributed, but their location is determined by tectonic conditions where sea water meets magma. • Where plates form, such as mid-oceanic ridges and in areas where there is volcanic activity, the Earth’s magma is close to the seafloor and can heat water which has seeped down. • The hydrothermal vents are therefore associated with regions of high tectonic activity and intersections of continental plates
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