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Hydrothermal circulation

Hydrothermal circulation in the oceans is the passage of the water through mid-ocean Ridge (MOR) systems.

The term includes both the circulation of the well known, high temperature vent waters near the ridge crests, and the much lower temperature, diffuse flow of water through sediments and buried basalts further from the ridge crests. The former circulation type is sometimes termed "active", and the later "passive". In both cases the principle is the same: cold dense seawater sinks into the seafloor and is heated at depth whereupon it rises back to the seafloor due to its lesser density. The heat source for the active vents is the newly formed basalt, and, for the highest temperature vents, the underlying magma chamber. The heat source for the passive vents is the still-cooling older basalts. Heat flow studies of the seafloor suggest that basalts within the oceanic crust take millions of years to completely cool as they continue to support passive hydrothermal circulation systems.

Hydrothermal vents are locations on the seafloor where hydrothermal fluids mix into the overlying ocean. Perhaps the best known vent forms are chimneys.

See also: Convection

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