Title
MidOcean Ridges: Hydrothermal Interactions Between the Lithosphere and Oceans (Geophysical Monograph Series),Used
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Published by the American Geophysical Union as part of the Geophysical Monograph Series, Volume 148.Midocean ridges play an important role in the platetectonic cycle of our planet. Extending some 5060,000 km across the oceanfloor, the global midocean ridge system is the site of creation of the oceanic crust and lithosphere that covers more than two thirds of the Earth's exterior. Approximately 75% of Earth's total heat flux occurs through oceanic crust, much of it at midocean ridges through complex processes associated with magma solidification, heat transfer, and cooling of young oceanic lithosphere. While the majority of this heat loss occurs through conduction, approximately one third of the total heat loss at midocean ridges is influenced by a convective process: hydrothermal circulation.
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