Mid-Ocean Ridges

Mid-Ocean Ridges

Editor(s): C.R. German, J. Lin, L.M. Parson

Published Online: 19 MAR 2013

Print ISBN: 9780875904139

Online ISBN: 9781118665879

DOI: 10.1002/9781118665879

About this Book

Published by the American Geophysical Union as part of the Geophysical Monograph Series, Volume 148.

Mid-ocean ridges play an important role in the plate-tectonic cycle of our planet. Extending some 50-60,000 km across the ocean-floor, the global mid-ocean 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 mid-ocean 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 mid-ocean ridges is influenced by a convective process: hydrothermal circulation.

Table of contents

    1. You have free access to this content
    2. Submarine Lava Flow Emplacement at the East Pacific Rise 9°50´N: Implications for Uppermost Ocean Crust Stratigraphy and Hydrothermal Fluid Circulation (pages 187–217)

      Daniel Fornari, Maurice Tivey, Hans Schouten, Michael Perfit, Dana Yoerger, Al Bradley, Margo Edwards, Rachel Haymon, Daniel Scheirer, Karen Von Damm, Timothy Shank and Adam Soule

    3. Vigorous Venting and Biology at Pito Seamount, Easter Microplate (pages 305–318)

      D. F. Naar, R. Hekinian, M. Segonzac, J. Francheteau, R. Armijo, J.-P. Cogne, M. Constantin, J. Girardeau, R. N. Hey and R. C. Searle

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