|Plate Tectonics: The Mechanism|
This text explains how detailed mapping of the ocean floor led scientists like Howard Hess and R. Deitz to revive the Holmes convection theory. Hess and Deitz modified the theory considerably and called their new theory Sea-floor Spreading. Among the seafloor features that supported the sea-floor spreading hypothesis were: mid-oceanic ridges, deep sea trenches, island arcs, geomagnetic patterns, and fault patterns. These features are treated in detail and related to the current Theory of Plate Tectonics.
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Copyright 1996-2000 by The Museum of Paleontology of The University of California, Berkeley; the Regents of the University of California; and The Paleontological Society. No part of the referring document residing on the server may be reproduced or stored in a retrieval system without prior written permission of the publisher, except for educational purposes, and in no case for profit.
DLESE Catalog ID: DLESE-000-000-005-213
This resource is part of 'Geology: Plate Tectonics'
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