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Serpentinites are curious rocks known for the most part as the source of the major form of asbestos and as ornamental facing stones in architecture. Recent research has indicated that these rocks are important markers of the architecture of the ocean crust, providing vital clues to the processes occurring in the Earth's tectonic plates. This advanced text presents the geological history of the serpentinites. Earth scientists investigating virtually all aspects of mid-ocean ridges, or the tectonic processes of convergent margins which contain serpentinites, will find this a useful reference.