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This book gives an historical perspective of plate tectonics. Furthermore, it discusses the foundations of rigid plate tectonics and the limitations of this approach. This classic approach can explain the data to a level of 95 % precision. Some anomalies subsit which must be explained by a more general model. The authors refer to these anomalies: for example discrepancies between spatial geodetical data and rigid kinematics in oceans or rheology significance of fractal dimensions in seismicity and faulting, etc. In this unique book the reader has access to data as well as to interpretations from a broad spectrum of disciplines. Great emphasis is placed on the limitations of the rigid plate tectonics theory of the earth.§