Description
Book SynopsisThis textbook explains how mountains are formed and why there are old and young mountains. It provides a reconstruction of the Earths paleogeography and shows why the shapes of South America and Africa fit so well together. Furthermore, it explains why the Pacific is surrounded by a ring of volcanos and earthquake-prone areas while the edges of the Atlantic are relatively peaceful.
This thoroughly revised textbook edition addresses all these questions and more through the presentation and explanation of the geodynamic processes upon which the theory of continental drift is based and which have led to the concept of plate tectonics.
It is a source of information for students of geology, geophysics, geography, geosciences in general, general natural sciences, as well as professionals, and interested layman.
Table of Contents1. Contractional theory, continental drift and plate tectonics2. Plate movements and their geometric relationships3. Continental graben structures4. Passive continental margins and abyssal plains 5. Mid-ocean ridges6. Hot spots7. Subduction zones, island arcs and active continental maragins8. Transform faults9. Terranes10. Early Precambrian plate tectonics11. Plate tectonics and mountain building12. Old orogens 13. Young orogens - the Earth's loftiest places
