Introduction to "The ABC's of Plate Tectonics"
The Basics of Plate Tectonics
Buoyancy and Floating Continents
Sedimentation and Continental Growth
When Continents Collide
The Mechanism of Plate Tectonics
The Formation of Pangaea: The Making of a Supercontinent
Earth Sciences Home Page
The Theory of Continental Drift has had a long and turbulent history since it was first proposed by Alfred Wegener in 1910. Vigorously challenged yet widely ignored, the theory languished for half a century, primarily due to its lack of a plausible mechanism to support the proposed drift. With the discovery of sea-floor spreading in the late 1950's and early 60's, the idea was reinvigorated, this time as the Theory of Plate Tectonics.
Plate tectonics is now almost universally accepted, its mechanisms plausible and to a degree demonstrable. However, many details of the mechanism are yet to be worked out, and many theories involving various details of plate tectonics rest on some questionable assumptions. This set of pages attempts to define some of the basic principles of the mechanism, and to examine their effect on the creation of landforms.
What follows is NOT a summary of the current thinking about plate tectonics and its mechanisms; rather, many new, and probably highly controversial, ideas are presented for consideration. What IS presented is a broad analysis of the basic principles that should apply to the movements of plates, some new hypotheses about how they apply to convection and landform formation, and some expected scenarios for differing tectonic events.
For those unfamiliar with the theory of plate tectonics, a separate page - The Basics of Plate Tectonics - is provided. This summary offers a brief condensation of the basic principles of Plate Tectonics. A much more comprehensive explanation of Plate Tectonics can be found on the USGS Web Site.