Overview
Syllabus
Continental Drift: An Idea Before Its Time
Pangaea 200 Million Years Ago
Similar Fossils on Different Continents
Continental Drift: Supporting Evidence
The Great Debate
The Theory of Plate Tectonics
Earth's Lithospheric Plates
Three Types of Plate Boundaries
Divergent Plate Boundary
Mid-ocean ridge system
Iceland: Mid-ocean ridge
Divergent Plate Boundaries
Continental Rifting
Convergent Plate Boundaries & Subduction
Oceanic-Continental Convergence
Continent-Continent Convergence
Plate Boundaries • Transform fault boundaries - Plates slide past one another
Changing Plate Boundaries
Deep-Sea Drilling
Hot Spots and Hot Spot Tracks
Testing the Plate Tectonics Model
Polar wandering paths for Eurasia and North America
Magnetic Reversals and Seafloor Spreading
Ocean Floor as a Magnetic Recorder
Heat Flow on the Sea Floor
How Is Plate Motion Measured?
What Drives Plate Motions?
Forces Driving Plate Motions
Forces Acting on Plates
Whole-Mantle Convection
Layer Cake Model
Taught by
Sven Holbik