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Ocean Floor as a Magnetic Recorder
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Classroom Contents
Plate Tectonics
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- 1 Continental Drift: An Idea Before Its Time
- 2 Pangaea 200 Million Years Ago
- 3 Similar Fossils on Different Continents
- 4 Continental Drift: Supporting Evidence
- 5 The Great Debate
- 6 The Theory of Plate Tectonics
- 7 Earth's Lithospheric Plates
- 8 Three Types of Plate Boundaries
- 9 Divergent Plate Boundary
- 10 Mid-ocean ridge system
- 11 Iceland: Mid-ocean ridge
- 12 Divergent Plate Boundaries
- 13 Continental Rifting
- 14 Convergent Plate Boundaries & Subduction
- 15 Oceanic-Continental Convergence
- 16 Continent-Continent Convergence
- 17 Plate Boundaries • Transform fault boundaries - Plates slide past one another
- 18 Changing Plate Boundaries
- 19 Deep-Sea Drilling
- 20 Hot Spots and Hot Spot Tracks
- 21 Testing the Plate Tectonics Model
- 22 Polar wandering paths for Eurasia and North America
- 23 Magnetic Reversals and Seafloor Spreading
- 24 Ocean Floor as a Magnetic Recorder
- 25 Heat Flow on the Sea Floor
- 26 How Is Plate Motion Measured?
- 27 What Drives Plate Motions?
- 28 Forces Driving Plate Motions
- 29 Forces Acting on Plates
- 30 Whole-Mantle Convection
- 31 Layer Cake Model
