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Published byTamsyn Nancy Stanley Modified over 5 years ago
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Warm Up! Draw a line to match the scientist to the idea or theory he made Harry Hess Theory Plate Tectonics Alfred Wegener Sea-Floor Spreading J. Tuzo Wilson Continental Drift
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Theory of Plate Tectonics
Big book pg. 150 Small book pg. 32
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John Tuzo Wilson Canadian scientist, studied physics
1965 – proposed the Theory of Plate Tectonics
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John Tuzo Wilson Canadian scientist, studied physics
1965 – proposed the Theory of Plate Tectonics
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John Tuzo Wilson Canadian scientist, studied physics
1965 – proposed the Theory of Plate Tectonics
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Plate Tectonics Pieces of Earth´s crust are in slow, constant motion
They move because of convection in the mantle
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Plate Tectonics Pieces of Earth´s crust are in slow, constant motion
They move because of convection in the mantle
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Plate Tectonics Pieces of Earth´s crust are in slow, constant motion
They move because of convection in the mantle
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Plate Boundaries – 3 types
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1. Divergent Boundaries 2 plates are moving apart
Ex: Mid ocean ridge, rift valley
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1. Divergent Boundaries 2 plates are moving apart
Ex: Mid ocean ridge, rift valley
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2. Convergent Boundaries
2 plates are colliding ex: Deep ocean trench (subduction), Himalayan & Andes mountains
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2. Convergent Boundaries
2 plates are colliding ex: Deep ocean trench (subduction), Himalayan & Andes mountains
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3. Transform Boundaries 2 plates are sliding past each other in opposite directions Ex. San Andreas Fault in California
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3. Transform Boundaries 2 plates are sliding past each other in opposite directions Ex. San Andreas Fault in California
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3. Transform Boundaries 2 plates are sliding past each other in opposite directions Ex. San Andreas Fault in California This crack in the crust created by plates moving is called a Fault
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3. Transform Boundaries 2 plates are sliding past each other in opposite directions Ex. San Andreas Fault in California
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Plate motion over time
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Classwork Define Key terms Plate Scientific Theory Fault Rift Valley
S5 Assessment #1, 2 (Due Friday)
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