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Theory of Plate Tectonics
1. Continents appear to “drift” with time
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Continental drift
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Evidence for continental drift
1. Puzzle like fit of continents
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Fossils correlation
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Rock Correlation
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Glacier Evidence
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Mountain Belts
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Buckled Mountains on Continental Margins
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Theory of Plate Tectonics
Continents appear to “drift” with time Lithosphere is broken up into rigid “plates”, that are moving
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Earth’s Plates
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Plate Plate ASTHENOSPHERE
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To keep the oceans from spilling out And losing all the fish!
The plates can’t curl down They must curl up To form a kind of dish To keep the oceans from spilling out And losing all the fish! - King, 1971, Nature
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Theory of Plate Tectonics
Continents appear to “drift” with time Lithosphere is broken up into rigid “plates”, that are moving There are three types of plate boundaries: Divergent Convergent Transform
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3 types of plate boundaries:
Divergent – 2 plates move away from each other, such as a mid ocean ridge where sea floor spreading occurs 2. Convergent – where 2 plates collide 3. Transform boundary – where 2 plates slide along side of one another
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Why do the plates move?
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Heat – the driving force
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Mid-Atlantic ridge Sea Floor Spreading!
Did you know that the ocean floor in the Atlantic is growing by 3cm per year? Which of the following pairs of continents are moving further away from each other? Europe and Africa Europe and North America South America and North America
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Divergent Plate Boundary Creation of An ocean Sea Floor Spreading
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Iceland – a country being split apart
is on the Mid-Atlantic Ridge
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A new ocean forming?
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Rift Valley in Africa
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Magnetic Anomalies Prove Seafloor Spreading
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The further from a ridge, the older the rock oldest youngest
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Divergent plate boundaries
MID OCEAN RIDGE A Ocean B Oceanic Crust Mantle Where would you find older rocks – at A or at B?
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