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Published byHeather Morgan Modified over 9 years ago
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Chapter 17 Plate Tectonics Part 2
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Plate Interactions We have two different types of crust Oceanic Continental We have three different types of boundaries. Convergent – plates coming together Divergent – plates moving apart Transform – plates slide past each other
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Plate boundaries
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Convergent boundaries
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Oceanic - Oceanic Pacific plate colliding with the North American plate Aleutian Islands are forming
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Aleutian Islands
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Convergent boundaries Continental – Continental Indian plate colliding with the Eurasian plate Himalayas are forming
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Himalayas
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Himalayas
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Himalayas
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Convergent boundaries Oceanic – Continental Nazca plate colliding with South American plate The Andes mountains are forming
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Andes Mountains
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Divergent boundaries Oceanic – Oceanic North American plate and the African plate Mid-Atlantic ridge
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Mid Atlantic Ridge
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Mid Atlantic Ridge @ Iceland
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Divergent boundaries Continental – Continental African plate splitting apart near Uganda East-African rift
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East African Rift
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Continental Rift Zone
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Lake Tanganyika 2 nd deepest lake in the World (4800 ft)
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Lake Tanganyika
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Victoria Falls
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Great Rift Valley
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Transform boundaries Pacific plate and the North American plate San Andreas fault California
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San Andreas Fault
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High altitude view
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Causes of Plate Motion Convective currents cause plate movement.
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Causes of Plate Motion Ridge push and slab pull also contribute to plate motion.
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