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Chapter 17 Plate Tectonics Part 2. Plate Interactions  We have two different types of crust  Oceanic  Continental  We have three different types of.

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Presentation on theme: "Chapter 17 Plate Tectonics Part 2. Plate Interactions  We have two different types of crust  Oceanic  Continental  We have three different types of."— Presentation transcript:

1 Chapter 17 Plate Tectonics Part 2

2 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

3 Plate boundaries

4 Convergent boundaries

5  Oceanic - Oceanic  Pacific plate colliding with the North American plate  Aleutian Islands are forming

6 Aleutian Islands

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9 Convergent boundaries  Continental – Continental  Indian plate colliding with the Eurasian plate  Himalayas are forming

10 Himalayas

11 Himalayas

12 Himalayas

13 Convergent boundaries  Oceanic – Continental  Nazca plate colliding with South American plate  The Andes mountains are forming

14 Andes Mountains

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18 Divergent boundaries  Oceanic – Oceanic  North American plate and the African plate  Mid-Atlantic ridge

19 Mid Atlantic Ridge

20 Mid Atlantic Ridge @ Iceland

21 Divergent boundaries  Continental – Continental  African plate splitting apart near Uganda  East-African rift

22 East African Rift

23 Continental Rift Zone

24 Lake Tanganyika 2 nd deepest lake in the World (4800 ft)

25 Lake Tanganyika

26 Victoria Falls

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28 Great Rift Valley

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30 Transform boundaries  Pacific plate and the North American plate  San Andreas fault  California

31 San Andreas Fault

32 High altitude view

33 Causes of Plate Motion  Convective currents cause plate movement.

34 Causes of Plate Motion  Ridge push and slab pull also contribute to plate motion.


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