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Plate tectonics (pp 339-343) Plate boundaries (pp 343-348) Earthquakes (pp 375-384) Wednesday July 11

Plate tectonics (pp 339-343) Plate boundaries (pp 343-348) Earthquakes (pp 375-384)

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Wednesday July 11. Plate tectonics (pp 339-343) Plate boundaries (pp 343-348) Earthquakes (pp 375-384). Free floating magnetite particles align following a well defined pattern around a magnet. - PowerPoint PPT Presentation

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Page 1: Plate tectonics (pp 339-343) Plate boundaries (pp 343-348) Earthquakes (pp 375-384)

• Plate tectonics (pp 339-343)• Plate boundaries (pp 343-348)• Earthquakes (pp 375-384)

Wednesday July 11

Page 2: Plate tectonics (pp 339-343) Plate boundaries (pp 343-348) Earthquakes (pp 375-384)
Page 3: Plate tectonics (pp 339-343) Plate boundaries (pp 343-348) Earthquakes (pp 375-384)

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Page 4: Plate tectonics (pp 339-343) Plate boundaries (pp 343-348) Earthquakes (pp 375-384)

Free floating magnetite particles align following a well defined pattern around a magnet.If support is frozen, and magnet is moved, magnetite particles keep trace of the old position of the magnet

Page 5: Plate tectonics (pp 339-343) Plate boundaries (pp 343-348) Earthquakes (pp 375-384)

Magnetic poles drift?

Yes, but not possible to have two north poles!!!

Page 6: Plate tectonics (pp 339-343) Plate boundaries (pp 343-348) Earthquakes (pp 375-384)

Plate tectonics is the explanation!!

Page 7: Plate tectonics (pp 339-343) Plate boundaries (pp 343-348) Earthquakes (pp 375-384)
Page 8: Plate tectonics (pp 339-343) Plate boundaries (pp 343-348) Earthquakes (pp 375-384)
Page 9: Plate tectonics (pp 339-343) Plate boundaries (pp 343-348) Earthquakes (pp 375-384)

Evidences of plate tectonics

1) Shape of continents2) Magnetic pole drift3) Hot spots4) Magnetic striping and age of seabed5) Similarities in fauna and flora

Page 10: Plate tectonics (pp 339-343) Plate boundaries (pp 343-348) Earthquakes (pp 375-384)
Page 11: Plate tectonics (pp 339-343) Plate boundaries (pp 343-348) Earthquakes (pp 375-384)
Page 12: Plate tectonics (pp 339-343) Plate boundaries (pp 343-348) Earthquakes (pp 375-384)

Evidences of plate tectonics

1) Shape of continents2) Magnetic pole drift3) Hot spots4) Magnetic striping and age of seabed5) Similarities in fauna and flora

Page 13: Plate tectonics (pp 339-343) Plate boundaries (pp 343-348) Earthquakes (pp 375-384)
Page 14: Plate tectonics (pp 339-343) Plate boundaries (pp 343-348) Earthquakes (pp 375-384)
Page 15: Plate tectonics (pp 339-343) Plate boundaries (pp 343-348) Earthquakes (pp 375-384)

Evidences of plate tectonics

1) Shape of continents2) Magnetic pole drift3) Hot spots4) Magnetic striping and age of seabed5) Similarities in fauna and flora

Page 16: Plate tectonics (pp 339-343) Plate boundaries (pp 343-348) Earthquakes (pp 375-384)
Page 17: Plate tectonics (pp 339-343) Plate boundaries (pp 343-348) Earthquakes (pp 375-384)

Plate motion and

boundaries

Page 18: Plate tectonics (pp 339-343) Plate boundaries (pp 343-348) Earthquakes (pp 375-384)

Why do plates move??

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Page 19: Plate tectonics (pp 339-343) Plate boundaries (pp 343-348) Earthquakes (pp 375-384)

PLATE MOTIONThree types of plate boundary

Page 20: Plate tectonics (pp 339-343) Plate boundaries (pp 343-348) Earthquakes (pp 375-384)

Divergent boundary

Page 21: Plate tectonics (pp 339-343) Plate boundaries (pp 343-348) Earthquakes (pp 375-384)

Animation 1

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Page 22: Plate tectonics (pp 339-343) Plate boundaries (pp 343-348) Earthquakes (pp 375-384)
Page 23: Plate tectonics (pp 339-343) Plate boundaries (pp 343-348) Earthquakes (pp 375-384)

Example: Mid-Atlantic

Ridge •a topographically high area near the middle of the Atlantic Ocean

•splits nearly the entire Atlantic Ocean north to south,

Page 24: Plate tectonics (pp 339-343) Plate boundaries (pp 343-348) Earthquakes (pp 375-384)

Divergent: Atlantic Ridge

LAVA FOUNTAINSKRAFLA VOLCANOICELAND

Page 25: Plate tectonics (pp 339-343) Plate boundaries (pp 343-348) Earthquakes (pp 375-384)

Rio Grande Rift

Page 26: Plate tectonics (pp 339-343) Plate boundaries (pp 343-348) Earthquakes (pp 375-384)
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Animation 2

Convergent boundary I:oceanic -continental plate involved ->

Subduction

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Page 29: Plate tectonics (pp 339-343) Plate boundaries (pp 343-348) Earthquakes (pp 375-384)

OCEANIC-CONTINENTAL COLLISONS SUSTAIN MOSTVOLCANIC ACTIVITY AROUND THE PACIFIC OCEAN

Page 30: Plate tectonics (pp 339-343) Plate boundaries (pp 343-348) Earthquakes (pp 375-384)

Convergent boundary II:oceanic -oceanic plates involved ->

SubductionSubduction processes in oceanic-oceanic plate convergence result in the formation of volcanic arc islands

Page 31: Plate tectonics (pp 339-343) Plate boundaries (pp 343-348) Earthquakes (pp 375-384)

Animation 3

Convergent boundary III:NO oceanic plate(s) involved -> Mountain

chains

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Page 32: Plate tectonics (pp 339-343) Plate boundaries (pp 343-348) Earthquakes (pp 375-384)

Convergent boundary III:NO oceanic plate(s) involved -> Mountain

chains

Page 33: Plate tectonics (pp 339-343) Plate boundaries (pp 343-348) Earthquakes (pp 375-384)

Example: Andes MtnsWest margin of the South American continent•oceanic Nazca Plate is pushed toward and beneath the continental portion of the South American Plate•typical example of a convergent plate boundary

Page 34: Plate tectonics (pp 339-343) Plate boundaries (pp 343-348) Earthquakes (pp 375-384)

Nazca - S.America plate collision

Page 35: Plate tectonics (pp 339-343) Plate boundaries (pp 343-348) Earthquakes (pp 375-384)

Transform boundary

Page 36: Plate tectonics (pp 339-343) Plate boundaries (pp 343-348) Earthquakes (pp 375-384)

Animation 4

Transform boundary

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Page 37: Plate tectonics (pp 339-343) Plate boundaries (pp 343-348) Earthquakes (pp 375-384)

Example:San Andreas fault in California

Pacific Plate slides past the North American Plate.

Page 38: Plate tectonics (pp 339-343) Plate boundaries (pp 343-348) Earthquakes (pp 375-384)

Transform boundary

Page 39: Plate tectonics (pp 339-343) Plate boundaries (pp 343-348) Earthquakes (pp 375-384)

Plate Motion Summary

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Earthquakes

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Page 42: Plate tectonics (pp 339-343) Plate boundaries (pp 343-348) Earthquakes (pp 375-384)

• Are due to the release of strain in the lithosphere

• They propagate as waves of two types:• Compression (or longitudinal or P-

mode) waves

• Deformation (or transversal or S-mode) waves

Page 43: Plate tectonics (pp 339-343) Plate boundaries (pp 343-348) Earthquakes (pp 375-384)
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