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Plate Tectonics (cont.d)

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Presentation on theme: "Plate Tectonics (cont.d)"— Presentation transcript:

1 Plate Tectonics (cont.d)
Lecture 3 Plate Tectonics (cont.d) Earthquakes As Evidence Most large earthquakes occur at subduction zones. Earthquake activity mirrors tectonic plate boundaries. © 2011 Pearson Education, Inc.

2 Global Distribution of Earthquakes
© 2011 Pearson Education, Inc. © 2011 Pearson Education, Inc.

3 Global Plate Boundaries
© 2011 Pearson Education, Inc. © 2011 Pearson Education, Inc.

4 Plate Tectonics Theory
Lithosphere – tectonic plates that float on ductile asthenosphere Large scale geologic features occur at plate boundaries Two major tectonic forces Slab pull Slab suction © 2011 Pearson Education, Inc. © 2011 Pearson Education, Inc.

5 Types of Plate Boundaries
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6 Examples of Plate Boundaries
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7 Divergent Boundary Features
Plates move apart Mid-ocean ridge Rift valley New ocean floor created Shallow focus earthquakes © 2011 Pearson Education, Inc. © 2011 Pearson Education, Inc.

8 Generation of a Divergent Boundary
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9 Types of Spreading Centers
Oceanic rise Fast-spreading Gentle slopes East Pacific Oceanic ridge Slow-spreading Steep slopes Mid-Atlantic Ultra-slow Deep rift valley Widely scattered volcanoes Arctic and southwest India © 2011 Pearson Education, Inc. © 2011 Pearson Education, Inc.

10 Types of Spreading Centers
Mid-Atlantic Ridge East Pacific Rise © 2011 Pearson Education, Inc. © 2011 Pearson Education, Inc. © 2011 Pearson Education, Inc.

11 Convergent Boundary Features
Plates move toward each other Oceanic crust destroyed Ocean trench Volcanic arc Deep focus earthquakes © 2011 Pearson Education, Inc. © 2011 Pearson Education, Inc.

12 Three Types of Convergent Boundaries
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13 Types of Convergent Boundaries
Oceanic-Continental Convergence Ocean plate is subducted Continental arcs generated Explosive andesitic volcanic eruptions © 2011 Pearson Education, Inc. © 2011 Pearson Education, Inc.

14 Types of Convergent Boundaries
Oceanic-Oceanic Convergence Denser plate is subducted Deep trenches generated Volcanic island arcs generated © 2011 Pearson Education, Inc. © 2011 Pearson Education, Inc.

15 Types of Convergent Boundaries
Continental-Continental Convergence No subduction Tall mountains uplifted © 2011 Pearson Education, Inc. © 2011 Pearson Education, Inc.

16 Transform Boundary Features
Offsets oriented perpendicular to mid-ocean ridge Segments of plates slide past each other Offsets permit mid-ocean ridge to move apart at different rates Shallow but strong earthquakes © 2011 Pearson Education, Inc. © 2011 Pearson Education, Inc.

17 Transform Boundary Features
Oceanic Transform Fault – ocean floor only Continental Transform Fault – cuts across continent All transform faults occur between mid-ocean ridge segments. © 2011 Pearson Education, Inc. © 2011 Pearson Education, Inc.

18 Plate Interior (non-plate boundary)Topography Formation:
Mantle Plumes and Hotspots Intraplate features Volcanic islands within a plate Island chains Record ancient plate motions Hotspot Track

19 Global Hotspot Locations
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20 Hawaiian Island – Emperor Seamount Hotspot Track
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21 Plate Tectonics and Intraplate Features
Seamounts Rounded tops Tablemounts Flattened tops Subsidence of flanks of mid-ocean ridge Wave erosion may flatten seamount © 2011 Pearson Education, Inc. © 2011 Pearson Education, Inc.

22 Coral Reef Development
Fringing reefs – develop along margin of landmass Barrier reefs – separated from landmass by lagoon Atolls – reefs continue to grow after volcanoes are submerged © 2011 Pearson Education, Inc. © 2011 Pearson Education, Inc.

23 Coral Reef Development
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24 Detecting Plate Motion with Satellites
© 2011 Pearson Education, Inc. © 2011 Pearson Education, Inc.

25 Paleogeography Paleogeography – study of ancient continents
Continental accretion Continental material added to edges of continents through plate motion © 2011 Pearson Education, Inc. © 2011 Pearson Education, Inc.

26 Paleogeographic Reconstructions
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27 Future Predictions Future positions of continents and oceans
Assume same direction and rate of plate motions as now © 2011 Pearson Education, Inc. © 2011 Pearson Education, Inc.

28 World Map 50 million Years in Future
© 2011 Pearson Education, Inc. © 2011 Pearson Education, Inc.

29 Wilson cycle John Tuzo Wilson Life cycle of ocean basins Formation
Growth Destruction © 2011 Pearson Education, Inc. © 2011 Pearson Education, Inc.

30 Wilson cycle © 2011 Pearson Education, Inc.


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