lecture 3 plate tectonics (cont.d) © 2011 pearson education, inc. earthquakes as evidence most...

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

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Page 1: Lecture 3 Plate Tectonics (cont.d) © 2011 Pearson Education, Inc. Earthquakes As Evidence Most large earthquakes occur at subduction zones. Earthquake

Lecture 3

Plate Tectonics (cont.d)

© 2011 Pearson Education, Inc.

Earthquakes As Evidence

• Most large earthquakes occur at subduction zones.

• Earthquake activity mirrors tectonic plate boundaries.

Page 2: Lecture 3 Plate Tectonics (cont.d) © 2011 Pearson Education, Inc. Earthquakes As Evidence Most large earthquakes occur at subduction zones. Earthquake

© 2011 Pearson Education, Inc.© 2011 Pearson Education, Inc.

Global Distribution of Earthquakes

Page 3: Lecture 3 Plate Tectonics (cont.d) © 2011 Pearson Education, Inc. Earthquakes As Evidence Most large earthquakes occur at subduction zones. Earthquake

© 2011 Pearson Education, Inc.© 2011 Pearson Education, Inc.

Global Plate Boundaries

Page 4: Lecture 3 Plate Tectonics (cont.d) © 2011 Pearson Education, Inc. Earthquakes As Evidence Most large earthquakes occur at subduction zones. Earthquake

© 2011 Pearson Education, Inc.© 2011 Pearson Education, Inc.

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

Page 5: Lecture 3 Plate Tectonics (cont.d) © 2011 Pearson Education, Inc. Earthquakes As Evidence Most large earthquakes occur at subduction zones. Earthquake

© 2011 Pearson Education, Inc.© 2011 Pearson Education, Inc.

Types of Plate Boundaries

Page 6: Lecture 3 Plate Tectonics (cont.d) © 2011 Pearson Education, Inc. Earthquakes As Evidence Most large earthquakes occur at subduction zones. Earthquake

© 2011 Pearson Education, Inc.© 2011 Pearson Education, Inc.

Examples of Plate Boundaries

Page 7: Lecture 3 Plate Tectonics (cont.d) © 2011 Pearson Education, Inc. Earthquakes As Evidence Most large earthquakes occur at subduction zones. Earthquake

© 2011 Pearson Education, Inc.© 2011 Pearson Education, Inc.

Divergent Boundary Features

• Plates move apart• Mid-ocean ridge

– Rift valley• New ocean floor

created• Shallow focus

earthquakes

Page 8: Lecture 3 Plate Tectonics (cont.d) © 2011 Pearson Education, Inc. Earthquakes As Evidence Most large earthquakes occur at subduction zones. Earthquake

© 2011 Pearson Education, Inc.© 2011 Pearson Education, Inc.

Generation of a Divergent Boundary

Page 9: Lecture 3 Plate Tectonics (cont.d) © 2011 Pearson Education, Inc. Earthquakes As Evidence Most large earthquakes occur at subduction zones. Earthquake

© 2011 Pearson Education, Inc.© 2011 Pearson Education, Inc.

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

Page 10: Lecture 3 Plate Tectonics (cont.d) © 2011 Pearson Education, Inc. Earthquakes As Evidence Most large earthquakes occur at subduction zones. Earthquake

© 2011 Pearson Education, Inc.© 2011 Pearson Education, Inc.© 2011 Pearson Education, Inc.

Types of Spreading Centers

East Pacific Rise

Mid-Atlantic Ridge

Page 11: Lecture 3 Plate Tectonics (cont.d) © 2011 Pearson Education, Inc. Earthquakes As Evidence Most large earthquakes occur at subduction zones. Earthquake

© 2011 Pearson Education, Inc.© 2011 Pearson Education, Inc.

Convergent Boundary Features

• Plates move toward each other• Oceanic crust destroyed

– Ocean trench– Volcanic arc

• Deep focus earthquakes

Page 12: Lecture 3 Plate Tectonics (cont.d) © 2011 Pearson Education, Inc. Earthquakes As Evidence Most large earthquakes occur at subduction zones. Earthquake

© 2011 Pearson Education, Inc.© 2011 Pearson Education, Inc.

Three Types of Convergent Boundaries

Page 13: Lecture 3 Plate Tectonics (cont.d) © 2011 Pearson Education, Inc. Earthquakes As Evidence Most large earthquakes occur at subduction zones. Earthquake

© 2011 Pearson Education, Inc.© 2011 Pearson Education, Inc.

Types of Convergent Boundaries

• Oceanic-Continental Convergence– Ocean plate is

subducted– Continental arcs

generated– Explosive andesitic

volcanic eruptions

Page 14: Lecture 3 Plate Tectonics (cont.d) © 2011 Pearson Education, Inc. Earthquakes As Evidence Most large earthquakes occur at subduction zones. Earthquake

© 2011 Pearson Education, Inc.© 2011 Pearson Education, Inc.

Types of Convergent Boundaries

• Oceanic-Oceanic Convergence– Denser plate is subducted– Deep trenches generated– Volcanic island arcs generated

Page 15: Lecture 3 Plate Tectonics (cont.d) © 2011 Pearson Education, Inc. Earthquakes As Evidence Most large earthquakes occur at subduction zones. Earthquake

© 2011 Pearson Education, Inc.© 2011 Pearson Education, Inc.

Types of Convergent Boundaries

• Continental-Continental Convergence– No subduction– Tall mountains uplifted

Page 16: Lecture 3 Plate Tectonics (cont.d) © 2011 Pearson Education, Inc. Earthquakes As Evidence Most large earthquakes occur at subduction zones. Earthquake

© 2011 Pearson Education, Inc.© 2011 Pearson Education, Inc.

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

Page 17: Lecture 3 Plate Tectonics (cont.d) © 2011 Pearson Education, Inc. Earthquakes As Evidence Most large earthquakes occur at subduction zones. Earthquake

© 2011 Pearson Education, Inc.© 2011 Pearson Education, Inc.

Transform Boundary Features• Oceanic Transform Fault – ocean floor only• Continental Transform Fault – cuts across

continent• All transform faults

occur between mid-ocean ridge segments.

Page 18: Lecture 3 Plate Tectonics (cont.d) © 2011 Pearson Education, Inc. Earthquakes As Evidence Most large earthquakes occur at subduction zones. Earthquake

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

Page 19: Lecture 3 Plate Tectonics (cont.d) © 2011 Pearson Education, Inc. Earthquakes As Evidence Most large earthquakes occur at subduction zones. Earthquake

© 2011 Pearson Education, Inc.© 2011 Pearson Education, Inc.

Global Hotspot Locations

Page 20: Lecture 3 Plate Tectonics (cont.d) © 2011 Pearson Education, Inc. Earthquakes As Evidence Most large earthquakes occur at subduction zones. Earthquake

© 2011 Pearson Education, Inc.© 2011 Pearson Education, Inc.

Hawaiian Island – Emperor Seamount Hotspot Track

Page 21: Lecture 3 Plate Tectonics (cont.d) © 2011 Pearson Education, Inc. Earthquakes As Evidence Most large earthquakes occur at subduction zones. Earthquake

© 2011 Pearson Education, Inc.© 2011 Pearson Education, Inc.

Plate Tectonics and Intraplate Features

• Seamounts – Rounded tops

• Tablemounts– Flattened tops

• Subsidence of flanks of mid-ocean ridge• Wave erosion may flatten seamount

Page 22: Lecture 3 Plate Tectonics (cont.d) © 2011 Pearson Education, Inc. Earthquakes As Evidence Most large earthquakes occur at subduction zones. Earthquake

© 2011 Pearson Education, Inc.© 2011 Pearson Education, Inc.

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

Page 23: Lecture 3 Plate Tectonics (cont.d) © 2011 Pearson Education, Inc. Earthquakes As Evidence Most large earthquakes occur at subduction zones. Earthquake

© 2011 Pearson Education, Inc.© 2011 Pearson Education, Inc.

Coral Reef Development

Page 24: Lecture 3 Plate Tectonics (cont.d) © 2011 Pearson Education, Inc. Earthquakes As Evidence Most large earthquakes occur at subduction zones. Earthquake

© 2011 Pearson Education, Inc.© 2011 Pearson Education, Inc.

Detecting Plate Motion with Satellites

Page 25: Lecture 3 Plate Tectonics (cont.d) © 2011 Pearson Education, Inc. Earthquakes As Evidence Most large earthquakes occur at subduction zones. Earthquake

© 2011 Pearson Education, Inc.© 2011 Pearson Education, Inc.

Paleogeography

• Paleogeography – study of ancient continents

• Continental accretion– Continental material added to edges of

continents through plate motion

Page 26: Lecture 3 Plate Tectonics (cont.d) © 2011 Pearson Education, Inc. Earthquakes As Evidence Most large earthquakes occur at subduction zones. Earthquake

© 2011 Pearson Education, Inc.© 2011 Pearson Education, Inc.

Paleogeographic Reconstructions

Page 27: Lecture 3 Plate Tectonics (cont.d) © 2011 Pearson Education, Inc. Earthquakes As Evidence Most large earthquakes occur at subduction zones. Earthquake

© 2011 Pearson Education, Inc.© 2011 Pearson Education, Inc.

Future Predictions

• Future positions of continents and oceans– Assume same direction and rate of plate

motions as now

Page 28: Lecture 3 Plate Tectonics (cont.d) © 2011 Pearson Education, Inc. Earthquakes As Evidence Most large earthquakes occur at subduction zones. Earthquake

© 2011 Pearson Education, Inc.© 2011 Pearson Education, Inc.

World Map 50 million Years in Future

Page 29: Lecture 3 Plate Tectonics (cont.d) © 2011 Pearson Education, Inc. Earthquakes As Evidence Most large earthquakes occur at subduction zones. Earthquake

© 2011 Pearson Education, Inc.© 2011 Pearson Education, Inc.

Wilson cycle

• John Tuzo Wilson

• Life cycle of ocean basins–Formation

–Growth

–Destruction

Page 30: Lecture 3 Plate Tectonics (cont.d) © 2011 Pearson Education, Inc. Earthquakes As Evidence Most large earthquakes occur at subduction zones. Earthquake

© 2011 Pearson Education, Inc.© 2011 Pearson Education, Inc.

Wilson cycleWilson cycle