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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.
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Global Distribution of Earthquakes
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Global Plate Boundaries
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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.
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Types of Plate Boundaries
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Examples of Plate Boundaries
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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.
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Generation of a Divergent Boundary
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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.
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Types of Spreading Centers
Mid-Atlantic Ridge East Pacific Rise © 2011 Pearson Education, Inc. © 2011 Pearson Education, Inc. © 2011 Pearson Education, Inc.
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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.
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Three Types of Convergent Boundaries
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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.
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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.
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Types of Convergent Boundaries
Continental-Continental Convergence No subduction Tall mountains uplifted © 2011 Pearson Education, Inc. © 2011 Pearson Education, Inc.
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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.
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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.
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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
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Global Hotspot Locations
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Hawaiian Island – Emperor Seamount Hotspot Track
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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.
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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.
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Coral Reef Development
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Detecting Plate Motion with Satellites
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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.
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Paleogeographic Reconstructions
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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.
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World Map 50 million Years in Future
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Wilson cycle John Tuzo Wilson Life cycle of ocean basins Formation
Growth Destruction © 2011 Pearson Education, Inc. © 2011 Pearson Education, Inc.
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Wilson cycle © 2011 Pearson Education, Inc.
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