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Plate tectonics (pp 339-343) Plate boundaries (pp 343-348) Earthquakes (pp 375-384) Wednesday July 11
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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
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Magnetic poles drift? Yes, but not possible to have two north poles!!!
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Plate tectonics is the explanation!!
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Evidences of plate tectonics 1)Shape of continents 2)Magnetic pole drift 3)Hot spots 4)Magnetic striping and age of seabed 5)Similarities in fauna and flora
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Evidences of plate tectonics 1)Shape of continents 2)Magnetic pole drift 3)Hot spots 4)Magnetic striping and age of seabed 5)Similarities in fauna and flora
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Evidences of plate tectonics 1)Shape of continents 2)Magnetic pole drift 3)Hot spots 4)Magnetic striping and age of seabed 5)Similarities in fauna and flora
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Plate motion and boundaries
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Why do plates move??
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PLATE MOTION Three types of plate boundary
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Divergent boundary
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Animation 1
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Example: Mid-Atlantic Ridge a topographically high area near the middle of the Atlantic Ocean splits nearly the entire Atlantic Ocean north to south,
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Divergent: Atlantic Ridge LAVA FOUNTAINS KRAFLA VOLCANO ICELAND
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Rio Grande Rift
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Animation 2 Convergent boundary I: oceanic -continental plate involved -> Subduction
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OCEANIC-CONTINENTAL COLLISONS SUSTAIN MOST VOLCANIC ACTIVITY AROUND THE PACIFIC OCEAN
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Convergent boundary II: oceanic -oceanic plates involved -> Subduction Subduction processes in oceanic- oceanic plate convergence result in the formation of volcanic arc islands
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Animation 3 Convergent boundary III: NO oceanic plate(s) involved -> Mountain chains
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Example: Andes Mtns West 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
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Nazca - S.America plate collision
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Transform boundary
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Animation 4 Transform boundary
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Example: San Andreas fault in California Pacific Plate slides past the North American Plate.
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Transform boundary
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Plate Motion Summary
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Earthquakes
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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
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