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Published byLucas Hussey Modified over 10 years ago
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Plate Tectonics A geological theory that states that pieces of Earth’s crust are in constant, slow motion, driven by convection currents in the mantle The plates of the lithosphere float on the top of the asthenosphere Convection currents rise in the asthenosphere and spread out beneath the lithosphere Geologists believe this causes plate movement Copyright © Houghton Mifflin Company. All rights reserved.
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Convection Currents: The movement of a fluid, caused by differences in temperature, that transfers heat from one part of the fluid to another Copyright © Houghton Mifflin Company. All rights reserved.
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Plates are a section of the lithosphere that slowly moves, carrying pieces of continental and oceanic crust As plates move, they collide, pull apart, or grind past each other producing spectacular changes in the earth’s surface. Copyright © Houghton Mifflin Company. All rights reserved.
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Crust is neither created nor destroyed
Transform Boundary A plate boundary where two plates move past each other in opposite directions Crust is neither created nor destroyed Fault lines are usually created in which earthquakes happen Copyright © Houghton Mifflin Company. All rights reserved.
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Figure 1-13 Transform Motion
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Geology at a Glance Plate Boundaries (cont'd)
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Convergent Boundaries
A plate boundary where two plates move toward each other Collisions can occur between: oceanic crust and oceanic crust (subduction) deep ocean trenches oceanic crust and continental crust volcanic eruptions continental crust and continental crust mountain ranges Copyright © Houghton Mifflin Company. All rights reserved.
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Geology at a Glance Plate Boundaries (cont'd)
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Figure 1-12a Continental Collision
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Figure 1-12b Continental Collision (cont'd)
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Figure 1-11 Plate Subduction
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A plate boundary where two plates move away from each other
Divergent Boundaries A plate boundary where two plates move away from each other Most divergent boundaries occur at the mid-ocean ridge Divergent boundaries that occur on land are called rift valleys Ocean Basins are usually the result of this type of movement Copyright © Houghton Mifflin Company. All rights reserved.
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Geology at a Glance Plate Boundaries (cont’d)
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Transform Convergent Divergent Summary of Boundaries
Plates slip past each other (grind) Convergent Plates come together (collide) Divergent Plates move apart (pull apart) Copyright © Houghton Mifflin Company. All rights reserved.
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Geology at a Glance Plate Boundaries
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Major Plates Six major plates: Eurasian African Indo-Australian
Pacific North American South American Copyright © Houghton Mifflin Company. All rights reserved.
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