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Published byJonas Maxwell Modified over 9 years ago
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Theory of Plate Tectonics
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Power of Plate Motion Chilean Earthquake Chile Quake Poses Possible Hawaii Tsunami Threat Major Earthquake in Hati 2010
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A New Theory Sea-floor spreading supported Wegener’s Continental Drift How do we explain Sea-floor spreading and Continental Drift? Plate Tectonics
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Theory that the Earth’s lithosphere is divided into tectonic plates that move on top of the asthenosphere Plate movement
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Convection Hot material rises while cool material sinks Cool material is dense The motion of sinking and rising material drags the tectonic plate away from mid-ocean ridge Flash Presentation
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Tectonic Plate Boundaries Convergent Divergent Transform
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Convergent Plate Boundaries When two plates push into each other Classification based on crust: Continental/Continental Continental/Oceanic Oceanic/Oceanic
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Subduction Zones Region where the oceanic plate sinks into the asthenosphere Volcanic formations frequently occur Formed at Convergent Boundary Continental/oceanic Oceanic/oceanic Ocean Trenches
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Divergent Plate Boundary Two plate move away from each other Where new oceanic lithosphere forms Can form on land as well: rift valley Example is mid-ocean ridge
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Transform Plate Boundary Two plates slide past each other horizontally San Andreas Fault is example
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