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Published byHeather Daniel Modified over 8 years ago
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November 14, 2011
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I will return your exams tomorrow. (Grades Look Good) Pick up a textbook from the library We will start Unit 3 today( Tectonic Processes) This unit has a lot of vocabulary words. Please download the vocabulary pdf from my website.
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Let's look at Tectonic Processes. These are the forces that are trying to build the earth. Physical evidence of this happening includes volcanoes, earthquakes, folds, and faults.
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Knowledge has come from studying seismic waves which are generated by earthquakes and are registered on seismographs
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1) Body Waves: travel through the interior of the earth a) primary (P) or compression waves: travel fastest through any material b) secondary (S) or shearing-deformation waves: travel only through solid materials
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Surface Waves: travel only through the crust (i.e. L or long waves)
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Crust or Lithosphere 5 to 64 km thick brittle shell of solid rock that cracks, warps, and bends thinnest on the ocean floors Sial (i.e. light granitic rock): major component of the continents Sima (i.e. dense basaltic rock): major component of the ocean basins
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approx. 2900 km thick upper part is known as the asthenosphere very hot, approx. 1650 deg. C in upper part driving force for volcanoes, mountain building, and continental drift
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approx. 2900 km thick Outer core: likely made of liquid iron Inner core: believed to be solid iron, 4000 to 6000 deg. C, inner heat believed to be caused by the decay of radioactive rock
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located in the upper mantle - partially molten (i.e. approx. 10%) - lithosphere "floats" on top of the asthenosphere - zones that have become molten, or partially molten, can develop convection currents - convection currents in the asthenosphere are responsible for plate movement
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Convection currents in the outer core are partially responsible for the earth's magnetic field but do not drive the tectonic plates convection: transmission of heat within a liquid or gas by movement of heated particles. molten: liquefied by heat
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