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Science Unit D Chap 1 Movements of the Earth's Crust

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crustthe Earth's outermost layer
mantlethe layer directly beneath the Earth's crust
corethe Earth's innermost layer
lithospherethe cool, solid portion of Earth that includes all the crust and part of the upper mantle
asthenospherea zone of partially melted rock in the upper mantle of the Earth
plate tectonicsthe theory scientists use to explain the movements of the plates on the Earth's surface
divergent boundarya boundary where crustal plates move away from each other
convergent boundarya boundary where crustal plates collide with each other
transform fault boundarya boundary where crustal plates grind past each other
mid-ocean ridgethe place where plates of the Earth's crust along the ocean floor are being split apart and molten rock pushes up to form new ocean floor and a mountain range
rifta deep ocean valley formed where two crustal plates move apart
sea-floor spreadinga process in which magna is slowly pushed up through cracks in a rift and then cools to form new sea floor
earthquakethe sudden movement of rock along a fault which releases energy vibrations
focusthe point in the Earth's crust where the first major movement of an earthquake fault occurs
epicenterthe point on the Earth's surface directly above the focus of an earthquake
P wavea primary wave or "push-pull" wave of released energy in the Earth's surface that causes a back-and forth vibration in the same direction that the wave moves
S wavea slower kind of energy wave released by an earthquake that causes vibrations at right angles to the wave's direction of travel
surface wavean energy wave from an earthquake that travels only at the surface and moves less quickly than P waves and S waves but makes the ground roll and sway
Richter scalea scale that measures the amount of energy released during an earthquake
volcanoa mountain that may form around an opening in the Earth's surface where an eruption or molten rock occurs


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