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Chap. 5/6/7

Plate tectonics/Earthquakes/Volcnoes

AB
seismic waveearthquake waves that travel through the Earth
3 layers of Earthcrust, mantle, outer core, inner core
lithospherecrust & upper mantle; what plates are made up of
radiationheat/energy transfer through space
conductionheat/energy transfer between materials that are touching
convectionheat/energy transfer by currents in a fluid (liquid or gas); how heat transfer occurs in mantle & core; and cause of plate movements
Theory of Plate Tectonicsexplains the formation & movement of the Earth's plates
Pangaeasupercontinent, when continents were all connected millions of years ago
Wegenercame up with idea/hypothesis that the continents were once joined together
divergent boundarywhen 2 plates are moving apart
convergent boundarywhen 2 plates are moving towards each other
transform boundarywhen 2 plates are slipping past each other in opposite directions
mid-ocean ridgeundersea mountain chain where new ocean floor is produced
rift valleya deep valley that forms where 2 plates move apart
sea-floor spreadingsea floor spreads apart along both sides of a mid-ocean ridge as new crust is added
subductionocean floor sinks beneath another plate and into the mantle
trenchwhere subduction occurs
geothermal energywater heated by magma/Earth, provides an energy source
faulta break in the rock of the crust where rock surfaces slip past each other
focusarea beneath Earth's surface where the earthquake occurs (rock breaks)
epicenterpoint on the surface directly above the focus
magmamolten material that is still inside the Earth
lavamolten material that reaches the Earth's surface
Ring of Firemajor volcanic belt that rims the Pacific Ocean
hot spotarea where material from deep within the mantle rises and then melts (Hawaiian Islands, Yellowstone)



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