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Plate Tectonics- Mrs. Pierce

AB
continental driftWegener's hypothesis that all continents were once connected in a single, large landmass that broke apart about 200 million years ago and drifted slowly to their current positions
Pangaealarge, ancient landmass
seafloor spreadingHess's theory that new seafloor is formed when magma is forced upward toward the surface at a mid-ocean ridge
plate tectonicstheory that Earth's crust and upper mantle moves around on the asthenosphere
platea large section of Earth's oceanic or continental crust and rigid upper mantle that moves around on the astenosphere
lithosphererigid layer of Earth about 100km thick, made of the crust and a part of the upper mantle
asthenosphereplastic like layer of Earth on which the lithosphereic plates float and move around
convection currentcurrent in Earth's mantle that transfers heat in Earth's interior and is the driving force for plates tectonics
plate boundarieswhere Earth's plates come together
divergent boundaryboundary between plates that are moving apart from one another
convergent boundariesboundaries between Earth's plates that are moving together
subduction zonewhere oceanic plates and continental plates collide, the oceanic plate is pushed beneath the continental plate
transform boundarywhere two plates slide past one another
SONARdevice that uses sound waves to determine the depth of ocean and to map out the bottom of the ocean floor
mid-ocean ridgearea where new ocean floor is formed when lava erupts through cracks in the Earth's surface
Rift Valleya large valley shaped by plates that are pulling apart
controversialarguable, questionable

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