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Tectonic Processes

Terms

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lithosphere
consists of the crust and the rigid upper mantle
Pangaea
large supercontinent in the Mesozoic era
convergent boundary
plates moving together where crust is destroyed
subduction boundary
when one of two plates is descending beneath another
transform boundary
plates sliding past each other; neither creation nor destruction of crust
boundary
the place where two plates meet
seafloor spreading
thoery that states that new ocean crust is formed at ocean ridges and destroyed at deep-sea trenches
plate tectonics theory
theory explains that Earth's crust and rigid upper mantle broke into enormous slabs that move
Mid-Atlantic Ridge
divergent boundary in the middle of the Atlantic Ocean
continental drift hypothesis
proposal that Earth's continents had once been joined as a single landmass
plates
the lithosphere cracked into these
divergent boundary
plates move apart and new crust is formed
convection current
the mechanism responsible for plate tectonics
oceanic crust
youngest crust and most dense
ridge
divergent boundary where new crust is created
Alfred Wegener
proposed the continental drift hypothesis
trench
deepest part of the ocean where one plate is subducted beneath another converging plate
continental crust
oldest crust and less dense than oceanic
aesthenosphere
plastic like upper part of the mantle on which the plates move
collision boundary
two continental plates colliding to create mountains

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