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Plate Tectonics

AB
lithospherecombination of the Earth's crust and the top, rigid portion of the upper mantle
asthenosphereportion of the upper mantle that is acutally partially melted (molten) and able to flow
platesection of the Earth's lithosphere that moves due to convection currents in the asthenosphere
Mohorovicic Discontinuityboundary between the Earth's crust and the upper mantle
outer coreits fluid motion creates the Earth's magnetic field
hypothesis of continental driftstated that at one time all the continents were joined together in one supercontinent
HMS Challengerexpedition was responsible for discovering mid-oceanic ridges
SONARdiscovered trenches and confirmed length of mid-oceanic ridges
subduction zoneanother name for trench
Glomar Challengerdiscovered that the ocean floor is youngest near the ridges
hypothesis of seafloor spreadingstated that new crust is formed at the ridges and destroyed at the trenches
paleomagnetismrecord of the direction of Earth's magnetic field due to minerals in igneous rocks
normal polaritywhen the direction of the magnetic field in rocks matches today's alignment
reverse polaritywhen the direction of the Earth's magnetic field is opposite of today's alignment
Theory of Plate Tectonicsprovides the mechanism for continental drift
convergent boundaryplace where 2 continental plates are moving together
divergent boundaryplace where 2 continental plates are moving apart
transform faultplace where 2 continental plates slide horizontally past each other


IPC, Earth/Space Science & AP Environmental Science Instructor
Friendswood High School
Friendswood, TX

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