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Earth Science, Chapter 7: Plate Tectonics

AB
PangaeaA large landmass of all land on Earth joined together that began to break apart approximately 200 million years ago
Continental driftThe movement of Earth’s continents over time
Mid-ocean ridgeLong, narrow mountain range on the ocean floor; formed by magma at divergent plate boundaries
Ocean trenchA deep, underwater trough created by one plate subducting under another plate at a convergent plate boundary
Seafloor spreadingThe process by which new oceanic crust forms along a mid-ocean ridge and older oceanic crust moves away from the ridge
Normal polarityWhen magnetized objects, such as compass needles, orient themselves to point north
Reversed polarityWhen magnetized objects reverse direction and orient themselves to point south
Plate tectonicsThe theory that Earth’s surface is broken into large, rigid pieces that move with respect to each other
PlateA large section of Earth’s oceanic or continental crust and the rigid upper mantle that moves around on the asthenosphere
Divergent plate boundaryThe boundary between two plates that move away from each other
Transform plate boundaryThe boundary between two plates that slide past each other
Convergent plate boundaryThe boundary between two plates that move toward each other
SubductionThe process that occurs when one tectonic plate moves under another tectonic plate
ConvectionThe circulation of particles within a material caused by differences in thermal energy and density
UpliftThe process that moves large bodies of Earth materials to higher elevations



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