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Plate Tectonics

Terms

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lithosphere
rigid layer of Earth, about 100 km thick, made of the crust and upper part of the mantle
core
the central, spherical part of the Earth below the mantle
fault
a break in the Earth's crust along which blocks of the Earth slide
tension forces
type of stress that occurs when forces act to stretch an object, pulling apart
Pangaea
means "all land"
strike-slip fault
two plates sliding past one another without converging or diverging
plates
large sections of Earth's oceanic or continental crust and rigid upper mantle that moves around on the asthenosphere
convergent boundary
boundary between two plates moving together
sea floor spreading
new seafloor formed when magma is forced upward toward the surface at a mid-ocean ridge
subduction zone
place where oceanic plate sinks down into the asthenosphere at a convergent boundary
continental drift
theory that continents have moved slowly to their current locations
Earthquakes, volcanoes, mountains
evidence of plate motion
mantle
the layer of Earth between the crust and the core
asthenosphere
plastic like layer of Earth on which the lithosperic plates float and move around
transform boundary
where two plates slide past one another
compression force
stress that occurs when object is squeezed - pushing together
crust
the thin, outermost layer of the Earth - uppermost part of the lithosphere
plate tectonics
theory that Earth's crust and upper mantle are broken into plates that float and move around
convection current
current in the Earth's mantle that transfers heat in the Earth's interior - the driving force for plate tectonics
divergent boundary
boundary between two plates moving apart

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