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Divergent Plate Boundaries
plates move apart
associated with earthquakes and volcanic eruptions (basaltic, not explosive)
decompression melting
Transform Fault Boundaries
plates slide past each other horizontally (ex: san andres fault)
great earthquake hazard
strike-slip faults
Convergent Plate Boundaries
plates collide (subduction zones and continent-continent)
Subduction Zones
denser oceanic plate goes underneath an oceanic or continental plate (less dense)
associated with explosive volcanoes (andesitic or rhyolitic); severe landslides, earthquakes, mudflows, ash flows too (more than 80% subaerial eruptions)
water from subducting plate causes mantle melting
composite cones and stratovolcanoes
Continent-continent
collision zone
crust too low in density to subduct
associated with earthquakes and high topography (mountains), affecting climate