Stress at a divergent plate boundary

Stress at a convergent plate boundary

Upward-arching rock layer

Downward-arching rock layer

Hanging wall moves down relative to footwall

Hanging wall moves up relative to footwall

Sinking of rock layers

Rising of rock layers

The global positioning system can map the rate of tectonic plate movement using

A possible result of plates moving along a transform boundary is

Where two plates collide

where two plates are moving away from each other

Where two plates are moving horizontally past each other

Process of moving layers of rock by heating and cooling

Where denser oceanic lithosphere sinks beneath continental lithosphere

Where oceanic lithosphere slides downhill due to gravity

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