Composite volcanoes are formed at destructive plate boundaries because an oceanic plate is pushed towards the continental plate by convection currents. The oceanic plate is subducted ; this creates a deep ocean trench.
Shield volcanoes are formed at constructive plate boundaries becaus ethe two plates are moving apart from each other in opposite directions. Convection currents moving in opposite directions in the mantle move the two plates apart. As the plates move apart, magma from the mantle escapes and the magma fills the gap and eventually erupts onto the surface and cools as land. A good example of this is the mid atlantic ridge, where the eurasian plate moves away from the North american plate.
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