3 ways that plates move
Convection currents
Slab pull
Ridge push
Convection currents
In the mantle
Movement of particles from an area of high temp. to an area of low
Circular action from outer core to crust to outer core again
Drives movement of plates
Slab pull
Only at destructive plates
Subducting plate pulls the rest of the plate with it
Frictional resistance causes earthquakes
OCCURS AT DESTRUCTIVE BOUNDARIES
Ridge Push// Gravitational sliding
Upwelling of new magma pushes the middle of the ocean ridge
Slopes away from the ridge
Gravitational sliding from there
Also some frictional resistance causing earthquakes
OCCURS AT CONSTRUCTIVE BOUNDARIES