THE IDEA THAT HUGE LITHOSPHERIC PLATES MOVE

MAGMA CURRENTS THAT MOVE THE LITHOSPHERIC PLATES

THE PULLING FORCE EXERTED BY A PLATE BY ITS OWN WEIGHT

A FORCE THAT CAUSES A PLATE TO MOVE AWAY FROM A OCEAN RIDGE

WHEN TWO TECTONIC PLATES MOVE AWAY FROM EACH OTHER.

LANDFORM THAT RESULTS FROM A DIVERGENT PLATE BOUNDARY

UNDERWATER RIFT THAT IS CAUSED BY A DIVERGENT PLATE BOUNDARY

WHEN 2 PLATES MOVE TOWARD ONE ANOTHER AND COLLIDE

WHEN A OCEAN PLATE CRASHES INTO A CONTINENTAL PLATE

CREATED WHEN 2 OCEAN PLATES CONVERGED(VOLCANIC ARC)

HAPPENS WHEN 2 PLATES CRASH INTO EACH OTHER(MOUTAIN RANGE)

A PLACE WHERE ONE PLATE BEING DRAWN DOWN UNDER THE OTHER

IT IS A LONG NARROW STEEP-SIDED DEPRESSION IN OCEANIC CRUST

CAUSED WHEN 2 PLATES CRASHED AND SUBDUCTION OCCURED

WHEN TWO PLATES SLIDE AGAINST EACH OTHER IN A SIDEWAYS MOTION

ROADS AND STRUCTURES MIGHT BE DAMAGED