PIECES OF THE LITHOSPHERE ARE IN SLOW CONSTANT MOTION

THE FLOWTHAT TRANSFERS HEAT THROUGH A FLUID

THE PULL OF GRAVITY ON A PLATE THAT IS BEING SUBDUCTED

NEW LESS DENSE CRUST FORMING AT DIVERGENTPLATE BOUNDARIES PUSHES OLDER CRUST OUT OF THE WAY

PLATES MOVE AWAY FROM EACH OTHER

LAND FORM THAT RESULTS FROM A DIVERGENT PLATE BOUNDARY

UNDERWATER LANDFORM THAT IS CAUSED BY A DIVERGENT PLATE BOUNDARY

PLATES MOVE TOWARDS EACH OTHER

FORMS WHEN OCEANIC CRUST CONVERGES WITH CONTINENTAL CRUST

FORMED WHEN OCEANIC CRUST AND OCEANIC CRUST CONVERGED

FORMED WHEN CONTINENTAL CRUST AND CONTINENTAL CRUST CONVERGED

AN AREA WHERE TWO PLATES COLLIDE AND ONE SLIDES UNDER THE OTHER

NARROW TOPOGRAPHIC DEPRESSIONS OF THE SEA FLOOR

IS AN EXAMPLE OF A DEEP OCEAN TRENCH

PLATES THAT SLIDE PAST EACH OTHER

A RESULT OF TRANSFORM BOUNDARY, AN EXAMPLE IS THE SAN ANDREAS FAULT

IS AN EXAMPLE OF A TRANSFORM BOUNDARY