PEICES OF THE LITHOSPHERE ARE IN SLOW CONSTANT MOTION

THE FLOW THAT TRANSFERS HEAT THROUGH A FLUID

THE PULL OF GRAVITY ON A PLATE THAT IS BEING SUBDUCTED

NEW CRUST FORMING AT DIVERGENT PLATE BOUNDARIES PUSHES THE OLD CRUST OUT

PLATES MOVE AWAY FROM EACHOTHER

LAND FORM THAT RESULTS FROM A DIVERGENT PLATE BOUNDARY

UNDERWATER LANDFORM THAT IS CAUSED BY A DIVERGENT PLATE BOUNDARY

WHEN TWO PLATES COME TOGETHER

RESULTING TRENCH OF OCEAN VS CONTINENT

RESULT OF OCEANIC VS OCEANIC

RESULT OF CONTINENT VA CONTINENT

COLLOSION OF THE EARTHS CRUSTAL PLATES

ANY LONG NARROW STEEP SIDED DEPRESSION IM THE OCEAN BOTTOM

PERUVIAN TRENCH

A FAULT THAY IS NEITHER CREATED OR DESTROYED

MASSIVE AMOUNTS OF ENERGY BUILD UP

SAN ANDREAS FAULT