THE LITHOSPHERE IS BROKEN UP INTO SMALL PLATES THAT ARE MOVING.

THE CHANGE OF LIQUIDS DUE TO THEIR DENSITYS

WHEN GRAVITY PULLS A PLATE INTO THE MANTLE

WHEN THERE IS A DIVERGENT PLATE BOUNDRY AND LAVA FLOWS IN GAPS.

WHEN THE TWO PLATES ARE PULLING APART FROM EACH OTHER

LANDFORM THAT RESULTS FROM A DIVERGENT PLATE BOUNDRY

UNDERWATER LANDFORM THAT IS CAUSED BY DIVERGENT BOUNDRIES

IT IS WHERE TWO PLATES COLLIDE WITH EACH OTHER

WHEN TWO PLATES COLLIDE AND ONE SINKS BELOW THE OTHER.

A DEEP OCEAN TRENCH IS WHAT WOULD BE FORMED FROM SUBDUCTION

WHEN TWO CONTINENTAL PLATES COLLIDE AND MOVE UP

WHERE TWO PLATES COLLIDE AND ONE GOES UNDERNEATH.

WHEN A PLATE IS SUBDUCTED IN THE OCEAN A DEEP TRENCH IS MADE

THIS IS THE PUERTO RICO TRENCH

WHEN TWO PLATES SLIDE PAST EACH OTHER

FROMS WHEN TWO PLATES SLUDE PAST EACH OTHER

IS THE SAN ANDREAS FAULT