PIECES OF THE LITHOSPHERE ARE IN SLOW CONSTANT MOTION

THE FLOW THAT TRANSFERS HEAT THROUGH A LIQUID

THE PULL OF GRAVITY ON A PLATE THAT IS BEING SUBDUCTED

NEW, LESS DENSE CRUST FORMING AT DIVERGENT PLATE BOUNDARIES

WHERE 2 PLATES MOVE AWAY FROM EACH OTHER AND NEW CRUST FORMS

LAND FORM THAT RESULTS FROM A DIVERGENT PLATE BOUNDARY

UNDERWATER LANDFORM THAT IS CAUSED BY A DIVERGENT PLATE BOUNDARY

PIECES OF THE LITHOSPHERE MOVE TOWARD EACH OTHER AND COLLIDE

OCEAN VS. CONTINENT. CONVERGENT PLATE BOUNDARY

OCEAN VS. OCEAN. DIVERGENT BOUNDARY

CONTINENT VS. CONTINENT. CONVERGENT PLATE BOUNDARY

ONE TECTONIC PLATE MOVES UNDER ANOTHER TECTONIC PLATE AND SINKS. CONVERGENT BOUNDARY

DEEPEST PART OF THE OCEAN. SITS ON THE SUBDUCTION ZONE

DEEP OCEAN TRENCH

WHERE PLATES SLIDE SIDEWAYS PAST EACH OTHER

RESULTS OF A TRANSFORM BOUNDARY

TRANSFORM BOUNDARY