BY: PAIGE MANN

THE LITHOSPHERE IS BROKEN INTO PIECES THAT MOVE

THE TRANSFER OF HEAT INTO AN AREA OF COOLER FLUID

THE MOTION THAT AIDS SUBDUCTION BY PULLING ON THE LAND

LESS DENSE CRUST FORMS AND PUSHES THE OLD OUT

TWO PLATES ARE MOVING AWAY FROM EACH OTHER

LAND FORM THAT RESULTS FROM A DIVERGENT PLATE BOUNDRY

UNDERWATER LANDFORM THAT IS CAUSED BY A DIVERGENT PLATE BOUNDRY

TWO PLATES ARE MOVING TOWARD EACH OTHER

~ OCEAN VS. CONTINENT PLATE MOVEMENT

OCEAN VS. OCEAN PLATE MOVEMENT

CONTINENT VS. CONTINENT PLATE MOVEMENT

COLLISION BETWEEN PLATES WHERE A PLATE SINKS INTO THE MANTLE UNDER THE OTHER

LONG NARROW STEEP-SIDED DEPRESSION IN THE EARTH'S OCEANIC CRUST

DEEP OCEAN TRENCH

LOCATIONS WHERE TWO PLATES SLIDE PAST ONE ANOTHER

EARTHQUAKES HAPPEN

RESULT FROM TRANSFORM BOUNDRY