SQUEEZING FORCE AT A CONVERGENT BOUNDARY

HYPOTHESIS STATING THAT CONTINENTS MOVE

WHERE TWO PLANTS MOVE TOWARD EACH OTHER

WHERE TWO PLANTS MOVE APART FROM EACH OTHER

SIDE BY SIDE DRAGGING FORCE AT TRANSFORMS BOUNDARIES

AREA WHERE ONE PLATE SLIDES UNDER ANOTHER

PULLING FORCE AT A DIVERGENT BOUNDARY

LARGE DEPRESSION IN THE CENTER OF A VOLCANO

SURFACE ALONG WHICH THE CRUST MOVES

LOCATION WHERE VOLCANOES FORM FAR FROM PLATE BOUNDARIES

LONG STREAM OF MOLTEN ROCK

SMALL PIECES OF LAVA

RUPTURE AND SUDDEN MOVEMENT OF ROCKS ALONG EARTHS CRUST

TYPE OF MOUNTAIN THAT FORMS AS LAVA BUILDS UP A D COOLS

MINERALS AND SMALL PIECES OF ROCK