SQUEEZING FORCE AT A CONVERGENT BOUNDARY

HYPOTHESIS STATING THAT CONTINENTS MOVE

WHERE TWO PLATES MOVE TOWARD EACH OTHER

WHERE TWO PLATES MOVE APART FROM EACH OTHER

STATES THAT EARTH’S CRUST IS BROKEN INTO RIGID PLATES THAT MOVE SLOWLY OVER EARTH’S SURFACE

SIDE-BY-SIDE DRAGGING FORCE AT TRANSFORM BOUNDARIES

AREA WHERE ONE PLATE SLIDES UNDER ANOTHER

PULLING FORCE AT A DIVERGENT BOUNDARY

WHERE PLATES SLIDE HORIZONTALLY PAST EACH OTHER

LARGE DEPRESSION IN THE CENTER OF A VOLCANO

RUPTURE AND SUDDEN MOVEMENT OF ROCKS ALONG A BREAK OR A CRACK IN EARTH’S CRUST

SURFACE ALONG WHICH THE CRUST MOVES

LOCATION WHERE VOLCANOES FORM FAR FROM PLATE BOUNDARIES

LONG STREAM OF MOLTEN ROCK

TYPE OF MOUNTAIN THAT FORMS AS LAVA BUILDS UP AND COOLS