THE LITHOSPHERE IS BROKEN INTO PIECES THAT MOVE IN A SLOW CONSTANT MOTION

FLOW THAT TRANSFERS HEAT WITHIN A FLUID. HOT, MORE DENSE, RISES. COLD, LESS DENSE, SINKS

GRAVITY PULLS ON THE ENDS OF PLATES AT SUBSUCTION ZONES AND PULLS THEM TOWARD THE CENTER OF EARTH.

NEW, LESS DENSE CRUST FORMS AT DIVERGENT BOUNDARIES BY PUSHING OLDER, DENSER CRUST OUT OF THE WAY

BOUNDARY WHERE PLATES ARE MOVING APART FROM EACH OTHER

LANDFORM RESULTING FROM THE DIVERGENT BOUNDARY BETWEEN THE EURASIAN AND NORTH AMERICAN PLATES

LANDFORM RESULTING FROM DIVERGENT PLATE BOUNDARIES THAT PUSHED ARABIA AND EGYPT APART FORMING THE RED SEA

PLACE WHERE TWO PLATES CONVERGE (COLLIDE)

LANDFORM LOCATED IN BETWEEN GREECE AND PELOPONNESE TO TURKEY RESULTING FROM CONVERGENT OCEANIC & CONTINENTA.L PLATE BOUNDARIES

LANDFORM IN-BETWEEN KAMCHATKA AND ALASKA RESULTING FROM OCEAN VS OCEAN CONVERGENT PLATES

LAND FORM RESULTING FROM CONTINENTAL CONVERGENT PLATES. PASSES THROUGH INDIA, PAKISTAN, AFGHANISTAN, CHINA, BHUTAN, AND NEPAL

PLACE WHERE TWO PLATES COME TOGETHER, ONE SINKING BENEATH THE OTHER BACK INTO THE MANTLE

LONG, NARROW, STEEP-SIDED DEPRESSION IN THE OCEAN BOTTOM THAT FORM WHEN ONE PLATE SUBDUCTS UNDER ANOTHER

LANDFORM RESULTING FROM SUBDUCTION AND CONVERGENT OCEAN PLATE BOUNDARIES. LOCATED IN NORTH PACIFIC OCEAN EAST OF THE MARIANA ISLANDS.

TWO PLATES SLIDE PAST EACH OTHER

RESULTING EVENT FROM A TRANSFORM BOUNDARY WHERE 2 PLATES SLIDE PAST EACH OTHER

LANDFORM RESULTING FROM A TRANSFORM PLATE BOUNDARY. LOCATED IN THE EAST SIDE OF CALIFORNIA.