THE DYNAMICS OF PLATE MOVEMENT

THE FLOW THAT TRANSFERS HEAT THROUGH A FLUID

GRAVITY PULLING ON A SUBDUCTING PLATE

NEW CRUST FORMING PUSHES OLDER CRUST OUT OF ITS WAY

PLATES MOVE AWAY FROM EACH OTHER

LAND FORM THAT RESULT FROM A DIVERGENT PLATE BOUNDARY

UNDERWATER LANDFORM THAT WAS CAUSE BY DIVERGENT PLATE BOUNDARY

TWO TECTONIC PLATES MOVE TOWARD ONE ANOTHER AND COLLIDE

IS AN OCEANIC TRENCH IN THE EASTERN PACIFIC OCEAN

THE DEEPEST PART OF THE WORLD'S OCEANS, ITS LOCATED IN THE WEST

TWO LANDMASSES MET,THE TERRAIN WAS FORCED UPWARD TO CREATE THE

COLLISION OF THE EARTH'S CRUSTAL PLATES

HEMISPHERIC-SCALE LONG BUT THIN OF THE SEA FLOOR

REACHES A MAXIMUM DEPTH OF 8,065 METRES BELOW SEA LEVEL

WHEN TWO PLATES SLIDE PAST EACH OTHER

MASSIVE AMOUNTS OF ENERGY ARE BULIT UP

CONTINENTAL TRANSFORM FAULT THAT EXTENDS ROUGHLY 810 MILES