BY: DANIEL OELBRACHT

THE THEORY THAT THE EARTH'S LITHOSPHERE IS BROKEN INTO MOVING PIECES

THE MOVEMENT OF FLUID, DUE TO VARIED TEMPERATURES

WHEN A PLATE SLAB IS PULLED DOWN TO THE MANTLE BY SUBDUCTION

NEW CRUST THAT RESULTS FROM DIVERGENT PLATE BOUNDARIES, PUSHING AWAY OLDER CRUST

PLATES THAT MOVE AWAY FROM EACH OTHER

LANDFORMS THAT RESULT FROM A DIVERGENT PLATE BOUNDARY

UNDERWATER LANDFORM THAT IS CAUSED BY A DIVERGENT PLATE BOUNDARY

PLATES THAT MOVE TOWARDS EACH OTHER

UNDERWATER LANDFORMS THAT RESULT FROM OCEAN V. OCEAN

A UNDERWATER LANDFORM THAT RESULTS FROM OCEAN V. CONTINENT

LANDFORMS THAT RESULT FROM CONTINENT V. CONTINENT

A CONVERGENT BOUNDARY WHERE A TECTONIC PLATE SLIDES UNDERNEATH ANOTHER

A GAP IN THE OCEAN FLOOR THAT RESULTS FROM SUBDUCTION

A DEEP-SEA TRENCH LOCATED NORTH OF THE PACIFIC PLATE

PLATES THAT SLIDE PAST THE OTHER

THE EVENT THAT RESULTS FROM A TRANSFORM PLATE BOUNDARY

A FAULT LOCATED ON THE EASTERN SIDE OF THE PACIFIC PLATE