TOMMY FRAZIER 2ND PERIOD

PIECES OF THE EARTHS LITSHOSPHERE THATE ARE IN SLOW CONSTANT MOTION DRIVEN BY CONVECTION CURRENTS, GRAVITY, AND SEA FLOOR SPREADING.

GRAVITY PULLING ON THE PLATES IN THE SUBDUCTION ZONE HELP MOVE THE PLATES. (SLAP PULL)

NEW CRUST FORMING PUSHES THE TECTONIC PLAGES APART. (RIDGE PUSH)

THE TRANSFER OF HEAT BY THE MASS MOVEMENT OF HEATED PARTICLES INTO AN AREA OF COOLER FLUID

BOUNDARY WHERE THE PLATES ARE MOVING APART

RESULTING LAND FORM FROM DIVERGENT PLATE BOUNDARY. (LAND)

RESULTING LANDFORM FROM DIVERGENT PLATE BOUNDARY . (SEA)

THE PLACE WHERE TWO PLATES CONVERGE

RESULTING LANDFORM FROM OCEAN VS CONTINENT (CONVERGENT PLATE BOUNDRY)

RESULTING LANDFORM FROM OCEAN VS OCEAN. (CONVERGENT PLATE BOUNDARY)

RESULTING LAND FORM FROM CONTINENT VS CONTINENT. (CONVERGENT PLATE BOUNDARY)

THE PROCESS IN WHICH A PLATE SINKS BENEATH A DEEP OCEAN TRENCH AND IN TO THE MANTLE

A LONG DEEP DEPRESIION ON THE OCEAN FLOOR

EXAMPLE OF DEEP OCEAN TRENCH

PLACE WHERE TWO PLATES SLIDE PAST EACH OTHER

AN RESULTING EVENT FBROM TRANSFORM PLATE BOUNDARY