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MORE DECKS TO EXPLORE
PRESENTATION OUTLINE
CONVECTION CURRENT
LESS DENS LIQUID RISES AND MORE DENSE LIQUIDS SINK
SLAB PULL
TECTONIC PLATES ARE CONSTANTLY BEING PULLED BY THE MANTLE
RIDGE PUSH
GRAVITY PULLS THE LITHOSPHERE UNDER ANOTHE PLATE FOM GRAVITY
On land divergent plate boundaries form rift valleys surounded by two ridges
In the ocean, divergent plate boundaries form mid ocean ridges
CONVERGENT PLATE BOUNDARY
TWO PLATES COLLIDE FORMING A MOUNTAIN RIDGE
When ocean and continental crust coverage they form a mountain arc like the Andes mountains.
When ocean and continental crust converge they form a volcanic arc like the aleutian islands off the coast of Alaska.
When continental crust converges with continental crust converge it forms mountains like the Himalayan
Mountains
SUBDUCTION ZONE
THE AREA WHERE CRUST IS SUCKED UNDER CRUST
DEEP OCEAN TRENCH
A LANDFORM SEEN ON THE SURFACE FROM SUBDUCTION LIKE THE MARIANNA
TRANSFORM PLATE BOUNDARY
TWO PLATES SLIDE ALONG EACH OTHER
