Plate Tectonics
Published on Nov 19, 2015
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PRESENTATION OUTLINE
PLATE TECTONICS
IS THE THEORY OF THE EARTH BEING CUT INTO PIECES
CONVECTION CURRENTS
A LIQUID CURRENT THE RAISE AND LOWERS BASED ON ITS TEMPERATURE
SLAB PULL
GRAVITY PULLING ON A SUBDUCTING PLATE
RIDGE PUSH
THE SLIDING OF THE PLATES BECAUSE OF THE MID-OCEAN RIDGE
DIVERGENT PLATE BOUNDARY
IS WHEN 2 PLATE MOVE AWAY FROM EACH OTHER
MID OCEAN RIDGE
A WAY FOR A DIVERGENT BOUNDARYS TO MOVE APART IN THE SEA
Photo by Ocean Networks Canada
CONVERGENT PLATE BOUNDARY
WHERE LITHOSPHERE MOVE TOWARD ONE ANOTHER AND COLLIDE
DEEP SEA TRENCHES
DEEP DEPRESSION IN THE OCEAN FLOOR
SUBDUCTION
THE PROCESS THAT TAKES PLACE AT CONVERGENT BOUNDARY
MOUNTAIN BUILDING
AN AREA OF LAND THAT RISES ABRUPTLY FROM THE SURROUNDING REGION
SUBDUCTION ZONE
THE PROCESS THAT TAKES PLACE AT CONVERGENT BOUNDARY
DEEP OCEAN TRENCH
DEEP DEPRESSION IN THE OCEAN FLOOR
THE MARIANA TRENCH
A TYPE OF TRENCH IN THE OCEAN
PLATE BOUNDARY
LITHOSPHERE OF THE EARTH IS BROKEN INTO VARIOUS PLATES
TRANSFORM BOUNDARY
CRUST THAT IS NOT DESTROYED NOR CREATED
ALPINE FAULT
A FAULT THAT HAD FORMED IN NEW ZELAND
