tectonis plats
Published on Nov 28, 2015
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PRESENTATION OUTLINE
PLATE TECTONICS
PIECES OF THE LITHOSPHERE ARE IN SLOW CONSTANT MOTION
CONVECTION CURRENTD
THE FLOW THAT TRANSFERS HEAT THROUGH A FLUID
SLAB PULL
THE PULL OF GRAVITY ON A PLATE THAT IS BEING SUBDUCTED
RIDGE PUSH
NEW CRUST FORMS AND PUSHES THE OLD CRUST OUT OF THE WAY
DIVERGENT PLATE BOUNDRY
WHEN TWO TECTONIC PLATES ARE MOVING AWAY FROM EACH OTHER
RIFT VALLEY
A LANDFORM RESULTING FROM DIVERGENT PLATE BOUNDRY
MID-OCEAN RIDGE
RESULTING LANDFORM FROM DIVERGENT PLATE BOUNDR(SEA)
CONVERGENT PLATE BOUNDRY
TECTONIC PLATES MOVE TOWARD ONE ANOTHER AND COLLIDE
CHILE PERU DEEP SEA TRENCH
THE RESULT WHEN AN OCEAN PLATE AND A CONTINENTAL PLATE COLLIDE
MARIANA TRENCH(MARIANA ISLANDS)
THE RESULT WHEN TWO OCEANIC PLATES COLLIDE
HIMALAYAS
THE RESULT WHEN TWO CONTINENTAL PLATES COLLIDE
SUBDUCTION ZONE
TWO TECTONIC PLATES COLLIDE AND ONE SLIDES UNDERNEATH THE OTHER
DEEP OCEAN TRENCH
STEEP-SIDED DEPRESSION IN THE OCEAN BOTTOM
MARIANAS TRENCH
LOCATED IN THE MARIANA ISLANDS OF THE SOUTHEAST PACIFIC
TRANSFORM PLATE BOUNDARY
WHEN TWO TECTONIC PLATES SLIDE PAST EACH OTHER
RESULT OF TRANSFORM BOUNDARY
LITHOSPHERE IS NOT CREATED NOR DESTROYED
SAN ANDREAS FAULT
THE RESULTING EVENT FROM TRANSFORM PLATE BOUNDARY
