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Plate Tectonics

Published on Nov 23, 2015

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PRESENTATION OUTLINE

PLATE TECTONICS

THE THEORY THAT THE EARTH IS DIVIDED INTO PLATES ON THE MANTLE
Photo by Dominkab

CAUSE OF MOVEMENT #1

CONVECTION CURRENTS : MOVE IN A CONVEYOR BELT MOTION DUE TO HEAT

CAUSE OF MOVEMENT #2

SLAB PULL: A PLATE IS SLOWLY MOVING UNDER AN OTHER DUE TO GRAVITY

DIVERGENT

PLATES MOVE AWAY FROM EACH OTHER

CAUSE OF MOVEMENT #3

RIDGE PUSH: NEW CRUST FORMS AT A DIVERGENT BOUNDARY
Photo by Ken Lund

RIFT VALLEY

LAND FORM RESULT FROM A DIVERGENT BOUNDARY

MID OCEAN RIDGE

UNDER WATER LAND FORM CAUSED BY DIVERGENT BOUNDARY

CONVERGENT BOUNDARY

PLATES MOVE TOWARD EACH OTHER

DEEP OCEAN TRENCH

AN EXAMPLE IS THE MARIANA TRENCH

VOLCANIC ISLAND ARC

OCEAN VS OCEAN AN EXAMPLE IS HAWAIIAN AND ALASKAN ISLAND

MOUNTAIN RANGE

CON. VS CON. AN EXAMPLE IS THE ROCKY MOUNTAINS

SUBDUCTION ZONES

DEFINITION: WHEN TWO CONTINENTAL PLATES CRASH AND ONE SINKS

DEEP OCEAN TRENCH

DEFINITION: A STEEP DROP IN THE OCEAN FLOOR

DEEP OCEAN TRENCH

EXAMPLE: THE MARIANA TRENCH

TRANSFORM PLATE BOUNDARY

DEFINITION: WHEN A PLATE SLIDES PAST AN OTHER PLATE

A FAULT

TRANSFORM BOUNDARIES RESULT IN A FAULT IN THE CRUST

SAN ANDREAS FAULT

EXAMPLE OF A TEANSFORM BOUNDARY