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Plate Tectonics

Published on Nov 18, 2015

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PRESENTATION OUTLINE

PLATE TECTONICS

BY AMANDA ROSE

PLATE TECTONICS

THE LITHOSPHERE IS BROKEN UP INTO PIECES THAT MOVE.

CONVECTION CURRENTS

THE TRANSFER OF HEAT THROUGH A FLUID
Photo by Waifer X

SLAB PULL

THE PULL OF GRAVITY ON A PLATE THAT IS BEING SUBDUCTED

RIDGE PUSH

NEW CRUST PUSHES OLDER CRUST OUT OF THE WAY AT DIVERGENT PLATE
Photo by nwpuzzlr

DIVERGENT PLATE BOUNDARIES

THE PLATES MOVE APART FROM EACH OTHER

GREAT RIFT VALLEY

RIFT VALLEY FORMED BY A DIVERGENT PLATE BOUNDARY, IN EAST AFRICA

MID OCEAN RIDGE

OCEAN RIDGE FORMED BY A DIVERGENT BOUNDARY, MID OCEAN RIDGE

CONVERGENT PLATE BOUNDARY

TWO PLATES COME TOGETHER

LANDFORM FROM OCEAN VS CONTINENT

TRENCH WITH A VOLCANIC ARC, CONVERGENT, ANDES MOUNTAIN

LANDFORM FROM OCEAN VS OCEAN

TRENCH ISLAND ARC OR UNDERWATER VOLCANIC ARC, MARIANA TRENCH

LANDFORM FROM CONTINENT VS CONTINENT

MOUNTAIN RANGE HIMALAYAS, CONVERGENT, (MT. EVEREST)

SUBDUCTION ZONE

COLLISION BETWEEN TWO PLATES WHERE A PLATE GOES UNDER THE OTHER

DEEP OCEAN TRENCH

LONG NARROW STEEP-SIDED DEPRESSION IN THE OCEANIC CRUST

TRANSFORM PLATE BOUNDARY

TWO PLATES THAT SLIDE PAST EACH OTHER

RESULTING EVENT FROM TRANSFORM BOUNDARY

FAULT

EXAMPLE OF TRANSFORM PLATE BOUNDARY

SAN ANDREAS FAULT