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Plate Tectonics

Published on Nov 22, 2015

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PRESENTATION OUTLINE

PLATE TECTONICS

PLATES THAT FLOAT ABOVE THE MANTLE

SUBDUCTION

OCCURS WHEN ONE PLATE MOVES UNDER ANOTHER

SLAB PULL

GRAVITY PULLING ON TECT. PLATES CAUSING MOVEMENT

RIDGE PUSH

NEWLY FORMED CRUST PUSHING OLD CRUST AWAY

DIVERGENT BOUNDRY

THE AREA BETWEEN TWO PLATES THAT HAVE SPLIT

ÁLFAGJÁ RIFT VALLEY

SOUTHWEST ICELAND

RED SEA

(A DIVERGENT PLATE BOUNDRY THAT RESULTED IN AN OCEAN

CONVERGENT BOUNDRY

DESTRUCTIVE PLATE BOUNDRY

CONVERGENT BOUNDRY

OCEAN VS. CONTINENT

CONVERGENT BOUNDRY

OCEAN VS. OCEAN

CONVERGENT BOUNDRY

CONTINENT VS. CONTINENT

SUBDUCTION ZONE

A COLLISION BETWEEN TWO OF EARTH'S TECTONIC PLATES

DEEP OCEAN TRENCH

LONG NARROW DEPRESSIONS IN THE SEA FLOOR

PUERTO RICO TRENCH

TRANSFORM PLATE BOUNDRY

WHERE TWO PLATES SLIDE PAST EACHOTHER

RESULTING EVENT OF TRANSFORM BOUNDRY

EARTHQUAKE

EXAMPLE OF TRANSFORM BOUNDRY

SAN ANDREAS FAULT

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