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Plate Tectonics

Published on Dec 09, 2015

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PRESENTATION OUTLINE

PLATE TECTONICS

Pieces of the lithosphere are in slow, constant motion.
Photo by Ben+Sam

CONVECTION CURRENTS

The flow that transfers heat through a fluid
Photo by williamhartz

SLAB PULL

The pull of gravity on a plate that is being subducted
Photo by Dru!

RIDGE PUSH

New, less dense crust forming at divergent boundaries and pushing older crust out .

DIVERGENT BOUNDARY

PLATES MOVE AWAY FROM EACH OTHER

RIFT VALLEY

LAND RESULT OF DIVERGENT BOUNDARY
Photo by VanDerFoto

EAST AFRICAN RIFT VALLEY

EXAMPLE OF DIVERGENT PLATE BOUNDARY

MID OCEAN RIDGE

UNDERWATER RESULT OF DIVERGENT BOUNDARY

CONVERGENT BOUNDARY

TWO OR MORE PLATESMOVE TOWARDS EACH OTHER AND COLLIDE
Photo by pmlbird

MOUNTAIN RANGE

RESULT OF CONTINENTAL CRUST VS. CONTINENTAL CRUST

TRENCH &ISLAND ARCH

RESULT OF OCEANIC CRUST VS. OCEANIC CRUST

SUBDUCTION ZONE

THE PLACE WHERE TECTONIC PLATES COLLIDE AND SINK INTO THE MANTLE

DEEP OCEAN TRENCH

A LONG, NARROW, STEEP SIDED DEPRESSION ON THE OCEAN BOTTOM

MARIANA TRENCH

EXAMPLE OF A DEEP OCEAN TRENCH

TRANSFORM BOUNDARY

PLACE WHERE TWO PLATES SLIDE PAST EACH OTHER

FAULT

RESULT OF A TRANSFORM BOUNDARY

SAN ANDREAS FAULT

EXAMPLE OF A TRANSFORM BOUNDARY