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Tectonic Plates

Published on Nov 22, 2015

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PRESENTATION OUTLINE

PLATE TECTONICS

PIECES OF THE LITHOSPHERE ARE IN SLOW CONSTANT MOTION

CONVECTION CURRENTS

THE FLOW THAT TRANSFERS HEAT THROUGH A FLUID

SLAB PULL

THE PULL OF GRAVITY ON A PLATE THAT IS BEING SUBDUCTED
Photo by Ken Lund



RIDGE PUSH

New crust pushes older denser crust out of the way as older, denser crust gets pulled away by gravity

DIVERGENT PLATE

WHEN TWO PLATES MOVE APART FROM EACH OTHER

RESULTING LANDFORM FROM A DIVERGENT PLATE BOUNDARY (LAND)

THE UPPER RHINE VALLEY IN GERMANY

RESULTING LANDFORM FROM A DIVERGENT PLATE BOUNDARY (SEA)

THE MID ATLANTIC RIDGE
Photo by jonathanpercy

CONVERGENT PLATE BOUNDARY

WHEN TWO PLATES COLLIDE TOWARDS EACH OTHER

RESULTING LANDFORM FROM OCEAN VS. OCEAN

MARIANAS TRENCH

RESULTING LANDFORM FROM OCEAN VS. CONTINENT

DEEP SEA TRENCH WITH ANDES MOUNTAINS

RESULTING CONTINENT FROM CONTINENT VS. CONTINENT

MOUNT EVEREST
Photo by watchsmart

SUBDUCTION ZONE

ONE PLATE SINKS INTO THE MANTLE UNDERNEATH THE OTHER PLATE

DEEP OCEAN TRENCH

A DEEP TRENCH THAT OCCURS DURING SUBDUCTION

DEEP OCEAN TRENCH EXAMPLE

JAPAN TRENCH

TRANSFORM PLATE BOUNDARY

WHEN TWO PLATES SLIDE PAST EACH OTHER

RESULTING EVENT FROM A TRANSFORM PLATE BOUNDARY

EARTHQUAKE
Photo by martinluff

EXAMPLE OF A TRANSFORM PLATE BOUNDARY

SAN ANDREAS FAULT