Tectonic Plates
Published on Apr 19, 2016
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PRESENTATION OUTLINE
MATTHEW BRANTHOOVER
PERIOD 2
PLATE TECTONICS
THE MOVEMENT OF PLATES IN THE UPPER LITHOSPHERE
CONVECTION CURRENTS IN THE MANLE
A CURRENT IN THE MANTLE FORMED BY CONVECTION
GRAVITY
GRAVITY PULLING ON THE SUBDUCTION ZONES ALSO HELPS MOVE THEM
SEA FLOOR SPREADING
NEW CRUST PUSHES THE TECTONIC PLATES APART
DIVERGENT
A PLATE BOUNDARY WHERE THEY ARE MOVING APART
DIVRGENT PLATE BOUNDARIES ON LAND
THE SAINT ANDREAS FAULT LINE
DIVERGENT PLATE BOUNDARIES IN THE SEA
A BRIDGE IN ICELAND CONECTING THE TWO PLATES
CONVERGENT PLATE BOUNDARY
WHEN TO PLATES COLLIDE IT IS A CONVERGENT PLATE
CONVERGENT OCEAN TO CONTINENT
IN SOUTH AMERICA AN OCEAN PLATE AND A LAND PLATE ARE COLLIDING
CONVERGENT OCEAN TO OCEAN
A VOLCANIC ISLAND IN OCEANA
CONVERGENT CONTINENT TO CONTINENT
MOUNT EVEREST IS STILL GROWING ABOUT AN INCH A YEAR
SUBDUCTION ZONE
THE COLLISION BETWEEN TWO OF THE PLANET'S TECTONIC PLATES
DEEP OCEAN TRENCH
ANY LONG, NARROW, STEEP-SIDED DEPRESSION IN THE OCEAN BOTTOM
DEEP OCEAN TRENCH EXAMPLE
THE MARIANA TRENCH
TRANSFORM PLATE BOUNDARY
TWO PLATES MOVE PAST EACH OTHER
RESULTS FROM TRANSFORM PLATE BOUNDARY
THE SAN ANDREAS FAULT
EXAMPLES OF TRANSFORM BOUNDARIES
THE SAN ANDREAS FAULT BETWEEN SAN FRANCISCO AND CALIFORNIA
