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Plate Tectonics

Published on Nov 21, 2015

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PRESENTATION OUTLINE

ASTHENOSPHERE

PLASTICLIKE LAYER BELOW THE LITHOSPHERE

CONTINENTAL DRIFT

CONTINENTS HAVE MOVED SLOWLY TO THEIR CURRENT LOCATION.

CONVECTION CURRENT

THIS ENTIRE CYCLE OF HEATING, RISING, COOLING, AND SINKING

LITHOSPHERE

THIS RIGID LAYER IS ABOUT 100KM THICK AND GENERALLY IS LESS DENSE.

PANGAEA

IT MEANS ALL LAND

PLATE

MOVE ON A PLASTICLIKE LAYER OF THE MANTLE.

PLATE TECHTONICS

EARTHS CRUST AND PART OF THE UPPER MANTLE ARE BROKE INTO SECTIONS.

SEAFLOOR SPREADING

PROPOSED THAT HOT LESS DENSE MATERIAL BELOW EARTH CRUST RISES.