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Plate Tectonics
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Published on Nov 21, 2015
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PRESENTATION OUTLINE
1.
ASTHENOSPHERE
PLASTICLIKE LAYER BELOW THE LITHOSPHERE
2.
CONTINENTAL DRIFT
CONTINENTS HAVE MOVED SLOWLY TO THEIR CURRENT LOCATION.
3.
CONVECTION CURRENT
THIS ENTIRE CYCLE OF HEATING, RISING, COOLING, AND SINKING
4.
LITHOSPHERE
THIS RIGID LAYER IS ABOUT 100KM THICK AND GENERALLY IS LESS DENSE.
5.
PANGAEA
IT MEANS ALL LAND
6.
PLATE
MOVE ON A PLASTICLIKE LAYER OF THE MANTLE.
7.
PLATE TECHTONICS
EARTHS CRUST AND PART OF THE UPPER MANTLE ARE BROKE INTO SECTIONS.
8.
SEAFLOOR SPREADING
PROPOSED THAT HOT LESS DENSE MATERIAL BELOW EARTH CRUST RISES.
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