Title
Published on Mar 22, 2016
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MORE DECKS TO EXPLORE
PRESENTATION OUTLINE
PLATE TECTONICS
- Pieces of the Earth lithosphere in slow motion driven by convection currents
CAUSE OF MOVEMENT
CONVECTION CURRENTS
CAUSE OF MOVEMENT
GRAVITY PULLING ON THE PLATES IN THE SUBDUCTION ZONE
LAND FORM FROM DIVERGENT
RED SEA RIFT
LAND FORMING FROM DIVERGENT
LAKE TAGANYIKA IN EASTERN AFRICA
CONVERGENT BOUNDARY
THE PLACE WHERE TWO PLATES CONVERGE
LAND FORM OCEAN VS CONTINENT
NEW ZEALAND
LAND FORING FROM OCEAN VS OCEAN
HAWAII
SUBDUCTION ZONE
PLATE TECTONICS COMING TOGATHER
DEEP OCEAN TRENCH
A DEEP NARROW OPEANING IN THE OCEAN
DEEP OCAEN TRENCH
MARIANA TRENCH IN SYDNEY
TRANSFORM PLATE BOUNDARY
TWO PLATES HITTING PAST EACH OTHER
RESULTING IN TRANSFORM BOUNDARY
A CRACK IN THE EARTH CRUST
TRANSFORM BOUNDARY
SAN ANDREAS FAUL
