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Plate Tectonics by Matthew Brown
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Published on Nov 20, 2015
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PRESENTATION OUTLINE
1.
PLATE TECTONICS
PIECES OF THE LITHOSPHERE ARE IN SLOW CONSTANT MOTION
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BlatantWorld.com
2.
CONVECTION CURRENT
THE FLOWTHAT TRANSFERS HEAT THROUGH A FLUID
3.
SLAB PULL
THE PULL OF GRAVITY ON A PLATE THAT IS BEING SUBDUCTED
4.
RIDGE PUSH
NEW LESS DENSE CRUST FORMING AT DIVERGENTPLATE BOUNDARIES PUSHES OLDER CRUST OUT OF THE WAY
5.
DIVERGENT PLATE BOUNDARY
PLATES MOVE AWAY FROM EACH OTHER
6.
RIFT VALLEY
LAND FORM THAT RESULTS FROM A DIVERGENT PLATE BOUNDARY
7.
MID-OCEAN RIDGE
UNDERWATER LANDFORM THAT IS CAUSED BY A DIVERGENT PLATE BOUNDARY
8.
CONVERGENT PLATE BOUNDARY
PLATES MOVE TOWARDS EACH OTHER
9.
VOLCANIC ARC
FORMS WHEN OCEANIC CRUST CONVERGES WITH CONTINENTAL CRUST
10.
SOLOMON ISLAND
FORMED WHEN OCEANIC CRUST AND OCEANIC CRUST CONVERGED
11.
MT. EVEREST
FORMED WHEN CONTINENTAL CRUST AND CONTINENTAL CRUST CONVERGED
12.
SUBDUCTION ZONE
AN AREA WHERE TWO PLATES COLLIDE AND ONE SLIDES UNDER THE OTHER
13.
DEEP OCEAN TRENCH
NARROW TOPOGRAPHIC DEPRESSIONS OF THE SEA FLOOR
14.
THE ALEUTIAN TRENCH
IS AN EXAMPLE OF A DEEP OCEAN TRENCH
15.
TRANSFORM PLATE BOUNDARY
PLATES THAT SLIDE PAST EACH OTHER
16.
FUALT
A RESULT OF TRANSFORM BOUNDARY, AN EXAMPLE IS THE SAN ANDREAS FAULT
17.
SAN ANDREAS FAULT
IS AN EXAMPLE OF A TRANSFORM BOUNDARY
Matthew Brown
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