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Plate Tectonics By Hannah Parmertor
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Published on Nov 25, 2015
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PRESENTATION OUTLINE
1.
PLATE TECTONICS
PIECES OF THE LITHOSPHERE ARE IN SLOW CONSTANT MOTION
Photo by
Vytautas Šėrys
2.
CONVECTION CURRENTS
THE FLOW THAT TRANSFERS HEAT THROUGH A LIQUID
Photo by
Waifer X
3.
SLAB PULL
THE PULL OF GRAVITY ON A PLATE THAT IS BEING SUBDUCTED
4.
RIDGE PUSH
NEW, LESS DENSE CRUST FORMING AT DIVERGENT PLATE BOUNDARIES
Photo by
USDAgov
5.
DIVERGENT PLATE BOUNDARY
WHERE 2 PLATES MOVE AWAY FROM EACH OTHER AND NEW CRUST FORMS
Photo by
Glyn Lowe Photoworks.
6.
RIFT VALLEY
LAND FORM THAT RESULTS FROM A DIVERGENT PLATE BOUNDARY
Photo by
VanDerFoto
7.
MID OCEAN RIDGE
UNDERWATER LANDFORM THAT IS CAUSED BY A DIVERGENT PLATE BOUNDARY
8.
CONVERGENT PLATE BOUNDARY
PIECES OF THE LITHOSPHERE MOVE TOWARD EACH OTHER AND COLLIDE
Photo by
Stuck in Customs
9.
ANDES MOUNTAINS
OCEAN VS. CONTINENT. CONVERGENT PLATE BOUNDARY
Photo by
Piero...
10.
MARIANA AND JAPAN TRENCH
OCEAN VS. OCEAN. DIVERGENT BOUNDARY
11.
HIMALAYA MOUNTAINS
CONTINENT VS. CONTINENT. CONVERGENT PLATE BOUNDARY
Photo by
nandadevieast
12.
SUBDUCTION ZONE
ONE TECTONIC PLATE MOVES UNDER ANOTHER TECTONIC PLATE AND SINKS. CONVERGENT BOUNDARY
13.
DEEP OCEAN TRENCH
DEEPEST PART OF THE OCEAN. SITS ON THE SUBDUCTION ZONE
14.
MARIANA TRENCH
DEEP OCEAN TRENCH
15.
TRANSFORM PLATE BOUNDARY
WHERE PLATES SLIDE SIDEWAYS PAST EACH OTHER
16.
FAULTLINE
RESULTS OF A TRANSFORM BOUNDARY
Photo by
Travis S.
17.
SAN ANDREAS FAULTLINE
TRANSFORM BOUNDARY
Janice Karberg
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