Science 1 Mick Lindner 4th period
Published on Nov 19, 2015
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PRESENTATION OUTLINE
PLATE TECTONICS
LITHOSPHERIC PIECES THAT ARE IN CONSTANT MOTION
CONVECTION CURRENTS
THE FLOW THAT TRANSFERS HEAT THROUGH A FLUID
SLAB PULL
A FORCE THAT PULLS A PLATE UNDER ANOTHER
RIDGE PUSH
NEW CRUST FORMING AT A DIVERGENT PLATE BOUNDARY THAT PUSHES OLDER CRUST OUT OF THE WAY
DIVERGENT PLATE BOUNDARY
PLATES PULLING APART
RIFT VALLEY
WHEN TWO PLATES COLLIDE IT FORMS ALANDFORM OF A DIVERGENT VALLEY
MID OCEAN RIDGE
AN UNDERWATER MOUNTAIN RANGE CAUSED BU A DIVERGENT PLATE BOUNDARY
CONVERGENT PLATE BOUNDARY
WHEN LITHOSPHERIC PLATES COLLIDE WITH EACH OTHER
TRENCHES
A LONG NARROW DITCH THAT FORMS WHEN PLATES MOVE APART.
DEEP OCEAN TRENCH
A TRENCH IN THE MIDDLE OF THE OCEAN THAT HAPPENS WHEN THERE IS DIVERGENT PLATES
LAND-OCEAN TRENCH
A TRENCH THAT FORMS WHEN OCEANIC AND CONTINENTAL PLATES COLLIDE
SUBDUCTION ZONE
A LANDFORM THAT HAPPENS WHEN THERE IS A COLLISION BETWEEN TECTONIC PLATES
DEEP OCEAN TRENCH
WHEN PLATES PULL APART. OFF THE COAST OF PEURTO RICO
TRANSFORM PLATE BOUNDARY
WHEN PLATES SLIDE PAST EACH OTHER
