PRESENTATION OUTLINE
Plate tectonic definition:
The theory explaining the structure of the earth's crust and many associated phenomena as resulting from the interaction of rigid lithosphere plates that move slowly over the underlying mantle.
Divergent:
Seafloor spreading
Convergent:
Mountain building, volcanoes, deep ocean trench.
Convection currents in the mantle act like conveyor belts that drag the plates around.
Gravity pulls on the end of plates at subduction zones and pulls them toward the center of the earth.
New earth forms at divergent boundaries and pushes plates apart.
Divergent plate boundary:
A linear feature that exists between two tectonic plates that are moving away from each other.
Convergent plate boundary:
Is an actively deforming region where two (or more) tectonic plates or fragments of the lithosphere move toward one another and collide.
Ocean - continental
Trench with volcanic arch.
Ocean - Ocean
Trench with island arch or underwater volcanic arch.
Resulting landform
Continent vs. Continent
Mountain range
Subduction Zone:
The biggest smash-up on earth, marking the collision between two of the planet's tectonic plates, the pieces of the crust that slowly move across the surface over millions of years. When two tectonic plates meet, one may slide underneath the other, curving down into the mantle.
Deep Ocean Trench:
Oceanic crust is formed at an oceanic ridge, while the lithosphere is subducted back into the asthenosphere at trenches. The oceanic trenches are hemispheric-scale long but narrow topographic depressions of the sea floor. They are also the deepest parts of the ocean floor .
Resulting landform from divergent plate boundary (land)
Rift Valley
Resulting land form from divergent plate boundary
Mid-ocean ridge
Transform:
The crust is neither destroyed or formed.
Resulting landform from transform plate boundary:
Faults
Example of transform plate boundary: San Andreas Fault