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The theory that states that pieces
of Earth’s lithosphere are in
constant, slow motion, driven by
convection currents in the mantle.
• The theory of plate
tectonics explains the
formation, movement,
and subduction of
Earth’s plates.
Forces that causes Earth’s
        plates to move.
• The plates of the lithosphere
float on top of the Asthenosphere.
• Convection currents rise in the
Asthenosphere and spread out
beneath the lithosphere.
Forces that causes Earth’s
  plates to move (continued).
•Convection current forces drag the
overlying plates along. The currents cool
and sink deeper into the mantle.
• Scientist think that the downward
movement may provide the force that
causes the subduction of plates carrying
oceanic crust.
QuickTime™ and a
          decompressor
are needed to see this picture.
Forces that causes Earth’s
     plates to move.
Slab Push Hypothesis
• Magma rising along the mid oceanic
ridge exerts a force that pushes an oceanic
plate away from the ridge.
• The force of gravity causes plate
movement by pulling cooler, denser
oceanic plates down toward the mantle.
• Slab push and pull work together with
convection currents to move the plates.
The earth’s surface is made
up of about nine large plates
 & several smaller plates.
Places where two plates meet.
There are three types of
 plate boundaries.
1. Transform Boundary
2. Divergent Boundary
3. Convergent Boundary
Two plates slip past each
other, moving in opposite
directions.
Earthquakes occur frequently
 along transform boundary.
The San
Andreas
fault in
California is
an example
of a
transform
boundary.
Two plates move away from
each other.
• When a divergent boundary
develops on land, two of
Earth’s plates slide apart.
• A rift valley forms along the
divergent valley.
• Ex. The Great Rift Valley in
east Africa is about 3,000
kilometers long.
Two plates move towards
      each other.
• When plates converge, it
 results in a collision.
 • Collisions happen between:
1. Oceanic crust to oceanic crust
2. Oceanic crust to continental crust
3. Continental crust to continental crust
This can happen where oceanic crust
        meets oceanic crust.
This can happen where oceanic crust
      meets continental crust.
This can happen where continental
  crust meets continental crust.
Plate Movement
• The plates move at about 1-10
centimeters per year.
• The North American and
Eurasian plates move at about 2.5
cm/year.
Plate Movement
• Pangaea existed about
260 million years ago.
• Approximately 225
million years ago Pangaea
began to break apart.
Plate Movement




http://www.classzone.com/books/earth_science/terc/content/visua
http://www.ucmp.berkeley.edu/geology/anim1.html

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Plate Tectonics (Jenny)

  • 1.
  • 2. The theory that states that pieces of Earth’s lithosphere are in constant, slow motion, driven by convection currents in the mantle.
  • 3. • The theory of plate tectonics explains the formation, movement, and subduction of Earth’s plates.
  • 4. Forces that causes Earth’s plates to move. • The plates of the lithosphere float on top of the Asthenosphere. • Convection currents rise in the Asthenosphere and spread out beneath the lithosphere.
  • 5. Forces that causes Earth’s plates to move (continued). •Convection current forces drag the overlying plates along. The currents cool and sink deeper into the mantle. • Scientist think that the downward movement may provide the force that causes the subduction of plates carrying oceanic crust.
  • 6. QuickTime™ and a decompressor are needed to see this picture.
  • 7. Forces that causes Earth’s plates to move.
  • 8. Slab Push Hypothesis • Magma rising along the mid oceanic ridge exerts a force that pushes an oceanic plate away from the ridge. • The force of gravity causes plate movement by pulling cooler, denser oceanic plates down toward the mantle. • Slab push and pull work together with convection currents to move the plates.
  • 9. The earth’s surface is made up of about nine large plates & several smaller plates.
  • 10.
  • 11. Places where two plates meet.
  • 12.
  • 13. There are three types of plate boundaries. 1. Transform Boundary 2. Divergent Boundary 3. Convergent Boundary
  • 14. Two plates slip past each other, moving in opposite directions.
  • 15. Earthquakes occur frequently along transform boundary.
  • 16. The San Andreas fault in California is an example of a transform boundary.
  • 17. Two plates move away from each other.
  • 18. • When a divergent boundary develops on land, two of Earth’s plates slide apart. • A rift valley forms along the divergent valley. • Ex. The Great Rift Valley in east Africa is about 3,000 kilometers long.
  • 19.
  • 20. Two plates move towards each other.
  • 21. • When plates converge, it results in a collision. • Collisions happen between: 1. Oceanic crust to oceanic crust 2. Oceanic crust to continental crust 3. Continental crust to continental crust
  • 22. This can happen where oceanic crust meets oceanic crust.
  • 23. This can happen where oceanic crust meets continental crust.
  • 24. This can happen where continental crust meets continental crust.
  • 25. Plate Movement • The plates move at about 1-10 centimeters per year. • The North American and Eurasian plates move at about 2.5 cm/year.
  • 26. Plate Movement • Pangaea existed about 260 million years ago. • Approximately 225 million years ago Pangaea began to break apart.