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Theory of Plate Tectonics

      Plate Tectonics
     Plate Boundaries
  Causes of Plate Tectonics
Plate Tectonics
What is Plate Tectonics
• The Earth’s crust and upper
  mantle are broken into
  sections called plates
• Plates move around on top of
  the mantle like rafts
What is the Lithosphere?
• The crust and part of the upper
  mantle = lithosphere
 –100 km thick
 –Less dense than the material
  below it so it “floats”
What is the Asthenoshere?
• The plastic layer below the
  lithosphere = asthenosphere
• The plates of the lithosphere
  float on the asthenosphere
2 Types of Plates

• Ocean plates - plates below
  the oceans
• Continental plates - plates
  below the continents
Plate Boundaries
Divergent Boundaries
• Boundary between two plates
  that are moving apart or rifting
           
• RIFTING causes SEAFLOOR
  SPREADING
Features of Divergent
     Boundaries
• Mid-ocean ridges
• rift valleys
• fissure volcanoes
Convergent Boundaries
• Boundaries between two
  plates that are colliding
            
• There are 3 types…
Type 1
• Ocean plate colliding with a
  less dense continental plate
• Subduction Zone: where the
  less dense plate slides under
  the more dense plate
• VOLCANOES occur at
  subduction zones
Andes Mountains,
 South America
Type 2
• Ocean plate colliding with
  another ocean plate
• The less dense plate slides
  under the more dense plate
  creating a subduction zone
  called a TRENCH
Aleutian Islands, Alaska
Type 3
• A continental plate colliding
  with another continental plate
• Have Collision Zones:
 –a place where folded and thrust
  faulted mountains form.
Transform Fault Boundaries
• Boundary between two plates
  that are sliding past each other
• EARTHQUAKES along faults
San Andreas Fault, CA
Causes of Plate
  Tectonics
Convection Currents
• Hot magma in the Earth
  moves toward the surface,
  cools, then sinks again.
• Creates convection currents
  beneath the plates that cause
  the plates to move.
Naturalists at Large: Plate tectonics

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Naturalists at Large: Plate tectonics

  • 1.
  • 2. Theory of Plate Tectonics Plate Tectonics Plate Boundaries Causes of Plate Tectonics
  • 4. What is Plate Tectonics • The Earth’s crust and upper mantle are broken into sections called plates • Plates move around on top of the mantle like rafts
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  • 6. What is the Lithosphere? • The crust and part of the upper mantle = lithosphere –100 km thick –Less dense than the material below it so it “floats”
  • 7. What is the Asthenoshere? • The plastic layer below the lithosphere = asthenosphere • The plates of the lithosphere float on the asthenosphere
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  • 9. 2 Types of Plates • Ocean plates - plates below the oceans • Continental plates - plates below the continents
  • 11. Divergent Boundaries • Boundary between two plates that are moving apart or rifting  • RIFTING causes SEAFLOOR SPREADING
  • 12. Features of Divergent Boundaries • Mid-ocean ridges • rift valleys • fissure volcanoes
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  • 16. Convergent Boundaries • Boundaries between two plates that are colliding   • There are 3 types…
  • 17. Type 1 • Ocean plate colliding with a less dense continental plate • Subduction Zone: where the less dense plate slides under the more dense plate • VOLCANOES occur at subduction zones
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  • 20. Type 2 • Ocean plate colliding with another ocean plate • The less dense plate slides under the more dense plate creating a subduction zone called a TRENCH
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  • 23. Type 3 • A continental plate colliding with another continental plate • Have Collision Zones: –a place where folded and thrust faulted mountains form.
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  • 26. Transform Fault Boundaries • Boundary between two plates that are sliding past each other • EARTHQUAKES along faults
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  • 29. Causes of Plate Tectonics
  • 30. Convection Currents • Hot magma in the Earth moves toward the surface, cools, then sinks again. • Creates convection currents beneath the plates that cause the plates to move.