Theory of Plate
  Tectonics
The crust (rocky and
rigid) is divided into
“plates” that move over the
mantle (that is plastic
like).
Boundary Fault   Plate     Creates
                           (o=ocean &
                 Direction c=continental)
Boundary Fault       Plate     Creates
                               (o=ocean &
                     Direction c=continental)
Divergent   Normal   Pull or Moving   Seafloor Spreading
                     Apart            (O vs. O)
                                      Or Valley (C vs. C)
Boundary Fault       Plate     Creates
                               (o=ocean &
                     Direction c=continental)
Divergent   Normal   Pull or Moving   Seafloor Spreading
                     Apart            (O vs. O)
                                      Or Valley (C vs. C)
Boundary Fault         Plate     Creates
                       Direction (o=ocean &
                                 c=continental)
Divergent    Normal    Pull or Moving   Seafloor Spreading
                       Apart            (O vs. O)
                                        Or Valley (C vs. C)

Convergent   Reverse   Move Together    Subduction Zone/
                                        Trench / Volcanoe
                                        (C vs. O)
                                        Mountain (C vs. C)
Oceanic-Continental Convergence
Boundary Fault         Plate     Creates
                       Direction (o=ocean &
                                 c=continental)
Divergent    Normal    Pull or Moving   Seafloor Spreading
                       Apart            (O vs. O)
                                        Or Valley (C vs. C)

Convergent   Reverse   Move Together    Subduction Zone/
                                        Trench / Volcanoe
                                        (C vs. O)
                                        Mountain (C vs. C)
Boundary Fault             Plate     Creates
                           Direction (o=ocean &
                                     c=continental)
Divergent    Normal        Pull or Moving    Seafloor Spreading
                           Apart             (O vs. O)
                                             Or Valley (C vs. C)

Convergent   Reverse       Move Together     Subduction Zone/
                                             Trench / Volcanoe
                                             (C vs. O)
                                             Mountain (C vs. C)

Transform    Strike-Slip   Slide Alongside   Earthquake and
                           One Another       Faultline
 Scientist believe convection currents
 move the plates by the hot material in
 the mantle rising and as it cools it
 carries the plates along with it until it
 sinks and starts the process all over
 again.
Previously scientists knew
 plates were moving, but new
 methods use lasers and
 satellites to measure precise
 movements.

Pc chapter 7-3

  • 1.
  • 3.
    The crust (rockyand rigid) is divided into “plates” that move over the mantle (that is plastic like).
  • 4.
    Boundary Fault Plate Creates (o=ocean & Direction c=continental)
  • 5.
    Boundary Fault Plate Creates (o=ocean & Direction c=continental) Divergent Normal Pull or Moving Seafloor Spreading Apart (O vs. O) Or Valley (C vs. C)
  • 7.
    Boundary Fault Plate Creates (o=ocean & Direction c=continental) Divergent Normal Pull or Moving Seafloor Spreading Apart (O vs. O) Or Valley (C vs. C)
  • 8.
    Boundary Fault Plate Creates Direction (o=ocean & c=continental) Divergent Normal Pull or Moving Seafloor Spreading Apart (O vs. O) Or Valley (C vs. C) Convergent Reverse Move Together Subduction Zone/ Trench / Volcanoe (C vs. O) Mountain (C vs. C)
  • 9.
  • 10.
    Boundary Fault Plate Creates Direction (o=ocean & c=continental) Divergent Normal Pull or Moving Seafloor Spreading Apart (O vs. O) Or Valley (C vs. C) Convergent Reverse Move Together Subduction Zone/ Trench / Volcanoe (C vs. O) Mountain (C vs. C)
  • 11.
    Boundary Fault Plate Creates Direction (o=ocean & c=continental) Divergent Normal Pull or Moving Seafloor Spreading Apart (O vs. O) Or Valley (C vs. C) Convergent Reverse Move Together Subduction Zone/ Trench / Volcanoe (C vs. O) Mountain (C vs. C) Transform Strike-Slip Slide Alongside Earthquake and One Another Faultline
  • 14.
     Scientist believeconvection currents move the plates by the hot material in the mantle rising and as it cools it carries the plates along with it until it sinks and starts the process all over again.
  • 18.
    Previously scientists knew plates were moving, but new methods use lasers and satellites to measure precise movements.