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Chapter 2: Plate Tectonics
Layers of the Earth
Layers of the Earth




                      Denser
                      Basaltic
                      Rocks
Layers of the Earth




                      Denser     Less dense
                      Basaltic   Granitic
                      Rocks      Rocks
Alfred Wegener’s
Continental Drift Theory
Evidences
Evidences
Evidences
Evidences


• Geological Evidence: Edges of continents fit like a
  jig-saw
Evidences


• Geological Evidence: Edges of continents fit like a
  jig-saw

• Biological Evidence: Fossils & Imprints of plants
Evidences


• Geological Evidence: Edges of continents fit like a
  jig-saw

• Biological Evidence: Fossils & Imprints of plants
• Climate Based Evidence: Glaciation
So does our earth still
move today?
So does our earth still
move today?
 How will earth look like
in the future?
What’s wrong with Wegener’s theory
       of Continental Drift?
What’s wrong with Wegener’s theory
       of Continental Drift?
What’s wrong with Wegener’s theory
       of Continental Drift?


 • Continents do NOT move.
What’s wrong with Wegener’s theory
       of Continental Drift?


 • Continents do NOT move.
 • It is the tectonic (crustal) plates that consist of both
   oceanic and continental crusts that moves.
Tectonic Plates vs.
 Plate Tectonics
Tectonic Plates vs.
          Plate Tectonics
• Tectonic (Crustal) Plates:
Tectonic Plates vs.
          Plate Tectonics
• Tectonic (Crustal) Plates:
   • Consist of both continental and oceanic crusts.
Tectonic Plates vs.
          Plate Tectonics
• Tectonic (Crustal) Plates:
   • Consist of both continental and oceanic crusts.
• Plate Tectonics:
Tectonic Plates vs.
          Plate Tectonics
• Tectonic (Crustal) Plates:
   • Consist of both continental and oceanic crusts.
• Plate Tectonics:
   • How plates move
Tectonic Plates vs.
          Plate Tectonics
• Tectonic (Crustal) Plates:
   • Consist of both continental and oceanic crusts.
• Plate Tectonics:
   • How plates move
   • Why they move
Tectonic Plates vs.
          Plate Tectonics
• Tectonic (Crustal) Plates:
   • Consist of both continental and oceanic crusts.
• Plate Tectonics:
   • How plates move
   • Why they move
   • How the movement changes the physical
     landscape
Memorise!
Plate Boundaries & Movements
Plate Boundaries & Movements
• 1. Constructive plate boundaries
Plate Boundaries & Movements
• 1. Constructive plate boundaries
   • Divergent (Move apart)
Plate Boundaries & Movements
• 1. Constructive plate boundaries
   • Divergent (Move apart)
   • Tensional force
Plate Boundaries & Movements
• 1. Constructive plate boundaries
   • Divergent (Move apart)
   • Tensional force
• 2. Destructive plate boundaries
Plate Boundaries & Movements
• 1. Constructive plate boundaries
   • Divergent (Move apart)
   • Tensional force
• 2. Destructive plate boundaries
   • Convergent (Move towards)
Plate Boundaries & Movements
• 1. Constructive plate boundaries
   • Divergent (Move apart)
   • Tensional force
• 2. Destructive plate boundaries
   • Convergent (Move towards)
   • Compressional force
Plate Boundaries & Movements
• 1. Constructive plate boundaries
   • Divergent (Move apart)
   • Tensional force
• 2. Destructive plate boundaries
   • Convergent (Move towards)
   • Compressional force
• 3. Conservative plate boundaries
Plate Boundaries & Movements
• 1. Constructive plate boundaries
   • Divergent (Move apart)
   • Tensional force
• 2. Destructive plate boundaries
   • Convergent (Move towards)
   • Compressional force
• 3. Conservative plate boundaries
   • Transform (Slide past)
Plate Boundaries & Movements
• 1. Constructive plate boundaries
   • Divergent (Move apart)
   • Tensional force
• 2. Destructive plate boundaries
   • Convergent (Move towards)
   • Compressional force
• 3. Conservative plate boundaries
   • Transform (Slide past)
   • Frictional force
Physical features in the World
Physical features in the World




        Mid-Atlantic Ridge
Physical features in the World




                    East
                  African
                 Rift Valley
        Mid-Atlantic Ridge
Physical features in the World




                      East
                    African
                   Rift Valley
  Andes
          Mid-Atlantic Ridge
Physical features in the World




Rockies
                       East
                     African
                    Rift Valley
   Andes
           Mid-Atlantic Ridge
Physical features in the World




                           Himalayas

Rockies
                       East
                     African
                    Rift Valley
   Andes
           Mid-Atlantic Ridge
Physical features in the World



St. Andrea’s
    Fault
                                   Himalayas

      Rockies
                               East
                             African
                            Rift Valley
           Andes
                   Mid-Atlantic Ridge
1. Constructive Plate
     Boundaries

                       Sea Floor Spreading




 Plates diverges & pulls apart
1. Constructive Plate
     Boundaries
1. Constructive Plate
     Boundaries
1. Constructive Plate
                Boundaries
• Case #1: Oceanic-Oceanic
 Crusts
1. Constructive Plate
                 Boundaries
• Case #1: Oceanic-Oceanic
  Crusts

• Ridges.
1. Constructive Plate
                  Boundaries
• Case #1: Oceanic-Oceanic
  Crusts

• Ridges.
  • Eg. Mid-Atlantic Ridge
1. Constructive Plate
                  Boundaries
• Case #1: Oceanic-Oceanic
  Crusts

• Ridges.
  • Eg. Mid-Atlantic Ridge
• Sometimes lava fountains are
  found in the middle of the
  ridges.
1. Constructive Plate
     Boundaries
1. Constructive Plate
                Boundaries
• Case #2: Continental-
 Continental Crusts
1. Constructive Plate
                Boundaries
• Case #2: Continental-
 Continental Crusts
1. Constructive Plate
                      Boundaries
• Case #2: Continental-
  Continental Crusts

• Rift Valleys
1. Constructive Plate
                      Boundaries
• Case #2: Continental-
  Continental Crusts

• Rift Valleys
  • Eg. East African Rift Valley
1. Constructive Plate
                      Boundaries
• Case #2: Continental-
  Continental Crusts

• Rift Valleys
  • Eg. East African Rift Valley
• Magma rises and squeezes through
  the widening cracks, sometimes to
  erupt and form volcanoes.
1. Constructive Plate
                      Boundaries
• Case #2: Continental-
  Continental Crusts

• Rift Valleys
  • Eg. East African Rift Valley
• Magma rises and squeezes through
  the widening cracks, sometimes to
  erupt and form volcanoes.

• The rising magma puts more
  pressure on the crust to produce
  additional fractures and, ultimately,
  the rift zone.
2. Destructive Plate
         Boundaries




Plates converges & collide
2. Destructive Plate
    Boundaries
2. Destructive Plate
    Boundaries
2. Destructive Plate
    Boundaries
2. Destructive Plate
          Boundaries

• Case #1: Oceanic-Continental Crusts
2. Destructive Plate
           Boundaries

• Case #1: Oceanic-Continental Crusts
• Mountains
2. Destructive Plate
           Boundaries

• Case #1: Oceanic-Continental Crusts
• Mountains
  • Eg. Andes
2. Destructive Plate
           Boundaries

• Case #1: Oceanic-Continental Crusts
• Mountains
  • Eg. Andes
• Trench
2. Destructive Plate
           Boundaries

• Case #1: Oceanic-Continental Crusts
• Mountains
  • Eg. Andes
• Trench
  • Eg. Peru-Chile Trench
2. Destructive Plate
           Boundaries

• Case #1: Oceanic-Continental Crusts
• Mountains
  • Eg. Andes
• Trench
  • Eg. Peru-Chile Trench
• Earthquakes
2. Destructive Plate
           Boundaries

• Case #1: Oceanic-Continental Crusts
• Mountains
  • Eg. Andes
• Trench
  • Eg. Peru-Chile Trench
• Earthquakes
2. Destructive Plate
           Boundaries

• Case #1: Oceanic-Continental Crusts
• Mountains
  • Eg. Andes
• Trench
  • Eg. Peru-Chile Trench
• Earthquakes
2. Destructive Plate
    Boundaries
2. Destructive Plate
    Boundaries
2. Destructive Plate
    Boundaries
2. Destructive Plate
          Boundaries
• Case #2: Oceanic-Oceanic Crusts
2. Destructive Plate
           Boundaries
• Case #2: Oceanic-Oceanic Crusts
• Oceanic trenches
2. Destructive Plate
           Boundaries
• Case #2: Oceanic-Oceanic Crusts
• Oceanic trenches
  • Eg. Marianas Trench
2. Destructive Plate
            Boundaries
• Case #2: Oceanic-Oceanic Crusts
• Oceanic trenches
   • Eg. Marianas Trench
• Volcanic islands  Island Arcs
2. Destructive Plate
            Boundaries
• Case #2: Oceanic-Oceanic Crusts
• Oceanic trenches
   • Eg. Marianas Trench
• Volcanic islands  Island Arcs
   • Hawaiian Islands
2. Destructive Plate
            Boundaries
• Case #2: Oceanic-Oceanic Crusts
• Oceanic trenches
   • Eg. Marianas Trench
• Volcanic islands  Island Arcs
   • Hawaiian Islands
• Earthquakes
2. Destructive Plate
    Boundaries
2. Destructive Plate
    Boundaries
2. Destructive Plate
    Boundaries
2. Destructive Plate
    Boundaries
2. Destructive Plate
    Boundaries
2. Destructive Plate
           Boundaries
• Case #3: Continental-Continental Crusts
2. Destructive Plate
           Boundaries
• Case #3: Continental-Continental Crusts
• Fold Mountains
2. Destructive Plate
           Boundaries
• Case #3: Continental-Continental Crusts
• Fold Mountains
  • Eg. Himalayas
3. Conservative Plate
       Boundaries




Plates slide past each other
3. Conservative Plate
     Boundaries
3. Conservative Plate
     Boundaries
3. Conservative Plate
     Boundaries
3. Conservative Plate
            Boundaries
• Fault lines
3. Conservative Plate
            Boundaries
• Fault lines
  • Eg. St. Andreas Fault, San Francisco
3. Conservative Plate
            Boundaries
• Fault lines
  • Eg. St. Andreas Fault, San Francisco
• Earthquakes
Dynamic movements of
   tectonic plates

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