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Alfred Wegener and Pangaea

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Alfred Wegener and Pangaea Pangaea is the name given to the single giant continent in a proposal by Wegener (1912). The theory of continental drift states that the ... – PowerPoint PPT presentation

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Title: Alfred Wegener and Pangaea


1
Alfred Wegener and Pangaea
  • Pangaea is the name given to the single giant
    continent in a proposal by Wegener (1912).
  • The theory of continental drift states that the
    continents were once a single landmass that
    drifted apart and are still doing so.

2
Evidence for Continental Drift
  • Wegener tried to support his theory with
    evidence
  • Maps - continents apparently fit together like a
    jigsaw-puzzle
  • Plant and animal fossils - coal in Antarctica

3
Evidence for Continental Drift
  • Why was his theory not accepted?
  • No explanation for how drift occurs
  • He was a meteorologist, not a geologist!
  • Plate tectonics theory - explanation for how
    continents move, making Wegeners theory widely
    accepted.

4
New Technology and Seafloor Knowledge
  • Sonar 1925 first seafloor map of ocean ridges
  • New features discovered
  • Mid-ocean ridges mountain ridges on ocean floor
  • Rift valleys valley in center of MOR
  • Trenches
  • Scientists observed patterns in features

5
Ridges and Trenches
6
Seafloor Spreading
  • Seafloor constantly being created and destroyed
  • New crust at rift valley
  • Crust destroyed at trenches

7
Evidence for Seafloor Spreading
  • Thin sediment in ridges
  • Age of rock at ridges much younger than
    continents
  • Patterns of magnetic polarity reversal

8
Seafloor Age
9
Types of Movement
  • Divergent plates moving apart (rift valleys in
    MOR)
  • Convergent plates coming together
  • Transform plates slide past each other

10
Island Arcs
  • Convergent ocean plates
  • Subduction of denser plate

11
Subduction Zones
  • Ocean plate into continent
  • Trench, mountains, volcanoes formed

12
Convergent Continents
  • Mountains form

13
Hot Spots
  • Magma chambers in mantle push through surface of
    crust
  • Crust moves over mantle forming island chain

14
Plate Movement
  • Convection is the primary force driving seafloor
    spreading andcontinental drift.
  • Convection currents form as hot material rises
    and cold material sinks. This occurs in the
    mantle.
  • This creates a current that moves the plates away
    from each other at the divergent boundaries,
    toward each other at the convergent boundaries,
    and past each other at the transform boundaries.
  • A second driving force comes from seafloor
    spreading.
  • As new seafloor forms, the platestend to slide
    away fromthe elevated mid-ocean ridges.

The Unifying Theory Plate Tectonics
Chapter 11 Pages 11-26 11-27
15
Plate Movement (continued)
  • Predicted changes over the next 50 million years
  • The Baja Peninsula will have moved past and apart
    from the North American Plate.
  • Southern California will pass San Francisco as it
    moves to the northwest.
  • A new sea will form in eastern Africa.
  • Australia will move toward Eurasia/the Equator.
  • The Mediterranean Sea will close as Africa pushes
    towards Europe.
  • The Atlantic and Indian Oceans will continue to
    grow while the Pacific will become smaller.

The Unifying Theory Plate Tectonics
Chapter 11 Pages 11-28 11-29
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