Continental Drift

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Continental Drift

• Earths crust is constantly moving
• horizontal
• vertical
• Crust is drifting on top of the liquid mantle
• Continental and Oceanic
• Shape and location of the continents and oceans
  have changed over millions of years (Constructive
  Destructive Forces)

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Alfred Wegener

• He hypothesized about 300 MYA the Earth had only
  one giant continent called Pangaea (meaning all
  lands)
• Published The Origin of Continents and Oceans in
  1915
• Evidence supporting the theory
• Landforms
• Fossil records
• Rock sequences
• Climates and changing polar regions

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Alexander Du Toit

• Proposed that 200 MYA Pangaea broke up into two
  supercontinents
• Gondwanaland
• Near the South Pole
• S.A., Africa, Antarctica, Australia, India
• Laurasia
• Near the Equator
• N. A., Eurasia

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Landforms

• Matching coastal lines fit together like a jigsaw
  puzzle
• South America Africa
• Similar mountain ranges
• Argentina and south Africa

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Fossil Records

• Similar plant fossils found on several different
  continents
• Separation by oceans suggests that the continents
  were once connected
• Glossopteris fern (southern continents)
• Cynognathus land reptile (S.A. Africa)
• Lystrosaurus land reptile (Africa, Antarctica,
  India)
• Mesosaurus freshwater reptile (S.A. Africa)

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Rock Structures

• Similarities in S.A., Africa, India, Antarctica,
  and Australia
• Paleomagnetism
• Study of the magnetism of ancient rocks and
  sediments

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Climate

• Continental ice sheets and glacial striations in
  South Africa
• Fossils of tropical plants found in Spitsbergen
  (small island north of Norway)
• Suggests movement from the equator and the poles

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Theory Rejected

• Wegener could not explain the forces that push or
  pull the continents
• Geologists rejected his theory of continental
  drift
• Lacked information on formation of mountains and
  continents
• Then new evidence was discovered