Plate Tectonics Theory & More Flashcards

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1
Q

Evidence For Change:

A
  • Deformed strata (layers of rock)
  • Seismic activity
  • Subsidence or sinking of the crust (Gulf of Mexico)
  • Uplift of the crust (mountains)
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2
Q

Discoveries Leading Up to the Theory of Plate Tectonics:

A
  • Continental Drift
  • Sea floor spreading
  • Paleomagnetic Data and Polar Wandering
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3
Q

Continental Drift Theory:

A
  • Proposed by German scientist Alfred Wegner in 1915
  • States that all continents were originally one land mass called Pangea
  • Was a radical theory at the time
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4
Q

Supportive Evidence for Continental Drift:

A
  • Fit of coast lines
  • Matching fossil evidence
  • Matching paleoclimates
  • Matching rock and mineral type and structural similarities
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5
Q

Strengths of Continental Drift:

A
  • Continents do really seem to fit together like a giant puzzle
  • Matching evidence from either side of Atlantic Ocean in Africa and South America of fossil remains, rocks, minerals and paleoclimates…
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6
Q

Weakness of Continental Drift:

A

Wegner could not explain how or why continents moved…

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7
Q

Sea Floor Spreading:

A

Harry Hess from Princeton University proposed that sea floor is spreading apart. This spreading was thought to be caused by convection currents in the mantle (1962)

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8
Q

Magnetic Reversals on Seafloor:

A
  • Pattern of magnetic polar reversals found on sea floor in 1963
  • Connects to idea of sea floor spreading by Harry Hess
  • Reversals coincide with age of rock on sea floor
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9
Q

Polar Wandering Data:

A

Mid 50’s scientists produce paleomagnetic data from several continents showing the apparent polar wandering consistent with Wegner’s theory (magnetic north poles changed position over time)

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10
Q

Unified Theory of Plate Tectonics:

A
  • All previous ideas can be explained by this theory

- Term “Plates” was coined in the 1960’s by J. Tuzo Wilson of the University of Tornto

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11
Q

Main Points of the Unified Theory of Plate Tectonics:

A
  • Surface of the Earth is composed of major rigid moving sections called “plates”
  • These plates float on the mantle
  • The plates consist of continental and oceanic rock
  • The boundary where plates meet is the area of the most crustal activity
  • Differences in the density of materials in the asthenosphere move the plates
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12
Q

Three Types Of Plate Motions:

A

Convergent
Divergent
Transform

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13
Q

Convergent:

A

Move together

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14
Q

Divergent:

A

Seperate

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15
Q

Trasnform:

A

Slide past

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