Plate Tectonics Theory & More Flashcards
Evidence For Change:
- Deformed strata (layers of rock)
- Seismic activity
- Subsidence or sinking of the crust (Gulf of Mexico)
- Uplift of the crust (mountains)
Discoveries Leading Up to the Theory of Plate Tectonics:
- Continental Drift
- Sea floor spreading
- Paleomagnetic Data and Polar Wandering
Continental Drift Theory:
- 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
Supportive Evidence for Continental Drift:
- Fit of coast lines
- Matching fossil evidence
- Matching paleoclimates
- Matching rock and mineral type and structural similarities
Strengths of Continental Drift:
- 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…
Weakness of Continental Drift:
Wegner could not explain how or why continents moved…
Sea Floor Spreading:
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)
Magnetic Reversals on Seafloor:
- 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
Polar Wandering Data:
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)
Unified Theory of Plate Tectonics:
- 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
Main Points of the Unified Theory of Plate Tectonics:
- 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
Three Types Of Plate Motions:
Convergent
Divergent
Transform
Convergent:
Move together
Divergent:
Seperate
Trasnform:
Slide past