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Published byGabriella Ford Modified over 9 years ago
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Plate Tectonics
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Alfred Wegener Published The Origin of Continents and Oceans (1915) Father of “Continental Drift”
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Evidence for Plate Tectonics Jigsaw Fit of Continental Shelves
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Mesosaurus (Late Paleozoic to Early Mesozoic) Evidence for Plate Tectonics Fossil Correlation Across Seas
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Evidence for Plate Tectonics Rock Correlation Across Seas
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Evidence for Plate Tectonics Rock Correlation Across Seas
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Differences in Ancient Climates Evidence for Plate Tectonics Glacial Imprints in Rocks in Tropics
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WW2 – Sonar – mapping seafloor
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North Pole South Pole
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Magnetite (Fe 3 O 4 )
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Minerals retain their magnetic moment when they are cooled below the Curie Temperature
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Magnetic Reversals North South
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Magnetic Reversals Through Geologic Time
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Magnetic Polarity Time Scale established back to about 180 million yrs
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Earth’s Magnetic Flux Lines Intensity of Magnetism N S
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Magnetic Stripes on the Seafloor
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Age of seafloor determined – led to acceptance of Plate Tectonics
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15 Tectonic Plates
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Tectonic Motions
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Location of World’s Major Volcanoes
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Lithosphere –The rigid outer layer of the Earth, including the crust and part of the upper mantle Asthenosphere –The portion of the upper mantle below the lithosphere that is easily deformed
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Subduction The thrusting of oceanic plate into the mantle at a plate boundary
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Continent-Ocean Plate Orogeny
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Juan de Fuca Plate
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Mt. St. Helens, Before 1980
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Ocean-Ocean Plate Orogeny
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Many mountain belts are built by Ocean-Continent AND Continent- Continent collisions.
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Mountain Building (Orogenesis) Continent- Continent Collisions
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Continent-Continent Orogeny
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Mt. Makalu, Nepal
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Divergent plate boundaries
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Birth of an Ocean at a Divergent Margin
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Transform (or Strike-Slip) Faults
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San Andreas: A Transform Fault on Land
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Hot Spots
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Tectonic Motions
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Convection The transfer of heat by the movement of matter. Convection Cell
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Double-Layer Convection Depressurized Melting
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