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Continental Drift

Seafloor Spreading and • Predecessor to modern plate Magnetic Reversals • Shape and “fit” of the was the initial evidence Brad Hubeny – Snider-Pelligrini (1858) – Taylor (1908) – Wegener (1915)

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Wegener (1915): Continental Drift Terrestrial • Proposed that all of the continents were once part of a Geologic large supercontinent - Pangaea • Based on: Evidence • Similarities in shorelines • Terrestrial Geologic Evidence • Distinctive groups found in & South Only occur in rocks > America 145 Ma BP!

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Paleontological evidence

•No Seafloor Spreading mechanism to transport across • Wegner proposed a mechanism for drift – Less dense silicic rocks plowed through more •Divergence dense ocean floor of species – ’s rotation was driving force following break-up • Although supporting evidence existed, the theory was not widely accepted • Lack of testable hypothesis!!

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1 of the Development of Plate Tectonic Ocean Floor Theory • Doc Ewing does • Original evidence for continental drift was NOT find granite from continental rocks when he dredges the • Technological advances in the 1950’s and ocean bottom!! 1960’s allowed investigation of the sea floor • New data provided intriguing new information!

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Geology of the Ocean Floor • Bathymetry of the Bathymetry ocean basins Reveals – Sonar revealed Ridge in ocean basins Oceanic – Ridge system is continuous around the Rift System entire globe – Central rift valley within the ridge

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Earthquakes and Volcanoes Harry Hess’ “Essay in Geopoetry”

• Seafloor spreading proposed in 1960 paper • Considered new data on ocean floor • Proposed NEW more robust mechanisms • Great HYPOTHESIS, but needed to be 11 tested 12

2 Enter Paleomagnetics! Earth’s Geodynamo System! • Magnetic reversals Magnetic Field – Earth’s magnetic field polarity has reversed through time

• Normal polarity – Nmagnetic = Ngeographic

• Reversed polarity - Nmagnetic = Sgeographic • Iron-rich basalts of ocean crust preserve this record of the magnetic field!

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Geologic Magnetic Recorders 02_10.jpg Polarity Reversals

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Reversals & the Geologic Record 02_23.jpg Geomagnetic Time Scale

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3 Development of Plate Tectonic Oceanic Magnetometers Theory • Vine & Matthews (1963) tested Hess’s hypothesis using magnetism – Magnetic polarity reversals recorded in ocean floor basalt • Magma cools forming new crust • Polarity at time of cooling preserved • Old crust pushed aside • Became a Scientific Revolution!

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Seafloor Ages

Seafloor Magnetic Anomalies

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