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REVIEW: Seismic Waves give us information on : 1) Plate boundary locations 2) Types of plate boundaries 3) Internal Structure of the Earth 4) How Plates can move – Brittle Lithosphere “floating” on hot plastic Asthenosphere. We can use gravity to examine the Earth’s Interior. ISOSTACY.
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REVIEW: Seismic Waves give us information on: 1) Plate boundary locations 2) Types of plate boundaries 3) Internal Structure of the Earth 4) How Plates can move – Brittle Lithosphere “floating” on hot plastic Asthenosphere.
Topography of the Sea-floor Development of the fathometer (echo –sounding) for World War II
Harry Hess and Sea-floor Spreading Hess had no real evidence that this was occurring. He called is own theory “Geopoetry” Evidence would be provided by new data from The Earth’s Magnetic Field
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The Earth’s Magnetic Field has reversed itself many times during the geologic past.
Polar Wandering? Or……… Continental Drift?
So, Earth’s Magnetism Explains: • Apparent polar wandering • Magnetic reversals recorded in rocks • Seafloor spreading
Final Proof of Sea-floor spreading came from dating the Ocean floor