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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.
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We can use gravity to examine the Earth’s Interior
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ISOSTACY
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Topography of the Sea-floor
Development of the fathometer (echo –sounding) for World War II
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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 has a magnetic field – a Geodynamo
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A B
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The Earth’s Magnetic Field has
reversed itself many times during the geologic past.
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Polar Wandering? Or……… Continental Drift?
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So, Earth’s Magnetism Explains:
Apparent polar wandering Magnetic reversals recorded in rocks Seafloor spreading
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Final Proof of Sea-floor spreading came from dating the Ocean floor
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MAP OF PLATE BOUNDARIES
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1) Divergent Boundaries
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