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The Earth is layered
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Major Plates of the World
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Mantle Convection
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Historical Movement (Past 250mya)
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Pangaea
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Evidence of Past Plate Movement
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Ice Sheets
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Magnetic Reversals
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Magnetic Reversals
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Magnetic Reversals
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Magnetic Reversals
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Location of Earthquakes
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Convergent Boundaries
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Transform Boundary
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Divergent Boundary
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Plate Boundary Review
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Plate Boundaries Plate boundaries are seismically active: Earthquakes
Volcanoes Mountains
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Causes of Earthquakes Eruption of a volcano Collapse of a cavern
Impact of a meteor Stress that builds up between two lithospheric plates.
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EQ Terminology
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EQ’s release energy in the form of waves
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P and S waves
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EQ waves are recorded using a Seismograph
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Earthquake P-Wave and S-Wave Travel Time – For EQ Location
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Locating EQ’s
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Can you find the Epicenter?
Seismic Stations P-wave arrival times: Calculate: 1. distance from seismic station and; 2. epicenter for each case study. Case Study I: Denver 2:40 New Orleans 2:00 Scranton 2:50 Case Study II: Cancun 4:00 Boston 3:20 Juneau 4:50
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