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Describe how earthquakes occur. Compare and contrast the different types of seismic waves. What are seismic waves? 03/02/2015
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Can earthquakes occur in Chicago?
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Forces within the Earth Tectonic plates are not smooth along their boundaries. They do not slide easily past one another. Rocks in the plates resist movement, resulting in stress buildup.
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Earthquake Sudden slip on a fault Results in ground shaking and radiating seismic energy Causes – Volcanic activity – Tectonic plate movement
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Faults A fracture in the Earth Normal, Reverse, Strike-slip – Strike-slip faults are most destructive Normal ReverseStrike-slip
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Faults
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Earthquake Sudden slip on a fault Results in ground shaking and radiating seismic energy Causes – Volcanic activity – Sudden stress changes in the Earth
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Diagram of an Earthquake Hypocenter/Focus: point underground where the waves originate Epicenter: point on Earth’s surface directly above the focus. Seismic Waves: energy radiating around from the focus in wave form.
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Seismic Energy 3 types of waves – Primary, Secondary, Surface
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1. Primary wave (P-wave)
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Causes rocks to be squeezed and pushed parallel to the direction of the wave. Fastest wave.
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2. Secondary waves (S-waves)
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2. Secondary Wave (S-wave) Causes rocks to move perpendicular to the wave direction Slower than P-waves
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P-waves and S-waves are both BODY waves because they pass through Earth’s interior.
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3. Surface Wave Travel only along Earth’s surface Cause the ground to move sideways and up and down Most destructive
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3. Surface Wave
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Seismic Energy
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