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Earthquakes Chapter 8 Earthquake - vibration of the earth caused by slippage along a fault. Characteristics 1. Focus- point in the Earth where a quake begins. 2. Epicenter- point on the surface above the focus. 3. Aftershock- small quake following a major quake. 4. Foreshock- small quake before a major quake. Cause Elastic Rebound Hypothesis - release of energy stored in deformed rocks.
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Elastic Rebound Hypothesis
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Slippage along a fault
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Measuring Quakes 1. Detection - Seismograph – instrument that records
earthquake waves. Wave Types 1. Surface Waves- waves on Earth’s outer layer. 2. Body Waves- waves in Earth’s interior. - P Waves- push-pull waves(1st) - S Waves- waves acting at right angles(2nd)
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Seismograph
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Seismogram
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Types of Waves
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2. Locating Epicenter - 3 or more seismograph stations measure the time it takes for waves to travel. 3. Magnitude - Richter Scale - measures strongest recorded waves - Moment Magnitude - measures energy released
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The Richter Scale Richter Magnitude TNT Energy Equivalent Example
Richter Magnitude TNT Energy Equivalent Example ounces pounds pounds pounds pounds ,000 pounds tons Small Atomic Bomb tons Average Tornado tons tons Massena, NY, 1994 tons ,550 ton Coalinga, CA, 1983 ,000 tons Hebgen Lake, MT 1959 ,000,000 tons ,270,00 tons San Francisco, CA 1906 ,550,000 tons Anchorage, AK, 1964 ,999,000 tons
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Locating Earthquakes
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Dangers of Earthquakes
1. Liquefaction - wet soil turns liquid - causes ground to collapse 2. Tsunami - vibrations create giant ocean waves 3. Landslide - vibrations cause soil to break loose
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TSUNAMI
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