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Published bySara Simmons Modified over 8 years ago
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Energy travels as seismic waves which are vibrations caused by earthquakes. All earthquakes start beneath the earth’s surface
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The focus of an earthquake is where rocks first begin to move. Seismic waves travel outward from earthquakes focus. The epicenter is the point right above the focus on the earth’s surface.
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If two earthquakes occur at the same time the one with a shallow focus will be more powerful Earthquakes produce three kind of waves: primary, secondary, and surface.
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Primary waves are the fastest waves and the first to reach a location P waves go through the earth at a speed of about 3 miles per second
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Secondary waves are the second wave to reach a location after the initial wave. Secondary waves can travel through rock but unlike primary waves they cant travel through liquid or gases.
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Surface waves are seismic waves that move along earth’s surface Surface waves are what make the ground roll up and down or shake from side to side.
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Seismograph is a instrument that constantly records ground movement Scientists use seismographs to measure thousands of earthquakes per year A seismogram is the recording produced.
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To locate a earthquakes epicenter scientists must have seismograms from at least three seismograph locations 1. Scientists find the difference between arrival times of primary and secondary waves at each 3 stations
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2. The time difference is used to determine the distance from epicenter from each station The greater the distance the farther away from the epicenter
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3. A circle is drawn around each station, where all the circles meet is the epicenter. The seismograph also helps scientists determine focus, depth, magnitude and strength
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