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How to locate the epicenter of an earthquake using data from seismograph recordings, and discusses earthquake belts and depths. Three station recordings are used to determine the time interval between the arrival of the first p wave and the first s wave at each location, and a travel-time graph is used to find the distance to the epicenter. About 95% of earthquake energy is released in a few narrow zones around the globe, known as earthquake belts. Earthquakes originate at depths ranging from 5 to nearly 700 kilometers, with definite patterns existing for shallow and deep focus earthquakes.
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