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In seismology, trigonometry is used to analyze seismic waves and determine the location and depth of earthquakes. By measuring the time it takes for seismic waves to travel from the earthquake's epicenter to various seismic stations, trigonometric calculations help triangulate the epicenter's position. Additionally, trigonometric functions assist in modeling wave propagation and understanding the angles of wave incidence and reflection, which are crucial for interpreting seismic data.

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Q: How is trigonometry used in seismology?
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