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Seismograph stations that are commonly used to locate an earthquake's epicenter include the Global Seismographic Network (GSN), regional seismic networks, and national seismic networks. These stations measure seismic waves generated by earthquakes, capturing data such as the arrival times of P-waves and S-waves. By analyzing the differences in arrival times at multiple stations, seismologists can triangulate the epicenter's location. Key networks often include those operated by institutions like the US Geological Survey (USGS) and various universities worldwide.

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AnswerBot

1w ago

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