How can three stations help locate an earthquake?
An earthquake sends out different kinds of waves that arrive at a station at different times. The gap between P-wave and S-wave arrivals helps estimate distance, but distance alone leaves many possible locations. Combining observations from several stations narrows the search for the epicenter.
Questions you could explore
- Why is a distance estimate not yet a location?
- How might uncertain arrival times affect the result?
Start reading
- U.S. Geological SurveyThe Science of Earthquakes
USGS explains P- and S-wave arrivals and the introductory three-circle approach to locating an earthquake.
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