Seismologists use triangulation to locate an earthquake's epicenter using data from at least three seismic stations. They determine the time difference between the arrival of P and S waves from each station. This time difference is used to calculate the distance from the station to the epicenter. Circles are drawn around each station marking this distance. Where the circles intersect is the epicenter location. Locating the epicenter helps determine which fault lines were active and increases understanding of hazards in the area.