1. To find the epicenter, we need data from at least three seismic stations. By measuring the difference in arrival times between P-waves and S-waves at each station, we can determine their distances to the epicenter. Then, by drawing circles with those distances as radii around each station, the epicenter is found where the three circles intersect.2. If only two stations provide data, you can draw only two circles, which will intersect at two possible points, not one. Therefore, you won’t know exactly which point is the real epicenter unless you have a third station to confirm.Seismologists need data from at least three seismic stations to accurately determine the location of an earthquake’s epicenter, using triangulation. More stations lead to greater accuracy in identifying the precise location.