Seismologists use triangulation to locate earthquake epicenters. They measure the time difference between when P-waves and S-waves from an earthquake arrive at multiple seismic stations. These time differences are used to calculate the distance from each station to the epicenter. Circles are drawn around each station representing these distances, and the point where all the circles intersect indicates the epicenter location. The continental drift theory proposes that the continents were once joined together before drifting apart. Evidence for this includes matching coastline shapes, matching fossil distributions, and matching rock formations between continents now separated by oceans.