As a seismologist with extensive experience in earthquake studies, I can explain the process of locating the epicenter of an earthquake. The epicenter is the point on the Earth's surface directly above where the earthquake rupture begins. Here's how you can determine it: 1. Seismograph Data: Seismographs around the world record the waves from an earthquake. The first waves to arrive are the primary (P) waves, which are faster and can travel through both solid and liquid rock. Following the P waves are the secondary (S) waves, which are slower and can only travel through solid rock. 2. Wave Arrival Times: By measuring the time difference between the arrival of P waves and S waves at various seismograph stations, you can estimate the distance to the epicenter from each station. 3. Travel Time Curves: Seismologists use travel time curves, which are graphs that show how long it takes for different types of seismic waves to travel various distances. These curves are derived from the known speeds of P and S waves and the Earth's layered structure. 4. Marking Points: On a map or a chart, you would mark the point for the calculated time difference (in this case, 24 seconds) for each seismograph station. 5. Triangulation: By plotting these points and using triangulation or other geometric methods, you can find the intersection of the circles or areas that represent the possible locations of the epicenter. The point where the circles intersect is the estimated epicenter. 6. Refinement: The process may be refined by using data from more seismograph stations, which can provide a more precise location. 7. Depth Determination: The depth of the earthquake can also be estimated using the time it takes for the waves to travel to the surface, but this is a separate process from locating the epicenter. 8. Modern Technology: Today, computers and advanced algorithms quickly process seismograph data from multiple stations around the globe to pinpoint the epicenter and depth with high accuracy. read more >>

This number will be used to tell you how far your seismograph is from the epicenter of the earthquake. Measure the distance between the first P wave and the first S wave. In this case, the first P and S waves are 24 seconds apart. Find the point for 24 seconds on the left side of the chart below and mark that point.read more >>