Earthquake Epicenter Overview

Aug 14, 2025

Overview

This lesson explains what an earthquake epicenter is, how it is determined, and why it is important for understanding and responding to earthquakes.

Earthquakes and Their Causes

  • Earthquakes occur due to sudden movement along faults in the Earth's crust.
  • The point where the rocks break underground is called the focus or hypocenter.
  • The energy released during an earthquake travels as seismic waves.

Epicenter: Definition and Importance

  • The epicenter is the point on the Earth's surface directly above the earthquake's focus.
  • The epicenter is usually the location where the earthquake's effects are most strongly felt.
  • Knowing the epicenter helps in assessing the impact and directing emergency response.

Seismic Waves and Their Types

  • Seismic waves are vibrations that travel through the Earth during an earthquake.
  • Body waves travel through the Earth's interior and include primary (P) and secondary (S) waves.
  • Surface waves travel along the Earth's surface and cause the most damage.

Locating the Epicenter

  • Seismologists use data from multiple seismograph stations to locate an earthquake's epicenter.
  • The difference in arrival time between P-waves and S-waves at each station is used to calculate the distance to the epicenter.
  • By drawing circles with each station at the center and matching the calculated distances, the epicenter is found where the circles intersect (triangulation).

Key Terms & Definitions

  • Earthquake — A sudden shaking of the ground caused by movement of tectonic plates.
  • Focus/Hypocenter — The point underground where the earthquake starts.
  • Epicenter — The point on Earth's surface directly above the focus.
  • Seismic Waves — Vibrations released during an earthquake, including P-waves, S-waves, and surface waves.
  • P-waves (Primary waves) — Fastest seismic waves that arrive first and move through solids and liquids.
  • S-waves (Secondary waves) — Slower than P-waves and only move through solids.
  • Triangulation — A method for finding the epicenter using distances from three or more seismograph stations.

Action Items / Next Steps

  • Review how to interpret seismograph data and practice locating epicenters using sample problems.
  • Read the next lesson about volcanoes for further understanding of earth processes.