What is an earthquake?

An earthquake is the shaking caused when energy is released inside the Earth. Many begin when rocks held in place by friction suddenly slip along a fault. The released energy travels outward as seismic waves.

The hypocenter, or focus, is where the rupture begins underground. The epicenter is the point directly above it on the surface. A large rupture can extend far beyond that starting point, so an epicenter alone does not describe the whole earthquake.

Start with a question, follow a map, or try a comparison.

See the connections

Most earthquakes occur near tectonic plate boundaries. Those boundaries help explain the pattern around the Ring of Fire and much of California’s earthquake activity.

Follow the Pacific to Japan to learn about subduction, major earthquakes, and the shindo scale used in Japanese shaking reports.

To understand an individual event, begin with magnitude and intensity. To understand what follows a larger earthquake, read about aftershocks.

The guides link to their scientific sources. For an introduction from the data provider, read USGS: What is an earthquake and what causes them to happen?. For questions about the Android app, visit App help.