Where earthquakes happen, and why
Nearly every dot on this map sits on or near a plate boundary. Plates are locked together along their edges by friction. As they keep moving a few centimeters a year, the rock bends until it snaps, and that sudden slip is an earthquake. Turn the range to 30 days and the outline of the plates appears on its own.
The deepest quakes, down to about 700 km, happen inside slabs of ocean floor sinking into the mantle at convergent boundaries such as those under Tonga, Japan and South America. Shallow quakes dominate along mid-ocean ridges and transform faults like the San Andreas.
How to use the map
Circle size and color show magnitude. A dark outline marks a quake in the last hour. Click a circle or a row in the list for the time, depth, the plate it struck on and a link to the official USGS event page. The 24-hour view includes small quakes that are mostly recorded in the United States, where seismic networks are densest.