A foreshock is an earthquake that occurs before a larger seismic event – the mainshock – and is related to it in both time and space. The designation of an earthquake as foreshock, mainshock or aftershock is only possible after the full sequence of events has happened. [1]

Foreshocks are earthquakes that precede larger earthquakes in the same location. An earthquake cannot be identified as a foreshock until after a larger earthquake in the same area occurs. Aftershocks are smaller earthquakes that occur in the same general area during the days to years following a larger event or "mainshock."

Observations show that the chance of an earthquake being followed by a larger one nearby and within a week is about 5%. That 5% foreshock probability varies with the activity level of an aftershock sequence.

28 June 2023 –Seismologists agree that foreshocks are the most widely identified signal of an upcoming mainshock earthquake. But do these foreshock sequences have distinctive characteristics that separate them from aftershock sequences, and could these characteristics be used to help forecast mainshocks?

Scientists for decades have sought to understand the physical processes that drive foreshocks, and why some earthquake sequences have them while others don’t. One leading theory proposes that foreshocks result from an acceleration of slipping movements along a fault.

The meaning of FORESHOCK is any of the usually minor tremors commonly preceding the principal shock of an earthquake.

2023年6月28日 · Seismologists agree that foreshocks are the most widely identified signal of an upcoming mainshock earthquake. But do these foreshock sequences have distinctive characteristics that separate...

Foreshocks are smaller seismic events that occur before a larger earthquake, known as the mainshock. They are important because they may indicate an increase in stress in the Earth's crust, suggesting that a significant earthquake could follow.

2004年1月24日 · A fast particle that escapes into the foreshock carries energy, and therefore it generally produces waves. Observationally, the Earth's foreshock is a rich “zoo” of different types of particles and the different waves they produce. Generally it is possible, and useful, to consider the shock and foreshock as separate aspects of the plasma.

A foreshock is a smaller earthquake that occurs in the same area as a larger earthquake, known as the mainshock, and often happens hours to days before it. These preliminary tremors can indicate an impending larger seismic event, although not every earthquake has foreshocks.