A seismic event is any occurrence that generates seismic waves, typically associated with the movement of tectonic plates in the Earth’s crust. The most common form of seismic event is an earthquake, which can range in intensity from small tremors to large, destructive quakes.
These events are measured using instruments called seismometers, which detect the vibrations that travel through the Earth. Seismic events can also include volcanic activity, landslides, and even human-induced phenomena like mining or the use of explosives. Understanding seismic events is crucial for assessing risks and preparing for potential disasters, especially in regions that are prone to earthquakes.