Earthquakes are ground motions produced by a sudden release of energy in the Earth’s crust that can cause significant damage to buildings and infrastructure.
The primary source of energy for earthquakes is friction between two or more tectonic plates.
These plates can be located anywhere on land or at the bottom of the ocean, making them extremely difficult to predict, although experts may be able to identify areas that are likely to experience seismic activity.
During an earthquake, seismic waves travel through solid rock and may cause shaking, landslides, tsunamis, and even volcanic eruptions.
It is essential for individuals in high-risk areas to practice safety measures before an event occurs in order to reduce the potential for injury or death.
