An earthquake is the shaking of the surface of the Earth resulting from a sudden release of energy in the Earth's lithosphere that creates seismic waves.
Earthquakes are caused by the movement of tectonic plates along faults. The release of accumulated stress along these faults results in seismic waves.
There are three main types of seismic waves: P-waves (primary waves), S-waves (secondary waves), and surface waves. P-waves are the fastest and can travel through solids, liquids, and gases. S-waves are slower and can only travel through solids. Surface waves are the slowest and cause the most damage.
Earthquakes are measured using instruments called seismographs. The magnitude of an earthquake is determined using the Richter scale, while the intensity of shaking is measured using the Modified Mercalli scale.
Earthquakes can cause ground shaking, tsunamis, landslides, and structural damage to buildings and infrastructure. They can also lead to loss of life and economic devastation.
It is important to be prepared for earthquakes by having an emergency kit, making a family communication plan, securing heavy items that could fall during shaking, and knowing evacuation routes.