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 sudden release of energy within the Earth's crust or upper mantle. This release of energy causes seismic waves that shake the Earth's surface.
Earthquakes occur along faults, which are fractures in the Earth's crust where movement has occurred. There are three main types of faults:
When an earthquake occurs, it generates seismic waves that travel through the Earth and along its surface. There are two main types of seismic waves:
Earthquakes are measured using instruments called seismometers. The most common scale for measuring the size of an earthquake is the Richter scale, which measures the amplitude of seismic waves. Another scale, the moment magnitude scale, takes into account the amount of slip on the fault, the area of the fault surface that slipped, and the rigidity of the rocks that slipped.
Earthquakes can have devastating effects, including ground shaking, surface rupture, landslides, tsunamis, and human impacts such as building and infrastructure damage, injuries, and loss of life.
It's important to be prepared for earthquakes. This includes creating an emergency plan, securing heavy items that could fall and cause injury, and knowing how to "Drop, Cover, and Hold On" during an earthquake.