0 reply
0 recast
0 reaction
Earthquakes are sudden and powerful natural phenomena caused by the movement of tectonic plates beneath the Earth's surface. When stress builds up along faults, the release of energy generates seismic waves, resulting in ground shaking. The magnitude of an earthquake is measured using the Richter scale, which quantifies the energy released. However, the intensity experienced at a location can vary greatly due to local geological conditions. Earthquakes can trigger secondary hazards like tsunamis, landslides, and liquefaction, amplifying their destructive potential. Countries located along tectonic plate boundaries, such as Japan and California, are particularly vulnerable. Despite advances in seismology, predicting the exact time and place of an earthquake remains a significant challenge. Preparedness, including building codes and emergency response plans, is crucial in minimizing casualties and damage. Historical earthquakes, like the 1906 San Francisco quake 0 reply
0 recast
0 reaction