Earthquakes are caused by the sudden release of energy within the Earth's crust, typically due to the movement of tectonic plates. These movements occur along fault lines where plates grind against, pull away from, or collide with each other. Stress builds up over time, and when it exceeds the strength of the rocks, it is released as seismic waves, causing the ground to shake. Natural causes like volcanic activity or human activities such as mining and reservoir-induced seismicity can also trigger earthquakes. The effects of earthquakes range from mild tremors to catastrophic destruction, depending on their magnitude and depth. Ground shaking can collapse buildings, infrastructure, and roads, leading to loss of life and economic damage. Secondary effects, such as tsunamis, landslides, and fires, often exacerbate the devastation. Additionally, earthquakes can displace populations and disrupt essential services like water, electricity, and communication, highlighting the need for preparedness and resilient infrastructure.