tectonic earthquake theory

Tectonic earthquake theory explains earthquakes as the result of movements in the Earth's crust due to tectonic plates. These plates are large sections of the Earth's surface that fit together like a jigsaw puzzle and constantly move, albeit very slowly. When they collide, slide past, or pull apart from each other, stress builds up. When this stress exceeds the strength of rocks, it releases energy in the form of seismic waves, causing an earthquake. Most earthquakes occur at plate boundaries, where these interactions are most intense. Understanding this theory helps us predict and mitigate the impact of earthquakes.