Answer:
True
Step-by-step explanation:
Earth's surface is made up of several large tectonic plates that move and interact with each other. When two plates collide or grind against each other, the rock layers in between can become deformed and subjected to stress. This stress builds up over time and, when it reaches a certain threshold, can cause the rock to suddenly break, releasing the energy stored in the form of seismic waves that result in an earthquake. This is called the elastic rebound theory and is the most widely accepted explanation for how earthquakes occur.