Seismic waves are produced by various activities that compress, twist, or stretch rocks, such as earthquakes, meteorite impacts, and explosions. When the elastic limit of rocks is exceeded, they typically break, which can still propagate seismic energy, but this energy is capped by the rock's strength. The maximum magnitude of an earthquake is limited, as exceeding this threshold results in energy being spent on breaking rocks instead of generating seismic waves. The discussion also clarifies that the Richter scale is outdated, with the moment magnitude scale now being the standard for measuring seismic activity. Overall, understanding the mechanics of seismic wave production is crucial for comprehending earthquake dynamics.