What happens when jagged edges of rock plates of rock grind past each other
When the jagged edges of rock plates grind past each other, it creates friction at the contact point between the plates. This friction causes a buildup of stress and pressure, which eventually exceeds the strength of the rocks. The accumulated stress is released in the form of an earthquake.
During an earthquake, the rocks along the fault line slip and slide past each other, releasing the stored energy. This sudden release of energy causes the ground to shake, resulting in vibrations that can be felt and measured at the Earth's surface.
Depending on the magnitude and duration of the earthquake, the resulting shaking can have various effects. It can cause damage to buildings, infrastructure, and the natural environment. In extreme cases, it can lead to landslides, tsunamis, and other secondary hazards.
Overall, the interaction of jagged rock edges grinding past each other leads to the generation of seismic energy, resulting in earthquakes with varying degrees of impact.