A strike-slip fault is a type of fault where two blocks of the Earth's crust slide past each other horizontally. This movement is typically caused by shear stress, which occurs when tectonic plates push against each other. In these faults, the displacement is mainly lateral, which can lead to earthquakes and is crucial for understanding the behavior of seismic activity in regions where these faults are present.
congrats on reading the definition of strike-slip fault. now let's actually learn it.