Transform faults are geological features where two tectonic plates slide past each other horizontally. This movement can cause earthquakes as the plates become stuck due to friction and then suddenly release. Transform faults are typically found on the ocean floor, but they can also occur on land. One of the most famous examples of a transform fault is the San Andreas Fault in California. This fault marks the boundary between the Pacific Plate and the North American Plate. The continuous movement along this fault contributes to the seismic activity in the region, making it a significant area of study for geologists.