Which fault is a northwest-trending, right-lateral, strike-slip fault over 750 feet long?

The San Andreas Fault is renowned for being a northwest-trending, right-lateral strike-slip fault that has a significant length, extending for over 750 miles. Its movement is characterized by the horizontal displacement of the earth's crust, where the two sides of the fault slide past each other without significant vertical movement. This means that if you were to stand on one side of the fault and face the other side, it would appear to shift sideways to your right, which is indicative of a right-lateral slip.

The San Andreas Fault plays a critical role in California's geology as it is a boundary between the Pacific and North American tectonic plates. The immense length and historical significance of this fault have made it a key focus for geologists studying tectonic activity, seismic hazards, and the geological history of the region. In terms of the other options provided, while there are other notable faults in California, they do not fit the specific criteria of being a right-lateral strike-slip fault that is both extensive and northwest-trending to the same degree as the San Andreas Fault.