The San Andreas is a right-lateral strike-slip fault network marking the boundary between the Pacific and North American plates across much of California. The geological fault is not visibly exposed as a continuous cliff or scar along its entire length, and its branches vary in structure and accessibility.
NASA's satellite and radar-topography presentation of the Carrizo Plain explicitly identifies the approximately 1,200-kilometre San Andreas as the longest fault in California. USGS describes the San Andreas Fault System as a roughly 1,300-kilometre transform boundary. The approximately 350-kilometre rupture in 1857 was an event-specific rupture, not a measure of the entire fault's length.