Mud pots and hot springs along the San Andreas Fault in California reveal new insights about the fault's structure and movement. Geologists have discovered that the fault is not a single clean fracture but is a complex network of smaller intersecting faults that split and rejoin. This finding helps explain why earthquake activity is broader than previously thought, with seismicity occurring miles away from the primary fault strand. It also suggests that stresses can build up over a wider area prior to a large earthquake on the fault.