Earthquake faults occur in interacting networks having emergent space-time
modes of behavior not displayed by isolated faults. Using simulations of th
e major faults in southern California, we find that the physics depends on
the elastic interactions among the faults defined by network topology, as w
ell as on the nonlinear physics of stress dissipation arising from friction
on the faults. Our results have broad applications to other leaky threshol
d systems such as integrate-and-fire neural networks.