San Andreas Fault tremors are triggered by SUPERHEATED rocks deep below the surface
Geologists have long thought that the central section of California’s famed San Andreas Fault – from San Juan Bautista southward to Parkfield, a distance of about 90 miles (145 km) – has a steady creeping movement that provides a safe release of energy. Creep on the central San Andreas during the past several decades, so … Read more