North side of 4th Street, looking east from near Locust Street. Note the 'waviness' in the curb. According to residents, the street develops a dip which has to be fixed every eight to ten years.
Image Credit: Joe Dellinger.
Photo Date: June 18, 1985
Seismic Creep
Seismic creep is the constant or periodic movement on a fault as contrasted with the sudden rupture associated with an earthquake. It is a usually slow deformation of rock resulting from constant stress being applied over a period of time. Sometimes aseismic slip is observed at the ground surface along a ruptured fault that has produced a substantial earthquake. Examples are from the Hollister and Hayward, California, region. Several of the slides are split images of a location, comparing fault movement over the years.