The San Andreas Fault line, which stretches some 800 miles across California, marks the boundary between the Pacific and ...

South of Parkfield, the fault is locked, meaning the two plates do not move against one another. North of Parkfield, the San Andreas fault moves freely, with the plates creeping against one ...

New research uncovers a surprising clue in earthquake forecasting: tiny curved scratches on fault planes. These marks reveal ...

The San Andreas Fault is a continental transform fault that extends roughly 1,200 kilometers (750 mi) through California. It forms the tectonic boundary between the Pacific Plate and the North ...

Rather, two plates move against each other, building up tension, then releasing the tension in a sudden and often violent jerk. This sudden jerk creates an earthquake. The San Andreas Fault is ...

A mid-ocean ridge would then mark the boundary between the plates. Mountains and a rift can be seen along the San Andreas Fault.

Movement along the San Andreas Fault was to blame. The North American and Pacific tectonic plates had moved past each other by more than 15 feet — compared to an annual average of two inches.

A good example of this is along the San Andreas Fault where the Pacific and the North American plates are sliding past each other.

If the plates move a significant distance very ... An example of this type of boundary is the San Andreas fault, California.