What Causes Earthquakes?
That sounds like a silly question. An earthquake is of course when the ground is shaking. In my life I have experienced dozens of earthquakes. Some are mere jolts, some are quick shakes, some are gentle roller and a few (thank God not too many) are long shakers. Sometimes a large truck goes by and rattles the windows and even that will get my heart pounding. So, again, what is an earthquake?
An earthquake is caused by a sudden slip on a fault. The tectonic plates are always slowly moving, but they get stuck at their edges due to friction. When the stress on the edge overcomes the friction, there is an earthquake that releases energy in waves that travel through the earth’s crust and cause the shaking that we feel.
In California there are two plates – the Pacific Plate and the North American Plate. The Pacific Plate consists of most of the Pacific Ocean floor and the California Coast line. The North American Plate comprises most the North American Continent and parts of the Atlantic Ocean floor. The primary boundary between these two plates is the San Andreas Fault. The San Andreas Fault is more than 650 miles long and extends to depths of at least 10 miles. Many other smaller faults like the Hayward (Northern California) and the San Jacinto (Southern California) branch from and join the San Andreas Fault Zone. The Pacific Plate grinds northwestward past the North American Plate at a rate of about two inches per year.
Parts of the San Andreas Fault system adapt to this movement by constant “creep” resulting in many tiny shocks and a few moderate earth tremors. In other areas where creep is NOT constant, strain can build up for hundreds of years, producing great earthquakes when it finally releases.
Enjoy this classic scene from the movie “San Fransisco” with Clark Gable.
A terrifying re enactment of the 1906 quake.