Before I go much further, I want to stress how serious earthquakes are. It's not really a laughing matter if you live as I do in earthquake country. Millions of people have died from earthquakes in the last century or two, and they are still recovering bodies in Venezuela from the quake last June (6,500 dead so far with tens of thousands still missing).
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| San Francisco after the 1906 earthquake |
And we all know who to blame when that day comes, right? It's the San Andreas's fault...
Well, let's see if that is true...how well do we know our most famous fault?
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| Trace of the San Andreas fault on the San Francisco Peninsula. San Andreas Lake is in the foreground. |
The fault was discovered and named in 1895 by Andrew Lawson, a professor at UC Berkeley. He was mapping the geology of part of the San Francisco Peninsula, and he named what he thought to be a minor fault after the nearby San Andreas Lake. In 1906 the catastrophic San Francisco earthquake struck and it was immediately apparent that the fault was far more important, as the surface rupture extended more than 200 miles. Subsequent mapping revealed a total length of some 600 miles.
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| Source: US Geological Survey |
The fault is a transform plate boundary, dividing the Pacific and North American plates. The two plates are moving northwest, but the Pacific Plate is moving faster, causing relative motion that is right lateral.
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| Tectonic plates of the world. Source: US Geological Survey |
Right lateral means that the side opposite the fault from the observer has moved to the observer's right, as seen below in a curb offset by lateral motion on the Calaveras fault in Hollister, California. The Calaveras parallels the San Andreas in Central California, and is considered part of the same system of plate motions.
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| Curb in Hollister, CA offset by right lateral motion on the Calaveras fault. |
The fault began forming about 29 million years ago, and has moved more than 200 miles (during countless earthquakes of 15-20 feet per earthquake). This is best illustrated by the Pinnacles Volcano (in Pinnacles National Park in the Coast Ranges south of Hollister), which formed 22 million years ago, and was split by the fault and shifted 195 miles (the other half is in the Palmdale region).
Lots of people talk about the San Andreas fault, but relatively few people have actually seen it (or didn't recognize it when they did). What does the San Andreas look like? As it turns out, it's not always readily visible. Erosion tends to quickly erase evidence of fault motions, but they are preserved in many places if you know where to look. One of the most famous localities is Wallace Creek at Carrizo Plains National Monument west of Bakersfield. At that spot the San Andreas has offset the creek by 400 feet during perhaps two dozen earthquakes over the last 4,000-5,000 years (below).
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| Wallace Creek in Carrizo Plains National Monument |
The fault is much easier to see where it is creeping continuously. The fault crosses Highway 25 near Pinnacles National Park, and I've documenting the changes there over the last quarter-century. The photo below shows the cracks in the highway as of October 2026.
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| San Andreas fault crosses Highway 25 north of Pinnacles National Park |
People say things about the San Andreas fault. They're always finding fault, so to speak. Are these things true? Let's see...
- California will fall into the sea
- The San Andreas Fault causes all California earthquakes
- California has more earthquakes, and bigger earthquakes than anywhere else
- We are waiting for the “BIG ONE”
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| Source: https://scedc.caltech.edu/recent/index.html |
California has more earthquakes, and bigger earthquakes than anywhere else:
Let's roll the numbers. I'm not including the magnitude 9 quake of 1700, as it was most likely far too the north of California. Here they are:
- Number of (near) magnitude 8 quakes: 3 (1857, 1872 and 1906)
- Number of magnitude 7 quakes: 12-15
- Number of magnitude 6 quakes: 140+
We are waiting for the “BIG ONE”
The Big One. The one no one wants to think about. The Big Show.
The problem is, and you won't like it, that the statement needs to be refined a bit.
We are waiting for the Big Ones!
As noted previously, the San Andreas fault is segmented, and different parts have different seismic histories. There was the 1906 event in San Francisco, and the 1857 in Southern California. There is a segment in the Coachella Valley that has been lock up and building stresses for some 300 years. And there are other major faults capable of mayhem. The 1872 quake in Lone Pine wasn't on the San Andreas fault, and neither were many other magnitude 7 events.
Seismologists cannot predict individual quakes with any kind of reliability, but they deal quite well with probability. Working groups have produced maps that reflect the possibility of major quakes on any number of California fault lines and have produced probability maps like that above. It is a bit dated (2008), but there have already been 3 or 4 magnitude 6.7 and greater quakes, showing that the long-term predictions are valid. The quakes are going to happen. We just don't know precisely when.So, no blame on the San Andreas, at least not yet this century!
This one is subject to change...
This blog post was written to coincide with the Great California Shakeout to be held on Thursday Oct. 15 at 10:15 am.
I will also be presenting a public lecture as part of Modesto Junior College's MAPS Speaker series on Friday night, October 16 is Sierra Hall, Room 132 on our west campus at 7:30 pm. I'll be speaking about, of all things, the San Andreas fault!






























