The Calaveras fault is an offshoot of the San Andreas, separating from the main fault a few miles south of town. The Calaveras is quite clearly active, as can be seen in these photos. The fault is well-known for creeping rather than sticking and slipping (and producing ruinous earthquakes).
The fault moves at rates as high as half an inch per year, although the rate is highly variable. The fault runs through numerous homes, and the movement is slowly tearing the foundations apart. Every decade or so homeowners must lift the houses up and replace the foundations.
The side of the porch has shifted to the right, away from the steps |
Our trip route took us south of town, to where Cienega Road intersects and then follows the San Andreas fault. Beyond the Hollister Hills State Recreation Area, one reaches the DeRose Winery, another famous fault locality. The winery was built directly on the trace of the fault, and has been destroyed twice by creep along the San Andreas.
The owners have always been kind to our students, allowing us to sneak through the wine-tasting event to have a look at the interior walls, which have been offset by several feet (below).
The wood post and the cement slab started out together...
The water-course at the south end of the winery is one of the most famous drainage culverts in existence because of how it has been offset by the fault (I forgot to get a picture this year; this is last year's version).
I don't know if realtors have to disclose the fault problems of home-buyers in Hollister, but if the DeRosa owners ever have to sell their winery building, they'll have a hard time hiding their fault...there is a brass plaque in the middle of the building declaring it a Registered Natural Landmark by the Department of the Interior!
The other San Andreas fault locality for our trip is on Highway 25 where the road is traversed by the fault. The road was completely repaved in the last year or two, but if you look carefully, you can see that the fault is already at work tearing the road apart again.
For a sense of comparison, below is a shot from 2003...
...and a shot from 2008 after a patch job.
We had an audience at our stop...a gang or rafter of dinosaur descendants trying to avoid being the main course later this week!
Wonderful photos, Garry. Thanks for such clear examples of how the ground is creeping - must feel a bit weird for the residents, surely?!
ReplyDeleteUnder the Alquist-Priolo act, it is necesssary in California to inform potential property buyers of hazards like faults, whether the property is located in a wildland fire interface zone, etc. I suspect it's really hard to sell one of those houses.
ReplyDeleteThose patches in the road, 11th picture down, look suspiciously like en echelon fractures.
ReplyDeleteAlthough I hadn't had much geoscience education at the time, both husband and I were educated enough (thanks to an undergrad intro Geology course) to get a fault map and make sure our house wasn't on any faults before we bought it. Since then we gathered that we're rather unique in that regard. How sad; some of this stuff should be taught in high school, at least in California!
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