The town of Hollister is bisected by the Calaveras fault, and numerous homes, sidewalks, and streets are slowly being torn apart by the constant movement, amounting to as much as 14 mm/year (0.55 inches). The embankment in the photo above appears in a number of geology textbooks as an example of fault motion.
The foundation for this 1920s vintage garage has also been seriously damaged. We've been visiting the spot for 28 years. It will be disappointing when they finally decide to renovate the building!
Probably the most famous example of fault creep in the region can be found at the DeRose Winery a few miles south of Hollister. The fault is far more active, with yearly offsets amounting to as much as 25 mm/year (1.0 inches). One can get a sense of the magnitude of the motion by comparing Saturday's image to one taken half a century ago (below)
Source: NOAA/NGDC, University of California, Berkeley. |
All of these incredible exposures are easily accessed. If you are ever in the vicinity of Hollister or Pinnacles National Park, don't miss the opportunity to lay your hands on a major transform plate boundary!
2 comments:
Your title is really corny, Garry! I need to go on this SAF geo-tour.
Always great photos of geology events, Garry. (great title by the way)
Sometimes I'm very glad I don't feel earthquakes where I live... well, only little bitty 3's and 4's Most movement happening on other side of Vancouver Island.
Cheers.
Post a Comment