January 7, 2021
The Fault is Not in Our Stars
I had to get out of the house to escape my laptop and my doomscrolling the news about the attack on the Capitol yesterday. What better way to counteract the doom and gloom than by doing something safe and soothing like riding along the San Andreas Fault. The fault, dear Brutus, is not in our stars but in our rocks.
You may have heard that California is what is called "geologically active." That's because two tectonic plates, the Pacific and the North American, are grinding against each other along the western part of the state at the San Andreas Fault. The San Andreas is probably the most famous fault in the world (at least to Californians), but of course there are many other active faults. For example, offshore from northern California to Vancouver Island is the Cascadia subduction zone, which might be the site of the next Really Big Quake. Kathryn Schulz won the Pulitzer Prize for her 2015 New Yorker article about it.
Geologists say that the San Andreas is really a fault system, with lots of other faults splitting off or paralleling the main fault. Two of the more active ones are across the bay from me, the Calaveras and the Hayward. The Calaveras is a creeping fault, moving several millimeters every year. The nice wide level places for building schools and libraries and city halls turned out to be right on the faults. That creep is hell on plumbing and curbs and buildings. When either of those decide to really move it will cause a lot of damage.
The main course of the San Andreas is easily seen if you use the Terrain layer on the route map.
Something else special about this ride is that I loaded up Pokey in the car and drove somewhere else - I didn't start from home. It's been a few months since I did that.
The first leg was on Cañada Road, a really nice road that goes past old estates and the Pulgas Water Temple, where the Hetch Hetchy Aqueduct finishes its travels from Yosemite. Then we crossed some hairy freeway on/off ramps to get to the next section, the Sawyer Camp Trail, which runs along the shore of a couple of reservoirs that sit right on the fault. After that I crossed over the top of the hill to see glimpses of San Francisco Bay, eventually looping back to Cañada Road.
Heart | 0 | Comment | 0 | Link |
Cañada Road is a lovely ride. It starts out in the horsey town of Woodside and goes north to Hwy 92, the route between the bay the the ocean. The northern half of it, the part I rode, used to be closed on Sundays to vehicular traffic but I think that's been suspended for the time being. It's got a few long rollers and slow curves to give interest. The last couple of miles are above Upper Crystal Springs Reservoir so the scenery is wonderful.
This area was where many San Francisco rich people had estates in the late 1800s and continues to this day, where they could escape the cold SF summers and have a bit more elbow room - you know, a thousand acres or so. One was the Bourn family and their estate Filoli, which is a word coined from their motto, Fight-Love-Live. Mr. Bourn made his wealth through the Empire gold mine in the Sierra. The second family to own the estate was Lurline Matson Roth and her husband. She was a member of the Matson shipping family. She donated the estate to the National Trust for Historic Preservation after her husband's death. Both the Empire mine and the Matson Line are big parts of California economic history.
However, the main claim to fame these days is the house's connection to the old prime time soap opera Dynasty. The exterior shots of the family home in the opening credits are those of Filoli.
Something I learned later is that the main fault runs directly under the mansion and gardens. Huh.
We did not go to Filoli today although spending a day there exploring the fabulous gardens might be a good covid activity soon.
Heart | 0 | Comment | 0 | Link |
My usual pitstop along Cañada Road was closed. That's the Pulgas Water Temple, an edifice that glorifies the end of the travels of the water transported along the Hetch Hetchy Aqueduct from the Hetch Hetchy Reservoir in Yosemite to the people of San Francisco. I also use Hetch Hetchy water every day. The grounds are nice and lots of weddings are held here. Not right now though.
Heart | 2 | Comment | 0 | Link |
Heart | 3 | Comment | 0 | Link |
Heart | 1 | Comment | 0 | Link |
The northern end of Cañada Road is where many cyclists park to before starting one of several good loops you can do in this area, with all the hill climbing you could want. The views open up and you have a good look at the Pacific Plate from the North American Plate.
After a rather hairy negotiation of on- and off-ramps where Hwy 92 becomes a freeway (don't think I need to do that again) I got to a newish bike path above Lower Crystal Springs Reservoir that takes you off a road with no shoulders. The path meanders along the contour line above the lake and best of all had the toilet I wish was available back at the water temple. Phew.
Heart | 1 | Comment | 0 | Link |
Heart | 0 | Comment | 0 | Link |
The dam that created the Crystal Springs reservoirs was redone a few years ago. Thankfully they incorporated more infrastructure for bikes and pedestrians. Nice views from there.
Heart | 1 | Comment | 0 | Link |
I had some trouble negotiating the transition from the dam to the Sawyer Camp Trail because the dam parking area was jammed with ranger trucks and cop cars. Turns out there was a missing person search going on.
Lifted from the San Mateo County Parks site: "Sawyer Camp Trail, later called San Andreas Valley Road, or simply Valley Road, was once the main highway between San Francisco and Half Moon Bay [on the coast]. Wagons pulled by teams of horses hauled wood over the road. Much of the old road was flooded by Crystal Springs Reservoir by 1888.
"When the city of San Francisco took over the watershed lands, narrow, winding Sawyer Camp Trail was then a county road. The Water Department fenced it for the protection of San Francisco's drinking water. In 1978, the San Mateo County Board of Supervisors designated the road a non-vehicular recreation trail and paved it for bicycles with funds provided by the State Department of Parks and Recreation."
Heart | 4 | Comment | 0 | Link |
The geology around here is pretty interesting. I took exactly one geology class - which I found a thousand times more interesting than I thought I would - so if anyone else knows more please feel free to correct. One thing I remember is that the rocks around here are known as the Franciscan Complex. It used to be called the Franciscan Melange which I kind of prefer. Those rocks were formed before the San Andreas was created, when the no-longer-existing Farallon Plate subducted under the North American Plate, scraping off all these rocks onto this margin of the North American Plate. From what I gather there are a few different ways the melange shows up. You can explore more photos at the Wikipedia page.
Heart | 4 | Comment | 0 | Link |
Heart | 5 | Comment | 0 | Link |
Halfway along is a tree called the Jepson Laurel. It's more than 600 years old, and is named after one of the early California botanists. There's a picnic area, a loo, and an archaeological artifact near the tree.
Heart | 3 | Comment | 3 | Link |
3 years ago
My park had to pay to keep the pay phones. We kept them because cell service is iffy up in the canyons. Once I had a devil of a time getting them reinstalled when a well-meaning IT guy had them removed due to low usage (4 times in six months) without telling us.
3 years ago
Heart | 2 | Comment | 0 | Link |
Once we leave the Jepson Laurel the trail climbs until we reach the dam that created the San Andreas Lake in 1868. The lake flooded the San Andreas Valley where various Spanish explorers camped now and again. The fault was named after the valley by geologist Andrew Lawson in 1895 (although many people think he named it after the lake).
This dam, which looks to be mostly earthen, survived two major quakes since it was built - in 1906 and in 1989 - plus many minor ones. I couldn't find any info about it being significantly damaged in either of those big quakes.
Heart | 3 | Comment | 0 | Link |
Heart | 0 | Comment | 0 | Link |
The San Andreas is what they call a strike-slip fault. The Pacific Plate is moving northwest relative to the North American Plate.
Heart | 2 | Comment | 0 | Link |
The trail keeps climbing up above the lake until we reach aptly named Skyline Boulevard. At the end of the trail is another plaque to commemorate Portola and his merry band who wandered around here and "discovered" San Francisco Bay.
Heart | 1 | Comment | 0 | Link |
This discovery thing is interesting. Sir Francis Drake sailed along the California coast in 1579, almost 200 years before Portola. He spent about six weeks somewhere near SF Bay to repair his ship but made no real mention of the bay or any exploration of it. Some say he was at what is now called Drake's Bay in Pt Reyes, outside SF Bay, and some think he was just inside the bay near Sausalito. Drake said he installed a plaque laying claim to Nova Albion for England but it's not been found. One possibility that might explain his missing the bay is the usual coastal fog that time of year. It can be pretty thick and it would be easy to miss the relatively narrow Golden Gate.
So, back to today, at the Portola plaque I left the Sawyer Camp Trail and crossed under the freeway to Skyline Boulevard. I made my own discovery of San Francisco Bay.
Heart | 1 | Comment | 0 | Link |
Heart | 2 | Comment | 0 | Link |
Heart | 0 | Comment | 0 | Link |
Heart | 2 | Comment | 0 | Link |
Heart | 0 | Comment | 0 | Link |
One of our local oddities is what has come to be called the Flintstone House. You can easily see it from the freeway. Read more about it and see better photos: Flintstone House.
After this I stayed on the main shoulderless road to head back to Cañada Road and the car, deciding not to go on the bike path that paralleled the road. That was a mistake sorta, since I forgot the path followed the contour and the road went up and over a nice hill. Ah well. Luckily traffic was light.
Heart | 2 | Comment | 0 | Link |
Just before I got back to the car, there is a formerly grand entrance to a former estate owned by the Phlegers (now part of the Golden Gate National Recreation Area). All the years I've been driving or riding by here I never stopped to explore the gate. Until today. Again, I blame you all for making me take a closer look at where I live. I looked in the window and saw there was a door on the other side. Then I saw you could walk behind the wall to see the door.
The car was just a few yards away. Loaded up Pokey and headed home.
Heart | 3 | Comment | 3 | Link |
I bought this car when (1) I needed a new car and (2) knew I would be buying a trike so found one that Pokey would fit in.
3 years ago
Afterword: I'm posting this a couple of weeks after the fact. About three days ago we had a nice little 4.5 quake about 30 miles south of us right on the San Andreas Fault. It shook the house and rattled the windows well enough that I just started thinking I better get under cover, but then it stopped. I was shaken but I did not stir.
Today's ride: 26 miles (42 km)
Total: 114 miles (183 km)
Rate this entry's writing | Heart | 9 |
Comment on this entry | Comment | 8 |
3 years ago
Glad you enjoyed the journal.
3 years ago
Great ride. And I'd love to see that Flintstone house. I have seen the Flintstones' Bedrock City campground in Custer, SD though. Freaky!
3 years ago
One of my favorite toys as a young kid was the Flintstones village I had. Plastic sheet with roads and houses marked out, plastic rock houses to put on them, and little dolls for all the characters. I think the Rubbles' house lasted into my teen years, still used by the youngest sibs.
3 years ago