Archive for the ‘Oakland rock types’ Category

The Skyline chert exposure

1 August 2022

For several miles starting near the top of Marlborough Terrace, Skyline Boulevard runs through a belt of blond chert that makes for striking roadsides and some of Oakland’s highest homes and best views. Near the south end of this stretch, north of Elverton Drive, the road runs east-west for about 700 feet. It’s just you, the view, and these rocks. In my book I describe them as “pale, flinty chert in layers a few inches thick alternating with thinner layers of soft brown shale. The layers, thousands of them, stand on end like a storm-swept forest of golden bamboo.”

Note that the nice wide verge is now blocked by a line of huge logs. These extend for miles along Skyline and Grizzly Peak Boulevard. There are still small places to park, though.

Here’s the location on the map. The land is an outlier of the Sibley Volcanic Regional Preserve, and a little trail runs along the ridgetop between the two boulevards.

The rock in this roadcut is chert: a hard, waxy-looking stone made from accumulations of microscopic diatom skeletons. It ranges from white to brown to black, simple to complex. It dates from the middle of the Miocene epoch, probably the Tortonian age around 12 million years ago.

The complexity extends to the larger, outcrop scale. Notice how the straight, even bedding on the left gives way to distorted layers on the right. The boundary between them is a fault. There are several more along the roadcut.

In addition to the faulting, this even-bedded, slowly accumulating sediment was periodically disrupted while it was still soft, presumbly by large undersea landslides triggered by earthquakes, just like today. Here’s a more extreme example; notice the wisp of chert entrained in the mixture on the left.

Here’s a foot-thick bed of clean white sandstone, preserving an ancient submarine landslide. By the way, it appears that nearly all of these rocks are overturned, their upper surfaces now facing to the right.

In the middle part of the roadcut, it really gets hairy. (This is the biggest image of the set.)

Other parts of the roadcut look tidy and regular, but erosion has cut into softer parts of the formation in the century since Skyline was built to attract developers.

Here’s a closeup of the groove in the middle. What caught my eye was the dark zone in it with orange veins, which shed pieces onto the roadside slope below.

The material (on the right) is a lightweight siltstone shot with films of black.

It’s likely that the black films are the remains of crude oil — not the only possible explanation, but it’s how to bet. Chert is a source rock for petroleum because the diatoms that compose the rock manufacture oil to help their opal shells float. As the diatom ooze becomes rock, the oil is released and migrates elsewhere until it’s trapped in an underground structure, eaten by microbes or oxidized in the atmosphere. Our Miocene chert is a close relative of the widespread Monterey Shale, which is responsible for California’s richest oil deposits. So the zone of orange veins might be a former escape avenue for the local oil — an injectite.

But above the roadcut, a little off the ridgetop trail, I encountered an intriguing alternative in this heavily etched material impregnated with silica.

Here’s a side view of another specimen showing the veins of hydrothermal quartz (chalcedony). The matrix between them appears to be the same stuff of the orange veins.

Now the formation of chert from plain diatom ooze, or diatomite, takes place at low temperatures and pressures. It’s very gentle. Hydrothermal silica is a sign of higher temperatures. Something more active than trickling crude produced this. Again, various explanations are possible, and these scattered blocks of rocks aren’t firmly connected to the putative injectite in the roadcut. I’ll just have to poke around here some more. The complexities multiply.

By the way, maybe some of you remember when this stretch of road was a cool, shady run through a high eucalyptus forest. That was how it was when I first explored the area. Google Earth stacks imagery of this area going back to aerial photos from 1939, and there was no eucalyptus here at all until the 1980s. Yet the trees were a hundred feet high in late 2003.

The Park District took them out around 2005, and in the fall of 2009 just a little fringe along Grizzly Peak was left.

Twelve years later, chaparral and oak-bay-madrone woods had made quite some headway.

But if you ask me, the site would be an excellent one to try restoring the traditional fire-groomed grassland that once covered all the hills north of the redwood groves. The Park District owns it, and California still has experts in the old ways.

PS: I’ve started an occasional newsletter. You can sign up and read the inaugural issue here.

PPS: The book’s fundraising drive has met its $5000 goal, but contributions still come in. More on the Deep Oakland page.

Avalon Hill

18 July 2022

There’s a little hill south of the UC Berkeley campus, near the Claremont Resort and the Hayward fault, that cried out for a visit. It stands out on Google Maps (with the “terrain” setting, naturally).

On the geologic map, it appears as a blob of Franciscan sandstone.

I thought I’d give it the same treatment I gave Easter Hill in Richmond: explore the rock and comb through old maps and documents.

The road running by the south side of the hill is Avalon Avenue, so I’ll call it Avalon Hill. It was never exactly a landmark, but it has a past and retains a certain presence.

The hill was owned by John Kelsey in the late 1870s, and Kelsey Street commemorates his name. Today’s Claremont Avenue was called Telegraph Avenue at the time, as shown in the 1878 Thompson map.

In 1884 the Berkeley Water Works excavated a large reservoir on the hill, and the following year the Alameda Water Company took it over. The Garber Reservoir held a million gallons and was lined with concrete. Here it is on the 1894 Wagner map.

It is not to be confused with today’s Garber Reservoir, the flat-roofed structure 1500 feet south on the north side of Claremont Avenue.

Development began to surround the hill in the 1890s and 1900s, especially after the 1906 earthquake. From then until the 1930s, the struggling private water companies of the northern East Bay merged, the East Bay Municipal Utility District swallowed them whole, and the water delivery system began a slow and expensive transition to the rational and robust setup we enjoy today. The 1912 street map shows the property still in the hands of the Peoples Water Company, the next-to-last of the private firms.

I don’t know when the reservoir was decommissioned and removed, but the homes adjoining it were built starting in the 1910s. The large home on the hilltop was apparently built in 1960.

The best picture of the hill itself is the digital elevation model made from a special survey of the Hayward fault. Its sides are too steep for streets, which has helped keep it quiet and isolated.

On the north side, Garber Street has a rustic interlude where a narrow road sashays down the hillside like a mini-Lombard Street. Avalon Avenue, on the south side, is blessed with three stairways, one at the end and two going down to Russell Street.

All those old houses with their mature landscaping cover up the rocks very effectively, I can testify. But there’s an excellent exposure at the end of Avalon Avenue underneath a private driveway.

What few flat surfaces there are on it appear to reflect fracture planes, imposed by the tectonic stresses on the rocks over the years, rather than any original bedding.

Up close, the rock is a hard siltstone much like the rocks in the quarries of the Piedmont crustal block: the Bilger, Blair and Davie tennis stadium quarries.

But just looking at it isn’t definitive. The geologists who’ve mapped it have left it unclassified (KJfs) rather than lumping it with the sandstone of the Novato Quarry Terrane (Kfn) exposed in the Piedmont block to its south. Here’s a larger piece of the geologic map showing what I mean: it might be the northern tip of the block or it might be the first of a string of rock bodies to its north. The thrust fault leading up to it, the dotted line with the teeth on the upthrown side, is reasonable but conjectural.

Avalon Hill is a cool little bit of Berkeley. Stick your nose in and poke around some time.

Yes, “Avalon Hill” is a private joke. My siblings and I warped our personalities in the 1960s by moving armies and fighting over the rules of the board-based wargames produced by the Avalon Hill company, starting with Tactics II and Gettysburg.

Return to Pine Top

25 April 2022

A brief visit to Mills College for the recent pow wow reminded me of some business — not unfinished business, but rather an inquiry ready to renew. The upper end of the Mills grounds is very different from the lush central campus with its beautiful floodplain setting, and it has the possibilities of bedrock and fault-related findings. And it’s been seven years. To refresh our memories, here’s the geologic map.


Pine Top is labeled Jb next to Lake Aliso at the east end of Mills College. Qpaf, Pleistocene alluvium (the Fan); Qhaf, modern alluvium; Jsv, Leona volcanics (Jurassic); Jb, basalt; Jgb, gabbro

I’ve always wondered about Pine Top. It stands up so steeply and dramatically at the foot of the high hills, right on the Hayward fault (which is poorly localized here). The digital elevation model of the hill makes it look as if it had been quarried, and indeed there are records of a quarry on the college land.

I’ve also wondered about Pine Top because the basalt “Jb” is hard to find, and I came up empty on my first visit. The hill appeared to be fully mantled in soil.

The campus is especially pretty right now. I hope they can get past their problems and resume their long successful history in Oakland.

Lake Aliso is its usual self, thanks to the late-season rains.

Supposedly the lake is a sag basin related to the Hayward fault, but I’m starting to think that it owes its existence entirely to damming.

This old photo of the lake, from around 1893, shows the side of Pine Top nicely forested in oaks, which would not be the case had there been a quarry there. I think the quarry was located north of the lake where the freeway now runs.

Source

This time I found the original footpath up the hill. Students used to have costumed processions up this path, bearing torches and regalia.

At the top, they would assemble around the Hearth and enjoy their celebrations.

Maybe some alumnae with long memories can add comments about how it used to be.

The view from the top has closed in as the trees have grown, but in the old days it was surely fine.

But anyway, this time I found bedrock — well, pieces of it, around the big microwave tower that was emplaced up here since my last visit. Here they are arranged for a portrait. I also found a little in the old footpath.

This is not basalt by any means, not even a highly altered basalt. This is the highly altered ash of the Leona volcanics, what the old-time geologists with their eyeballs and hand lenses called the Leona Rhyolite. That calls into question not only the “Jb” label for Pine Top, but the whole stripe of Jb drawn on the geologic map. Just some more things to go and check out this summer.

McAdam’s quarry

11 April 2022

One of my first outings during the pandemic era was a hike up Shepherd Canyon in search of Alexander McAdam’s sandstone quarry. But I was missing a telltale clue. Now I think I’ve found it.

I wanted to locate the quarry because it produced the stone used in the historic First Unitarian Church in downtown Oakland, the only example I’ve found of a truly local rock used as dimension stone in a building instead of crushed stone in an anonymous construction.

The clues I had pointed to a location “at the head of Thirteenth Avenue” somewhere “in Medos Cañon, back of Piedmont.” I thought this meant some place in present-day Montclair, but all the old maps I checked didn’t show any land there belonging to McAdam. Then I tracked down the 1894 Wagner map of Alameda and Contra Costa Counties, and here’s where his ranch was: over the ridge above Shepherd Canyon, in the valley of Redwood Creek.


Shepherd Canyon in the center; the old Thorn Road runs around its north edge. The Heyland property at lower left is in Dimond Canyon and the Hays School is in present-day Montclair. The McAdam property is at lower right past the county line, shown by stippling.

The land is within Redwood Regional Park, so I surveyed the territory last week. Here’s a closeup of the map, showing McAdam’s 131.24 acre holding.

And here’s where it sits in the geologic map.

This is very steep country, in an area where the redwood groves had been logged out forty years before. McAdam used it as ranchland, like others in this remote district, but he also operated a successful quarry here somewhere. It wasn’t in the coarse, crumbly Oakland Conglomerate (mint green) or the shaly stuff of the Shephard Creek Formation (pale green), but somewhere in the thick-bedded, fine-grained sandstone of the Redwood Canyon Formation (Kr on the map, olive green).

Fortunately, Redwood Regional Park maintains the old trails and logging roads, so I superposed McAdam’s land on the park’s trail map and gave it all a good look. Note: the poison oak is very healthy this year.

The only place a quarry would make sense is at the very top of the property, but if you’re up for it, the Tres Sendas trail takes you down to some nice woods.

The rock here is appropriate, just like the stone in the church.

And some of it fractures nicely enough to be dressed into ashlar blocks.

But it would be nuts to operate a quarry down in the back forty. Up on the ridgetop in the northwest corner of the land is where I think McAdam had his pit. It’s the backdrop of this view over the spot where McAdam’s ranchhouse was, at the westernmost corner where the Waterloo Staging Area is today.

It was accessible via the Castle Canyon road, as seen in the 1897 topographic map. The McAdam place is in the center, at the end of the road.

The hilltop is just off high-lonesome Wilton Drive, where I last took you three years ago for the Shepherd Canyon circumambulation. The views from there are still wonderful.

The slope immediately below, too steep to think about descending, is where I think the quarrying went on. The outcrops of Redwood Canyon Formation display good rock.

I’m glad to put this little mystery to bed. And if the Unitarian Church must replace its stone with authentic materials, they know where to look.