Berkeley Hills Landslide 2010

Standard

Last week’s third and final storm was a doozy, setting all-time record low pressure in a number of cities. Here in the Bay Area we got 3 to 8 inches of rain, and wind gusts of over 80 mph.

Powerful Thunderstorms Drench Berkeley and North Bay

All along the coast, 20 foot waves pounded the shore:

Storm Surf – Jan 2010

causing significant beach erosion:

Beach erosion – Great Highway, San Francisco – Lea Suzuki – Chronicle

And as I mentioned in my last post on the storms, the first of the three storms even produced a tornado (and some waterspouts) in Southern California. (see Berkeley Hills-El Nino Storms Hit Hard)

And of course, snow in the Sierras was measured in feet—8 to 10 feet in some spots!

Sierra Summit Had 10 feet of Snow! – Ken Clark

After the mid-week second storm, I wanted to hike into the Berkeley Hills to see the effects of the storm on the canyons. But because it was so muddy, instead of taking a fire trail, I took one of my favorite paved roads up into the Hills, Panoramic Way:

I usually walk south on Piedmont, past the Memorial Stadium:

And then take a left up Bancroft, just past the International House:

When Bancroft dead-ends, I walk up the Bancroft Steps and then cross over to Panoramic Way, which winds up into the Hills:

Panoramic Way – Google Map View

As soon as I got up into the upper, less-developed parts of Panoramic Way, I saw lots of rocks on the road and erosion like this:

Typical Panoramic Way Storm Erosion

Typical Panoramic Way Storm Erosion – Closeup

But I was really shocked when I came around a bend of on the upper part of Panoramic Way and found this:

Panoramic Way Landslide

A landslide!  Not a huge one, but still, impressive to see first-hand. Over a hundred feet of the steep upper slope adjoining the road had given way:

Source Area – Where the Slope Gave Way

And flowed down Panoramic Way for quite a distance:

Depositional Area on Panoramic Way

I was struck by how intact the top layer was; the whole section had been slipped down the slope pretty much in one piece, carrying along most of the shrubs intact.  Although small in scale, this little landslide had all three of the basic  elements of any landslide:

Of course, this landslide on Panoramic Way in the Berkeley Hills was a small one compared to the huge landslides California is famous for.  In the hills and on the cliffs all along the California Coast, heavy rains and steep, unstable land create a deadly combination that leads to highly destructive and often lethal landslides and debris flows. One of the worst in recent memory was the La Conchita landslide in 2005, which killed 10 people.

2005 La Conchita Landslide – John Lehmkuhl

In Southern California, this vulnerability is only made worse after wild fires, fanned by the infamous Santa Ana winds, denude the hills of vegetation.   Without vegetation to slow it down and trap it,  water runs off too quickly, causing flash floods and debris flows filled with huge rocks and tons of sand and gravel. Sometimes truly enormous boulders are set loose:

300 Ton Topanga Canyon Boulder – 2005 Landslide – (AP Photo)

You don’t have to have barren hills to be at risk for a landslide. Doing research for this article, I came across this amazing image of a landslide in England.  Known as the Holbeck Landslide, it occurred south of Scarborough in North Yorkshire:

Holbeck Hall Landslide – England 1993 – British Geological Survey

Fortunately, this particular landslide didn’t happen in a moment.  It took place over a two-day period, so people were able to evacuate when the first signs of movement became evident.  The scale of the movement of land is hard to fathom, until you know that the the cliffs in the depositional area are over 180 feet high! Geologist estimate over a million tons of loose glacial till (sediment) flowed down to the sea shore.

Looking at the Holbeck Hall image, I have to admit that the little landslide on Panoramic Way seems pretty insignificant! (Although I wouldn’t have wanted to be in its way when it broke loose!) Still, the soil physics involved are very similar.  All you need for a landslide is instability—relatively loose soil and rock, a steep-enough slope, and some sort of triggering mechanism, such as too much rain, an earthquake, or erosion of the base of a slope of land.  As this USGS diagram shows, there are all kinds of landslides:

Kinds of Landslides – USGS

The bottom line is that at some point, the friction and cohesion that hold the soil on a slope are simply overcome by gravity, and the soil and rock take off down hill, acting more like a liquid than “solid” land. In California, the majority of landslides caused by rainstorms, though earthquakes and tremors are a not-too-distant second.

Because of the unique geology and weather of California, landslides and debris flows are always going to be a part of the California experience, just like earthquakes, wildfires, Santa Ana winds, and El Niño events.  Because Californian love their hills and the vistas they offer, hill dwellers are always going to be in harm’s way.

Claremont Canyon Hills – Beautiful Vistas and Risk

We can do what we can to be safe, but as nature writer John McPhee makes so clear in The Control of Nature, even our best efforts may be inadequate.   In the last section of his outstanding book, he shows how  residents of the San Gabriel Mountains in Southern California have had little success in preventing debris flows from destroying their houses in spite of spending millions on creating man-made diversion pits and dams.

Landslide & Debris Flow Scars in the San Gabriel Mountains – USGS

From the standpoint of geology, landslides, mudslide, and debris flows are simply the more spectacular forms of the ceaseless erosion that shapes our beautiful planet, wearing down mountains and creating the sedimentary rock and soil so much of life depends upon.  Walking in the Berkeley Hills, you can see evidence of this  ceaseless erosion of wind and rain up-close and personal.

~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~

National Geographic has a fantastic video on YouTube about landslides.  The opening scene of a landslide in Portland, Oregon is simply amazing.  Watch as a fellow in a truck outruns a landslide coming down the street, sweeping away cars and everything in its path!

National Geographic Landslide Video

In this next amazing video, caught on camera by a Japanese research team, you can watch a whole mountainside slide across a road with the forest riding along intact!  Amazing!

Heyelan Japan Landslide

Advertisements

6 responses »

  1. Pingback: Rethinking Berkeley, Naturally! | The Nature of Berkeley

  2. Pingback: The Beauty of the Berkeley Hills-Part 1 | The Nature of Berkeley

  3. Pingback: The Beauty of the Berkeley Hills-Part 1 « Berkeley, Naturally!

  4. Pingback: Rethinking Berkeley, Naturally! « Berkeley, Naturally!

  5. Pingback: Have a look: Berkeley, Naturally – Berkeleyside

  6. Pingback: Taking a look at landslides in California « Goodheart's Extreme Science

Leave a Reply

Fill in your details below or click an icon to log in:

WordPress.com Logo

You are commenting using your WordPress.com account. Log Out / Change )

Twitter picture

You are commenting using your Twitter account. Log Out / Change )

Facebook photo

You are commenting using your Facebook account. Log Out / Change )

Google+ photo

You are commenting using your Google+ account. Log Out / Change )

Connecting to %s