Photos from the Vault

When will ‘the big one’ hit? Researchers dig for San Andreas Fault secrets in SLO County

Video: How prepared or unprepared are you for an earthquake?

FEMA explains what you should do before an earthquake happens and when it occurs in an animated video called "When The Earth Shakes."
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FEMA explains what you should do before an earthquake happens and when it occurs in an animated video called "When The Earth Shakes."

Most people prefer to be dead before they are buried. I’m one of them.

But if things shake out differently, we won’t be that lucky.

In 2011, I stood with three researchers in a trench 10 feet deep, a strip of blue sky overhead. That was unremarkable, except for the fact that we were inside the San Andreas Fault.

At that point near Wallace Creek on the Carrizo Plain, the fault averages a major violent rupture about every 150 years.

A major quake was four years past the average when we were inside the fault. It’s a dozen years overdue now.

Since 1985, scientists have been working in Parkfield — roughly 70 miles north west up the fault — trying to divine the secrets of how to predict earthquakes.

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Wallace Creek swings 430 feet northwest as the creek bed issues from the Panorama Hills before finding its historic outlet. Geology outpaces rainfall in the dry Carrizo Plain and the Z shape is the result of 3,700 years of movement on the San Andreas Fault. In 1857 up to 30 feet of offset was recorded in the Great Earthquake. The group was part of a Cuesta College mini-course led by Steve Schubert in 2003. David Middlecamp dmiddlecamp@thetribunenews.com

The Parkfield portion of the fault shakes with 6.0-magnitude quakes regularly, roughly every 22 years.

Further south, the San Andreas Fault has been locked. The last time it broke bad was 1857, when it ripped from Parkfield to Cajon Pass near San Bernardino — a distance of 255 miles.

Earthquakes are most frequently found where the earth’s massive tectonic plates bump into or scrape past each other.

But the San Andreas Fault only accounts for about half of the geologic collision between the Pacific Plate moving north and the North American Plate moving south. There are thousands of faults in the west that can or will wreak havoc.

The media obsesses over “the big one,” but countless quakes happen every year in California.

Only a few are large enough to be noticed and named. Temblors in Coalinga, San Simeon, Northridge, Whittier Narrows, Loma Prieta and now Ridgecrest are all remembered for loss of life and millions of dollars in damage.

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The San Andreas Fault is the line from left to right in the middle of this March 29, 1999 photo. It offsets this stream in the Carrizo Plain in this aerial view. This area is 60 miles south of Parkfield. Rainfall is so scarce in the plain that the stream follows the fault line briefly before regaining its old stream bed. David Middlecamp dmiddlecamp@thetribunenews.com

None of those quakes were “the big one.”

Nathan Welton wrote this story, published in The Tribune on Oct. 5, 2004.

Quake forecasts a shaky science

It’s like Old Faithful.

The San Andreas fault in Parkfield, like the legendary geyser, grumbles regularly — but predicting its geologic burps with clocklike accuracy has always been a shaky science.

Still, the area might yet be a fount of reliable earthquake activity. Because scientists have predicted a relatively powerful magnitude-6.0 rattler in that area for years, last week’s tremor seems to support mathematical models used for long-term quake warnings.

Besides showing that a temblor’s strength, location and approximate time — at least within a multiyear window — can be reasonably foreseen, scientists say last week’s quake also gives credence to other formulas that warn of shakers statewide.

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Sinan Akciz, a research scientist at U.C. Irvine shows an area of interest, an break in a former stream bed. By tying together the information from many data points the movement of the San Andreas fault is being documented at Wallace Creek by a research team. The location on the Carrizo Plain has been a favorite of researchers for decades. 7-29-2011 David Middlecamp dmiddlecamp@thetribunenews.com

One prediction says a 6.7-magnitude earthquake will hit San Francisco within 30 years, for example. The science behind that warning is similar to the science that forecasted last week’s event in Parkfield.

Experts hope to further polish their crystal ball with the help of a 10,000-foot-deep hole they’re now boring into the ground in Parkfield, into which they’ll place an array of sensors to measure the earth’s movements.

While long-term quake prediction appears sound, it’s the short-term predictions — such as warnings in the early 1990s that a quake could hit within days — that need to be re-evaluated.

“There was nothing there (in Parkfield) that met the rules we set up in the ‘80s,” explained Andy Michael, a U.S. Geological Survey seismologist. “We’re now looking at the data to see what might have been there that would have been new and interesting or could help us next time” in short-term predictions.

Long-term predictions

In the late 1970s, scientists began tracking seismic activity around Parkfield and developing a statistical warning system for earthquakes.

That system was and still is based largely on the fact that the area has experienced a magnitude-6.0 quake every few decades for the past 150 years.

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Members of the media inspect the drill pipe during a tour of EarthScope’s San Andreas Fault Observatory at Depth drill platform and research site on Sept. 2, 2004 Joe Johnston jjohnston@thetribunenews.com

David Oppenheimer, project chief for USGS Northern California seismic network, said long-term prediction “is not rocket science — it’s just a matter of doing your homework.”

The last two Parkfield temblors for which scientists have decent data — in 1966 and 1934 — occurred because of the same geologic phenomenon, he said.

North of Parkfield, the San Andreas fault slides along, with one side rubbing in a direction opposite the other. This so-called strike-slip fault — different from the up-and-down thrust that jolted San Simeon last December — typically moves smoothly because of relatively frictionless rock beneath the surface.

“There are little pieces inside the fault zone of different kinds of rock that are higher friction,” Oppenheimer said. “They get stuck and pop off quakes of lower magnitudes like one and two.”

On the south side, however, there lies a bend in the fault line that stalls the continual creeping. Eventually that stall builds up enough force and a stronger quake, such as the one on Sept. 28, occurs.

Oppenheimer said that the geology of the area guarantees the fault will let loose a quake in that area every so often.

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David Haddad, a PhD candidate from Arizona State University, wears a mask to guard against Valley Fever as he smooths the wall of a trench before it is photographed July 29, 2011. The movement of the San Andreas fault is being documented at Wallace Creek by a research team. The location on the Carrizo Plain has been a favorite of researchers for decades. David Middlecamp dmiddlecamp@thetribunenews.com

Although the numbers say last week’s shaker should have happened around 1988, according to Michael, it wasn’t statistically late. And while forecasters didn’t pinpoint the exact time, they still nailed the location and the magnitude.

In some ways, earthquake prediction is akin to the “best before” date on a milk container: Scientists can predict what’s going to happen (a curdle or a quake) and where it’s going to happen (in the carton or in Parkfield) but they can’t say precisely when.

But they say their mostly accurate predictions validate the methods used to forecast future large earthquakes in metropolitan areas. And in the meantime, scientists are probing the San Andreas fault for clues to improve their accuracy.

“It’s still called the Parkfield Prediction Experiment,” Oppenheimer said, emphasizing the last word. “We saw some quasi-periodic behavior in the earthquake cycle when we first started in 1979, so the idea was let’s get instrumentation in the ground and get funding and record data before a significant earthquake.”

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Liza Fierro, along with her 9 month-old son Diego, inspects her bedroom where her dresser was knocked over and some pictures fell off the wall as a result of the 6.0 magnitude earthquake in 2004 near Parkfield, Calif. Joe Johnston jjohnston@thetribunenews.com

In the short term

What could be improved most about earthquake prediction in Parkfield is the short-term warning system, Oppenheimer said, which for years has been in place to caution people of imminent, strong quakes.

For more than two decades, and particularly in the early 1990s, experts continually warned of the possibility of an impending temblor, using a scheme similar to the federal government’s current terror alert system.

The warnings have an A through D severity rating and say a quake could theoretically occur within several days.

The system has cried wolf with every alert issued.

The reports are based on two main measurements along the fault in Parkfield: the speed and distance one side moves when compared with the other, and the strength of minor quakes in the area.

Those minor quakes are relatively common — about 30 shake the state daily.

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An old water tank is shown outside the Parkfield Cafe in 2004 in Parkfield. Michael A. Mariant file

A key to the prediction system was historical: The last few magnitude-6 Parkfield shakers followed a strong, magnitude-5 foreshock less than 20 minutes before.

So when a magnitude-4.7 tremor occurred in October 1992, scientists for three days warned the public of a 37 percent chance a magnitude-6.0 quake would strike.

It never did.

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Chris Walls, with the Southern California Plate Boundary Observatory, gathers his media group together as he gets ready to take them up to the drill platform during a tour of EarthScope’s San Andreas Fault Observatory at Depth drill platform and research site in 2004. Joe Johnston jjohnston@thetribunenews.com

In 1996, after realizing their cautions came too frequently, scientists redefined the area where a foreshock would have to occur, making it more specific, and increased by 1.5 the magnitude necessary for a foreshock to trigger an alarm.

The future of predictions

Scientists will soon have a new tool to better their understanding of subterranean geology and maybe even improve their ability to accurately predict quakes.

In June, a 182-foot-tall drill began boring a 10,000-foot hole into the Earth on a ranch in Parkfield with the goal of placing hundreds of sensors that will measure temperature, pressure and the tiniest of the Earth’s movements.

The goal of the $300 million project, called the San Andreas Fault Observatory at Depth, or SAFOD, is to allow scientists to study how faults work and how earthquakes happen. The fault zone is poorly understood at that depth.

Scientists hope that the information gained during future quakes will help accurately predict earthquakes.

Since drilling began in June on the Bear Valley Ranch, 25 miles northeast of Paso Robles, the rig has already penetrated more than 7,000 feet. Scientists will conclude their drilling in 2007 and then invest 15 years monitoring the fault.

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