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Photos of Murray and Segall are available at http://newsphotos.stanford.edu
(slug: Murray & Segall).
Their study, Testing time-predictable
earthquake recurrence by direct measurement of strain
accumulation and release, will be published in
the Sept. 19 issue of Nature.
Study casts doubt on validity of standard earthquake-prediction model
A new study by Stanford University geophysicists is raising serious questions about a fundamental technique for making long-range earthquake predictions.
Writing in the journal Nature, geophysicists Jessica Murray and Paul Segall show how a widely used earthquake model failed to predict when a long-anticipated magnitude 6 quake would strike the San Andreas Fault in Central California.
In their Sept. 19 Nature study, Murray and Segall analyzed the "time-predictable recurrence model" -- a method scientists use to calculate the probability of future earthquakes. Developed by Japanese geophysicists K. Shimazaki and T. Nakata in 1980, the time-predictable model has become a standard tool for hazard prediction in many earthquake-prone regions -- including the United States, Japan and New Zealand.
For example, the U.S. Geological Survey (USGS) relied on the time-predictable model and two other models in its widely publicized 1999 report projecting a 70-percent probability of a large quake striking the San Francisco Bay Area by 2030.
The time-predictable model is based on the theory that earthquakes in fault zones are caused by the constant build-up and release of strain in the Earth's crust.
"With a plate boundary like the San Andreas, you have the North American plate on one side and the Pacific plate on the other," explained Segall, a professor of geophysics. "The two plates are moving at a very steady rate with respect to one another, so strain is being put into the system at an essentially constant rate."
When an earthquake occurs on the fault, a certain amount of accumulated strain is released, added Murray, a geophysics graduate student.
"Following the quake, strain builds up again because of the continuous grinding of the tectonic plates," she noted. "According to the time-predictable model, if you know the size of the most recent earthquake and the rate of strain accumulation afterward, you should be able to forecast the time that the next event will happen simply by dividing the strain released by the strain-accumulation rate."
Although the model makes sense on paper, Murray and Segall wanted to put it to the test using long-term data collected from an ideal setting. Their choice was Parkfield -- a tiny town in Central California midway between San Francisco and Los Angeles.
Perched along the San Andreas Fault, Parkfield has been rocked by a magnitude 6 earthquake every 22 years on average since 1857. The last one struck in 1966, and geologists have been collecting earthquake data there ever since.
"Parkfield is a good place to test the model because we have measurements of surface ground motion during the 1966 earthquake and of the strain that's been accumulating ever since," Murray noted. "It's also located in a fairly simple part of the San Andreas system because it's on the main strand of the fault and doesn't have other parallel faults running nearby."
When Murray and Segall applied the time-predictable model to the Parkfield data, they came up with a forecast of when the next earthquake would occur.
"According to the model, a magnitude 6 earthquake should have taken place between 1973 and 1987 -- but it didn't," Murray said. "In fact, 15 years have gone by. Our results show, with 95 percent confidence, that it should definitely have happened before now, and it hasn't, so that shows that the model doesn't work -- at least in this location."
Could the time-predictable method work in other parts of the fault, including the densely populated metropolitan areas of Northern and Southern California? The researchers have their doubts.
"We used the model at Parkfield, where things are fairly simple," Murray observed, "but when you come to the Bay Area or Los Angeles, there are a lot more fault interactions there, so it's probably even less likely to work in those places."
Segall agreed: "I have to say, in my heart, I believe this model is too simplistic. It's really not likely to work elsewhere, either, but we still should test it at other sites. Lots of people do these kinds of calculations. What Jessica has done, however, is to be extremely careful. She really bent over backward to try to understand what the uncertainties of these kinds of calculations are -- consulting with our colleagues in the Stanford Statistics Department just to make sure that this was done as carefully and precisely as anybody knows how to do. So we feel quite confident that there's no way to fudge out of this by saying there are uncertainties in the data or in the method."
Use with caution
Segall pointed out that scientists in the United States and other Pacific Rim countries routinely use this technique for long-range hazard assessments.
"We're in a tough situation, because agencies like the USGS -- which has the responsibility for issuing forecasts so that city planners and builders can use the best available knowledge -- have to do the best they can with what information they have," Segall observed. "The message I would send to my geophysical colleagues about this model is, 'Use with caution.' "
Technological advances in earthquake science could make long-range forecasting a reality one day, added Murray, pointing to a recently launched San Andreas Fault drilling experiment in Parkfield under the aegis of USGS and Stanford.
"I always tell people to prepare," Segall concluded. "We know big earthquakes have happened in the past; we know they will happen again. We just don't know when."
Funding for the Nature study was provided by Stanford Graduate Fellowships and the USGS Earthquake Hazards Reduction Program.
By Mark Shwartz