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Chance of Hayward Fault Quake Downgraded, but Risk Still High
By USHA LEE MCFARLING, Times Science Writer
A stretch of Northern California's most dangerous fault--the
Hayward--running underneath densely populated portions of San Francisco's
East Bay is far less likely to spawn an earthquake than previously
thought, according to a new report being published in today's issue of
the journal Science.
The study shows that a 12-mile section of the fault running north from
Berkeley is creeping along steadily, thus avoiding the locking that can
build strain and lead to earthquakes. The finding was made using new
precision satellite data and recordings of barely perceptible microquakes
deep within the Earth.
While praising the study, earthquake experts were quick to warn that
the seismic hazard remains high in the area--because of quakes that could
originate on parts of the fault system to the south or north and on other
area faults.
"Folks should not be unbolting their water heaters," said Robert
Simpson, a geophysicist at the U.S. Geological Survey in Menlo Park who
has studied the fault for a decade.
"It's false to give the impression that the hazard is lower," added
David Schwartz, head of the San Francisco Bay Area Earthquake Hazards
Project for the survey.
The Hayward fault, a major branch of the San Andreas fault system,
runs for more than 60 miles through the densely populated East Bay from
Fremont through Hayward, Oakland and from goal post to goal post
underneath UC Berkeley's football stadium. It runs underneath freeways
and aqueducts and close to many Bay Area reservoirs, freeways and
hospitals.
Since the late '80s, the lesser known Hayward has overshadowed the
legendary San Andreas as a potential fault hazard: It is considered to be
the Bay Area fault most likely to rupture in a major quake in the next
three decades. A 1995 study suggested that the financial toll of a major
quake on the Hayward fault could be twice that of Northridge and that
thousands of people would be injured or killed. "The Kobe quake [in
Japan] is a preview of Hayward," Schwartz said.
While the fault's future is uncertain, its past is murky as well.
Geologists divide the fault into two portions: a northern stretch that
runs from the Oakland and Berkeley border past El Cerrito, and a southern
stretch running from Oakland to Fremont.
Historical records show that the southern portion of the fault
ruptured in 1868, in a quake that was known as "the big one" until the
1906 San Francisco quake. It was long thought that the northern part of
the fault had ruptured in a large 1836 earthquake.
Gold Rush Documents
But in the mid-1990s, enterprising seismologist Tousson Toppozada of
the California Division of Mines and Geology delved into scanty pre-Gold
Rush historical records and determined that newspaper reports of a quake
on the northern part of the fault in 1836 were wrong. There had been no
such quake.
That finding made the northern stretch of the Hayward seem even more
dangerous. If it hadn't ruptured in the recent past, the fault was
thought to be overdue for a big quake. So geologists began to study the
northern stretch of the fault in earnest.
To find out when the last big earthquake occurred there, a team of
paleoseismologists in 1997 carved a trench over the fault--on the second
fairway of El Cerrito's Mira Vista golf course. There, disturbed layers
of sand and earth confirmed that the fault had not seen an earthquake for
200 to 300 years.
That led to more scientific questions. Why hadn't it ruptured in so
long? And was it overdue for a dangerous quake?
That's what Roland Burgmann, the lead author of the current study and
a UC Berkeley geologist, hoped to find out. It was known that the surface
of the fault crept along at 5 millimeters per year. But such creeping
would only prevent earthquakes if it also occurred deep within the fault,
miles below the surface, where locking occurs.
Burgmann's team could only answer the questions using new technology.
They compared images of the fault taken from satellites in 1992 and in
1997 to measure how far the ground had moved.
The satellite technique is precise and able to measure small
differences in ground movement over a large area, said Eric Fielding, a
geophysicist at NASA's Jet Propulsion Laboratory who helped develop the
technology. Previously, geologists had to rely on a smattering of
painstakingly gathered individual readings of ground motion and did not
have enough observations to see the whole fault in context.
Burgmann also worked with geologists Robert Nadeau and Thomas McEvilly
at Lawrence Berkeley National Laboratory to measure clusters of nearly
imperceptible microquakes six miles underneath the surface. These little
quakes, which are recorded by seismometers at the surface even though
they cannot be felt by people, indicate that small patches of the fault
have slipped deep underground and can be used to infer how fast the earth
is creeping at those depths.
"It's like having a creep-meter at depth," said the geological
survey's Simpson, who was not involved in the study but said the new
technology provided "terrific new tools" for geologists.
Most Faults Do Not Slip So Easily
Putting all the data together, Burgmann found that the fault is
slipping at about the same rate underground as it is at the surface.
"However hard you push it, it will eventually respond by creeping.
There's no locking going on," he said. Most faults outside California do
not slip so freely. California faults may differ because of the state
rock, serpentine. Soft and easily fractured, the greenish rock may
lubricate faults, Burgmann said. The work adds to the knowledge about the
little understood process of creep and how it alters fault behavior.
The finding, in preliminary form, has already been used by geologists
who assess quake risks.
Such probabilities are determined by scientific committee, using a
mixture of history, science and instinct. They balance the strain caused
by the motion of the Earth's plates with the strain that has been
released by earthquake and by creep. They hone these estimates using
knowledge of historical quakes and theoretical knowledge of fault
behavior.
In October, when the most recent assessment was made, scientists used
the new report to downgrade the likelihood of a major quake on the
northern stretch of the Hayward fault within the next 30 years from 28%
to 16%. The risk for the entire fault system, including the Rodgers Creek
fault, which runs north through Napa County, is 32%--the highest in the
Bay Area.
The hazard on the northern section of the Hayward fault did not drop
to zero, because the area still could rupture from quakes that originate
on other parts of the fault system. "It ain't going to start the quake,
but you're sitting between two segments that can," Toppozada said of the
northern section of the fault.
In addition, shaking from distant parts of the fault could cause major
damage in Oakland and Berkeley. The Loma Prieta quake of 1989 severely
damaged the Bay Bridge, about 60 miles from the epicenter.
* * * ON THE INTERNET:
New radar images of fault:
http://www.jpl.nasa.gov/pictures/haywardfault/
Photo tour of fault:
http://www.mcs.csuhayward.edu/~shirschf/tour-1.html
Earthquake probabilities:
http://quake.wr.usgs.gov/study/wg99/
Search the archives of the Los Angeles Times for similar stories about:
Earthquakes - Northern California,
Seismology,
Earthquake Safety. You will not be charged to look for stories, only to retrieve one.
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