November 21, 1999
Hidden Risk That Science Saw
Related Article
Why
Insurers Shrink From Earthquake Risk
By JUDITH BERCK
ORTLAND, Ore. -- This
wasn't supposed to be major earthquake country. Floods, landslides,
even the occasional volcanic eruption, perhaps. But there has not
been a major quake in the Pacific Northwest since European settlers
first arrived here, so few people in Oregon, Washington or British
Columbia ever worried about the ground shaking.
But scientists now believe that the potential makings of a giant
earthquake -- of 8 or 9 magnitude -- have been quietly building here.
Using new data from Global Positioning System satellites,
oceanographers from Oregon State University who were studying minute
movements in the earth's crust found to their surprise that the Juan
de Fuca Plate, a section under the Pacific Ocean, is moving northeast
and shoving under the North American mainland much faster than was
previously thought.
Worse, rather than passing smoothly, the two plates are snagged
somewhere, probably under the Coastal Range west of Portland, leading
to growing pressure that can be relieved only by an earthquake.
The affected region extends 750 miles, from British Columbia to
northern California, and inland to the Cascade Mountains east of
Portland and Seattle, where the same geological forces have created
active volcanoes.
Preliminary data shows that the Juan de Fuca Plate, once thought to
be almost motionless, may be moving 10 to 15 millimeters a year --
"about as fast as your fingernail grows," said Chris Goldfinger,
assistant professor of oceanography at Oregon State and a co-author of
a report presented at the Seismological Society of America meeting in
Seattle last May.
"This is very, very fast, geologically," he said. Because of the
motion, he added, "the North American plate is being compressed like a
spring."
When the spring finally breaks free of the snag, the region will
suffer a subduction-zone earthquake, a more potentially destructive
type than California usually experiences. Most quakes there occur
along faults where the ground moves laterally, and severe damage is
fairly localized. Subduction-zone quakes affect wider areas and can be
much stronger, like the 9.2-magnitude quake that struck Alaska in
1964.
The last major earthquake in the Cascade region occurred in 1700,
and the average interval between such quakes seems to be about 600
years, but could be less, Goldfinger said.
Other research has found that small crustal faults in the Portland
hills, thought to be inactive, may be able to produce significant
quakes.
Reactions to these alarming reports have varied from fatalism to
urgent concern. Demand for residential earthquake insurance has picked
up somewhat, though not explosively. And some homeowners, including
Portland's mayor, Vera Katz, have made alterations to their homes to
make them safer in a quake.
"A lot of our community is in a denial stage, yet they are
informed," Mayor Katz said. "One of the first questions I asked as
mayor was about the potential of an earthquake. There was a deadly
silence in the room."
Much of downtown Portland was built using methods and materials,
like brick and terra cotta, that often fare poorly in earthquakes. The
city government has begun a program to retrofit public buildings and
bridges and to improve emergency plans.
The state's urban building codes took little account of earthquake
risk until a moderate 5.6-magnitude temblor near Salem, the state
capital, did $30 million in damage in 1993. Since then, the codes have
been tightened somewhat, but they are still less strict than those in
coastal areas or in quake-prone California, and apply only to new
construction, not existing buildings. State officials say they need
more data from the latest studies before taking new action.
In recent years, the Oregon legislature has been reluctant to
appropriate money for seismic upgrades of the state's highways and
bridges or for new maps of earthquake hazard zones.
Without actual experience of a quake to go by, officials have
trouble deciding how much preparation is needed. "I'm so ambivalent
about this," Mayor Katz said. "If it's a very severe quake, I don't
know if we've planned far enough. I don't know if any community can
plan far enough."