Oregon daily emerald. (Eugene, Or.) 1920-2012, October 07, 1991, Page 7, Image 7

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    QUAKE
Continued from Page 1
pared for a major quake.
"The perception is definitely
lagging behind the scientific
data," Weldon said. "People
are going to ho surprised by
this. In general, people are un
derestimating the hazard that
exists.”
Unfortunately, it is going to
take a sizable quake to hit the
Northwest before Oregonians
realize the hazard that exists,
Pezzopane said
These recently completed
maps have already appeared in
the autumn issue of the Univer
sity's Old Dragon magazine.
The maps will also be pub
lished in technical journals,
Pezzopane said.
By studying the history of
earthquakes, geologists have
found that large quakes re-oc
cur every 300 to 300 years in
this state, Pezzopane said, and
the last one to shako the area
occurred about 300 years ago.
"The coast will bo hit the
hardest because the subduction
zones would be closest to the
source of the biggest quake,” he
said.
Aitnougn uregon is clearly ai
risk from a major quake off the
coast — where an oceanic
crustal plate is sliding under
neath the North American con
tinental plate — fault lines that
radiate across the state also
pose a risk.
In the Cascades, the potential
hazards could come from vol
canic activity and crustal faults.
Closer to home, the Willamette
Valley could suffer consider
able damage because of loose
soil conditions. These condi
tions could amplify a quake's
vibration, increasing the risk to
Oregon's most populated areas.
"This could be a problem be
cause soft sediment amplifies
like Jell-O," l'ezzopane said.
The amount of damage done
to the LI u go no area from a
coastal earthquake depends
mostly on the magnitude, Wel
don said.
Weldon said an 8 on the
Richter scale could do some
■ high
IV moderate
□ low
LouM««y g'»p*'C
This map shows tho potential risk duo to strong ground shaking
from earthquakes associated with active faults near and within
Oregon. Roughly 80 percent of the Oregon population resides within
a high-risk area
dumugo and perhaps cause
deaths in particular situations,
such as construction workers
on ladders or workers in a
trench.
‘The perception is
definitely lagging
behind the
scientific data.
People are going to
be surprised by
this. In general,
people are
underes tima ting
the hazard that
exists.’
— Silvio Pezzopane,
Graduate Gudent
"If it is a 9, that is -to times
the energ\ release. Weldon
said. “That would cause signifi
cant damage and considerable
loss of life. However, we are
still f.ir enough away that it
would not cause total devasta
lion."
I'o/zopnnc said people
should prepare ihorusoKes and
their homes in the event that .i
quake should hit
"Kvervoue should place all
heavy objects on tin- flour, strap
down your water heater and
make sure your house is
strapped down to the founda
tion because some are not,"
Pezzopano said
in addition, l’ez/.opune said
everyone should prepare a sup
ply of food, water, flashlights
and first aid kits
' The conferences that I've
been going to .ill say that it will
be at least 72 hours that we'll
have to go without help from
anyone (directly following an
earthquake]," Pezzopane said
"And iiia! is the unnyntim ”
Pezzopane created his maps
on the computer, using Land
scape Architecture Professor
Dave Hulse's program, called
Geographical Information Svs
tum, The maps are only one ut
Pezzopurio's projects that he is
working on to complete his
doctorate.
"27 years of
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