Possible next Tsunami victim:
America’s West Coast
Posted Dec. 29,
2004
Courtesy the University of Oregon
and World Science staff
North America’s West Coast
could be the next victim of the next Tsunamis as severe as those that devastated
southeast Asia on Sunday, geologists say.
Such giant waves, spurred by
undersea earthquakes, have have happened repeatedly in the past off this coast,
according to a University of Oregon geoscientist. Native legends seem to confirm
this, he added.
“From northern California to
Vancouver, B.C., the Native American stories tell of battles between gods along
the coast, whales carried over the land and dropped, rivers becoming salty
during the flood, and canoes thrown into trees,” said Ray Weldon, who
researches and teaches about of geologic hazards at the university.
Geologists believe a tsunami
caused by a magnitude 9.0 earthquake occurred on Jan. 26, 1700. It wiped out
local tribal villages and causing damage as far away as Japan, which has written
records of the event.
Weldon said he hopes coastal
residents will be learn about the tsunami potential in light of the devastation
along the coasts of nine Asian nations on the Indian Ocean.
Weldon is leading a team of
scientists studying uplift – the gradual rise of the Earth’s surface –
along the coast. This helps predict the size of future earthquakes and tsunamis.
A comparison of modern uplift rates in the Pacific Northwest reveals many
similarities to the rates predicted by models of past earthquakes, like the one
of 1700, Weldon added.
The uplift reveals that a
subduction zone – an area on a planet's crust in which the edge of an oceanic
continental plate is being pushed beneath another plate – is accumulating
strain that can trigger a great earthquake, he said. Historically, such events
tend to occur, on the average, every 300 to 500 years.
Damage from an undersea
earthquake as large as the one that shook the Indian Ocean could span from
Northern California to Vancouver, B.C., Weldon said. He and his colleagues
estimate that the resulting tsunami would add to the damage in the low-lying
coastal part of the Pacific Northwest and extend beyond the region to as far
away as Japan.
There is a geological record of
the 1700 tusnami, according to Weldon. This includes widespread evidence of
submerged coastal estuaries (the wide mouths of rivers), marine fossils and sand
deposits carried by the tsunami far up coastal rivers, and drowned coastal
forests. Chemical dating and tree ring analysis established that most of these
forests were drowned in the winter of 1699–1700.
Weldon, who has lived in
Indonesia and has relatives in Thailand, said last weekend’s tragedy brings
home the need for coastal residents and tourists to learn about and take
precautions against tsunamis.
“For an earthquake as strong
as the one that hit southeast Asia, the shaking at the Oregon coast would last
for up to 90 seconds and be great enough to cause significant damage and loss of
life,” he said. “Most significantly, a tsunami will arrive at the coast as
soon as minutes following the shaking to within a half-hour.”
If
a major earthquake occurs off the coast it is crucial to move immediately to
higher ground, preferably at least 100 feet above sea level, Weldon said. He
warned against becoming “lulled into complacency” by small initial waves or
by the sight of the water withdrawing, as this can rapidly reverse – a feature
of the deceptive behavior of the ocean during subduction earthquakes.