Like some peace and quiet? You can find it where scientists listen for earthquakes.
On a remote hilltop west of Corvallis, John Nabelek unlocks a door into an underground bunker covered with bushes and blackberry vines. Inside, cold air bathes a rack of electronic gear fed by power cables that lie like snakes along the concrete walls. Ignoring a “Do Not Enter” sign, he opens another door, crosses a narrow airspace and enters an inner chamber through a third door.
Quiet. Not a sound.
If your ears could listen with the sensitivity of the instruments in this room, you would hear the planet tremble as tectonic plates grind against each other, continents rise and fall imperceptibly in tidal cycles and ocean waves crash on distant beaches. All the resulting vibrations — short- and long-wave from all parts of the compass, the Himalayas, the Caribbean, the Middle East, Alaska, the Cascadia Subduction Zone off the Oregon Coast — are picked up here as they pass through Western Oregon.
“Most of the noise we see in the data comes from ocean waves at the coast,” says Nabelek, a geophysicist in OSU’s College of Oceanic and Atmospheric Sciences. “We have to filter that out to detect seismic waves with the same or lower amplitude.” Other seismic monitoring stations have the same problem. West Coast surf is detectable in the middle of the country.
Moreover, the station itself is on the move. “Relative to North America, we are moving north at about two centimeters per year,” he adds. Data from the GPS receivers established here in 1996 conclusively showed that the Oregon Coast pivots around a point in northeastern Oregon.
Node on Global Network
The station near Corvallis is the Pacific Northwest’s primary listening post for the tremors beneath our feet. Nabelek, manages the facility, which was built in 1950 by the University of California. It is known as “COR” on the global seismographic network that is supported by the National Science Foundation, and in 1989, became one of a select group of stations managed by IRIS (Incorporated Research Institutions for Seismology), a non-profit scientific organization in Washington D.C.
Seismometers are exquisitely sensitive to local vibrations, even changes in atmospheric pressure, says Nabelek. So COR’s instruments are shielded in vacuum chambers that sit on concrete pillars extending deep into the soil beneath the bunker. To isolate the instruments from local traffic, each pillar is isolated from the bunker floor by a flexible membrane. The vacuum chambers sit loosely on each pillar, unattached. If the North American plate on which the station sits lurches, as it has done so many times in the past, “these instruments would go flying,” says Nabelek. A backup seismometer would continue to operate; it is bolted to its foundation.
COR is a study in contrasts. It contains the latest seismometer technology (purchased in 2010 with federal Stimulus Bill funds), but still sitting in the instrument room is one of the original devices that, says Nebelek, is too heavy to move. In 1950, seismic data were recorded on photographic paper, and the instrument chamber was essentially a darkroom. A technician had to renew the paper role daily. Black paint still covers the walls, but a bright fluorescent light has replaced the red bulb that originally hung from the ceiling.
In the past, a heavy, stationary object was at the heart of most seismometers. The instrument’s frame vibrated around the object, giving scientists a measure of seismic waves.
Not surprisingly, seismology has gone digital. Today’s instruments record vibrations by the electronic resistance they generate with an object that is relatively light. Known as “broadband” technology, they are sensitive to the full range of seismic wave frequencies. “Broadband seismometers changed everything,” says Nabelek. Technicians visit the station only when problems arise. Data are sent in real-time to the U.S. Geology Survey in Golden, Colorado, and automatically posted to the station’s website.
Despite it’s quiet surroundings, the station witnesses some of the most violent events on the planet. In the past few years, it has documented the planetary echoes of cataclysmic shaking in China, Indonesia, Haiti, Iran and Chile. Tremors show up just as clearly when faults closer to home slip, but one day soon, it will ring when the coiled spring of our own Cascadia Subduction Zone lets loose.
On the Web: You can see earthquake data as it is recorded here and transmitted in near real-time on a website, http://quakes.oce.orst.edu/COR/.
OSU is a member of the Pacific Northwest Seismic Network at the University of Washington.
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Robert Yeats has devoted his career to raising awareness about earthquake risks in the Pacific Northwest.
Learn about the Earthscope program, funded by the National Science Foundation and headquartered at Oregon State University.
Oregon State University scientists and engineers responded to the 2010 earthquake in Chile and a resulting tsunami.