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The Log | School News

From Tiny Quakes, Major Insights into Earth

Peter Malin, a geology professor, is examining microearthquakes on Montserrat, Kenya’s Rift Valley and along California’s San Andreas fault

Duke University scientists are using waves from tiny earthquakes as geological equivalents of diagnostic X-rays. Emerging from the ground, the waves can reveal clues about the anatomy of a West Indian volcano.They can also help in finding geothermal steam in East Africa, and in zeroing-in on the epicenter of big earthquakes on the U.S. west coast.

The “microearthquakes” involved are so small that they may not even register on some sensitive instruments, the researchers said. Nevertheless they offer useful probes of the earth’s structure and geological processes because they occur much more frequently than do larger ones. They are also located at shallow enough depths for earthquake wave detectors called seismographs to be installed relatively nearby.

“We have these three major projects that are dovetailing together,” said Peter Malin, a geology professor at the Nicholas School. Malin’s seismology group is now carrying out microearthquake studies on the volcanic island of Montserrat, in the Rift Valley in Kenya and along the notorious San Andreas earthquake fault in California.

The true goal of all three efforts is basic science, Malin said in an interview. “Our group is trying to understand the relationship between stresses in Earth’s crust and the generation of these very small earthquakes,” he said.

In the process, the scientists gain a fringe benefit—information that is useful to society. The federal government, for example, has already committed more than $6 million through the National Science Foundation (NSF) to better understand the San Andreas fault, the locus of the great San Francisco earthquake as well as other big and damaging temblors.

The current focus of that project is a $1 million, 7,000-foot pilot drill hole near Parkfield, Calif. That is where Malin installed seismometers he helped design—rugged enough to endure 220 degree Fahrenheit temperatures and pressures of 300 atmospheres—that will help scientists decide where to finish drilling the San Andreas Fault Observatory at Depth (SAFOD).

In Montserrat, a tropical island located in the Caribbean southeast of Puerto Rico, the question is not when the volcano will erupt but rather for how long. The Soufriere Hills Volcano’s latest eruption began in 1995 and has since caused two-thirds of the population to flee.

This growing mountain continues to belch out not molten lava, but rather hot boulders that rumble down its slopes. By day, these big stones look dark like simmering coals, and by night they glow red. Even more perilous are the occasional explosions of hot gases that can rush across the hilly terrain faster than a car can drive. Such a “pyroclastic flow” killed a group of residents that attempted to farm land within the government-established danger zone.

“We’re trying to understand the volcano system better, giving the government the information they need to know which areas are dangerous to occupy and which are not,” said Elyan Shalev, a Duke research scientist in seismology. Towards that end, a NSF-supported scientific team that includes Shalev and Malin has lowered four different kinds of instruments down four different 600-foot drill holes. Duke’s contribution is a set of seismographs that might hint where molten magma is circulating underneath the summit.

The researchers’ third major project will take place in Kenya’s Rift Valley, where East Africa is splitting apart along a line of volcanoes. There, the geologists will use microearthquakes in attempts to track the location of underground fluids, in this case not hot magma but hot water. The goal is to determine where to drill for volcanically derived steam to fuel Kenya’s next geothermal electric power plant, which would be the country’s second.

— For the complete article by Monte Basgall of Duke News and Communications, go to http://www.dukenews.duke.edu/2003/06/microquakes.html

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