Cascadia quake simulations

The slow slip and tremor events in Cascadia are also being studied by Stanford geophysics Professor Paul Segall, although in an entirely different manner. Segall's group uses computational models of the region to determine whether the cumulative effects of many small events can trigger a major earthquake.

"You have these small events every 15 months or so, and a magnitude 9 earthquake every 500 years. We need to known whether you want to raise an alert every time one of these small events happens," Segall said. "We're doing sophisticated numerical calculations to simulate these slow events and see whether they do relate to big earthquakes over time. What our calculations have shown is that ultimately these slow events do evolve into the ultimate fast event, and it does this on a pretty short time scale."

One thing that makes Segall's work difficult is a lack of data from actual earthquakes in the Cascadia region. Earlier this year, however, earthquakes in Mexico and Costa Rica occurred in areas that experience slow slip events similar to those in Cascadia. Segall plans to speak with geophysicists who have studied the lead-up to those earthquakes to compare the data to his simulations.

[link to news.stanford.edu]