Geologists who hoped to study what happens before a quake, and in particular any signs that might enable them to predict future earthquakes, installed an elaborate array of seismometers and other instruments in and around Parkville starting in 1985.
As of mid-2002, the expected significant earthquake had not occurred. Researchers have been asking why not. A possible explanation for part of the delay is that earthquakes near Coalinga, California in 1983 reduced the stress on the Parkville section of the San Andreas fault. This stress reduction is estimated to have delayed the "next" Parkville quake by about ten years. Seismicity at Parkville increased in the late 1990s and early 2000s, suggesting that this section of the San Andreas fault may be returning to its previous cycle.
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