Old Earthquake Faults are Like Worn Brake Pads

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Old Earthquake Faults are Like Worn Brake Pads

Earthquake faults are worn smooth over time by friction, like the brake pads of an old car, according to a new study.

The finding, detailed in the March issue of the journal Geology, suggests old and new faults might generate different types of earthquakes.

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Over the course of two years, the researchers analyzed about 15 sites in southern California, Oregon, Nevada and Utah. The findings support the idea that old and young faults have fundamentally different structures and that faults evolve over time.

The study found that while mature faults tend to be smooth at small scales, they have regular features on larger scales. In contrast, younger faults tend to be rough on all scales with no discernable pattern.

“The thing that was really surprising was that the mature faults have a really distinct structure, little hills on them, at the 10-meter scale,” said study team member Emily Brodsky, a University of California, Santa Cruz geologist.

This is surprising because most geologists thought fault lines are fractal, meaning they exhibit the same structure and complexity regardless of the scale of observation.

The researchers say the next step is to figure out what implications their findings have for earthquakes. Because old and new faults are so different, everything about the earthquakes they generate—their birth, strength and propagation—could be different as well, the researchers speculate.

“We don’t know how the amount of shaking from the same size earthquake acts on different kinds of faults,” Brodsky said. “It could be that the smoother, mature faults give you a less bumpy ride.”