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Seismologist explains connection between deep tremors, earthquakes
UC Berkeley seismologists have detected a series of mysterious tremors on a section of the San Andreas Fault. These unusual vibrations, typically connected to volcanoes, occur deep below the earth’s surface.
Seismologist Robert Nadeau of UC Berkeley explained to KPCC’s Larry Mantle how these vibrations happen.
Robert Nadeau: “Down below where the earthquakes are, the deformation doesn’t cause earthquakes, but we can see its generating these tremors. Below the top 10 miles it’s rather brittle and will break as earthquakes, but down below is more ductile – a little bit like silly putty; probably embedded with harder pieces of rock. And when the lower part moves these rocks start to crack and generate these tremors, these long duration rumblings.”
Nadeau said data collected from the underground tremors helps scientists better analyze earthquake activity along the fault.