Tiny tremors and earthquakes provide intriguing clues about seismic activity

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The black line is the interface between the Philippine and Eurasian tectonic plates which gets deeper from right to left (towards the northwest). Black dots are conventional earthquakes and red dots are tiny low-frequency earthquakes (LFEs) which wer ...
The black line is the interface between the Philippine and Eurasian tectonic plates, which gets deeper from right to left (towards the northwest). Black dots are conventional earthquakes, and red dots are tiny low-frequency earthquakes (LFEs), which were found in the high fluid pressure/transient slip zone where silent earthquakes likely form. Mapping out the LFEs could enable scientists to locate silent slips and thus provide an early warning of a potential major rupture on the adjacent locked section of the plate interface. Credit: David Shelly, Stanford University

The elusive science of earthquake prediction has been reinvigorated in recent years with the discovery of "non-volcanic tremors"--faint vibrations that originate deep inside active fault zones. Since 2002, these mysterious signals have been recorded in seismically active sections of Japan, the Pacific Northwest and California's San Andreas Fault.


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