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A team of researchers from San Jose State University has determined that the San Andreas Fault is moving at a faster rate than geologists previously calculated. The findings challenge earlier assessments of the fault’s movement and have significant implications for understanding seismic risk in California.
Investigators involved in the study discussed their discovery and what the accelerated slippage means for earthquake preparedness and geological modeling. The research adds new data points to ongoing efforts to monitor one of North America’s most consequential fault lines.
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