More on M8.2 Chile Earthquake - There were Foreshocks
Submitted by john on Tue, 04/01/2014 - 18:33
Defining the polygon below:
We can compute the change in probability with time for M>6 earthquakes within the polygon. There were clearly foreshocks, the computed probabilities increased dramatically prior to the event.
About OpenHazards Bloggers
Steven Ward is a Research Geophysicist at
the Institute of Geophysics and Planetary Physics, UC Santa Cruz. He specializes in the quantification and simulation of
natural hazards. Read Steve's blog.
John Rundle is a Distinguished Professor of Physics
and Geology at UC Davis and
the Executive Director of the APEC Collaboration for Earthquake Simulations. He
chaired the Board of Advisors for the Southern California Earthquake Center from 1994 to 1996. Read John's blog.
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