
Finite element model calculated stress changes following the 1992 Landers earthquake, which may explain the triggering of the subsequent Hector Mine quake.
Earthquake Triggering
Previous Studies
Earthquake triggering is the process by which an earthquake on one fault can cause
an increase in stress on neighboring faults, resulting in earthquake sequences.
Understanding the manner in which faults communicate to each other through stress
changes can be used to identify regions of elevated seismic hazard (see our review
article on the subject:
Freed, Annual Reviews, 2005
).
Our group was the first to show that postseismic relaxation of a viscous mantle can induce
a time-dependent transfer stress that may explain the time-delay in earthquake sequences,
such as the triggering of the 1999 M7.1 Hector Mine earthquake following the 1992
Landers earthquake (
Freed and Lin, Nature, 2001
).
A similar study shows that diffusion of stress following these earthquakes is currently building
stress on faults close to the Los Angeles region (
Freed and Lin, Geology, 2004
).
Postseismic relaxation may explain the triggering of the 2002 M7.9 Denali earthquake
following the great 1964 M9.2 Alaska earthquake (
Ali and Freed, GJI, 2010
),
and may explain why seismic activity appears to toggle between the two major strike-slip
fault systems in Haiti (
Ali et al., GJI, 2008
). In a broad
study of southern California earthquakes over the past 200 years, we determined
that consideration of stress changes associated with postseismic relaxation is a
significant factor in the triggering of earthquakes (
Freed et al., GJI, 2007
).
Current Studies
With the finding that the 2010 Haitian earthquake occurred on the previously unmapped
Léogâne Fault, we are now addressed the question of what this means for the potential
of an earthquake to occur on the Enriquillo Fault that passes through the heavily
populated Port-au-Prince region. We are also working to understand a sequence of
earthquakes in the northern Baja region of Mexico, culminating in the 2010 El Major
earthquake. If we can interpret the stress communication between the faults that
has led to this sequence, we may better understand how these earthquakes have influences
faults within nearby southern California.