Unraveling the San Gorgonio Knot, California: A Three-Dimensional Numerical Investigation of San Andreas Fault
Configuration through the San Gorgonio Pass
Laura Dair and Michele Cooke
University of Massachusetts – Geosciences Department Amherst, MA [email protected]
The San Andreas fault
poses significant earthquake hazards for the 24 million residents of southern California. While geologic evidence shows that the San Andreas
fault
in the San Gorgonio knot has complex, dipping and discontinuous
fault
strands, predictive earthquake models of this region have disregarded these complexities. We investigate alternative three-dimensional configurations of the San Andreas
fault
through the San Gorgonio Pass to show the influence of
fault
geometry on uplift patterns and slip rates. The different models include both a simplified vertical, continuous
fault
and a north-dipping discontinuous
fault
. The north-dipping model corresponds better to observations of recent uplift within the San Bernardino Mountains. The vertical
fault
configuration has greater net slip and more efficiently transmits deformation through the San Gorgonio Pass, but the north-dipping
fault
configuration may better match uplift patterns. There has been an ongoing debate over the slip partitioning between the Coachella Valley segment of the San Andreas and the San Jacinto
fault
. Our study indicates that the slip portioning between the two faults has less of an effect on the slip rates and deformation than
fault
geometry.












AAPG Search and Discovery Article #90070 © 2007 AAPG Foundation Grants in Aid