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Discover the 2010 Fault Activity Map of California including detailed fault intersections and earthquake ruptures. Explore the dynamic validation workshop and fault models for a comprehensive understanding of fault interactions.
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Fault Intersections in Map View (and more) Tim Dawson California Geological Survey SCEC Dynamic Code Validation Workshop Pomona, CA February 25, 2011
2010 Fault Activity Map of California • Updated version of 1975 and 1994 maps by Jennings • Compiled at original resolution of source maps • Companion digital database (GIS data) available as the USGS Q-faults compilation
2010 Fault Activity Map of California Also viewable on Google Maps interface on CGS website: http://www.quake.ca.gov/gmaps/GMC/stategeologicmap.html or Google:
Some Examples from California San Andreas - San Jacinto – Cucamunga fault intersection
Some Examples from California San Jacinto fault: Anza/Clark – Coyote Creek stepover
Some Examples from California San Andreas – Garlock fault intersection
Some Examples from California 1992 Landers rupture and Pinto Mountain fault
Some Examples from California 1999 Hector Mine: Complex rupture at fault intersection
2002 Denali Earthquake 2002 Denali earthquake: “Simple” fault intersection
Denali-Totschunda Intersection 45 Sun Angle 0 1 km Open Topography Schwartz and others, in prep
Denali-Totschunda Intersection 45 Sun Angle Initiation of fault separation Eastern Denali BRANCH POINT 0 500 m Totschunda Open Topography
Combined Geology – Relocated Seismicity Jim Lienkaemper, USGS
Hosgri – Shoreline fault intersection PG&E, 2010
1999 Izmit Rupture, North Anatolia fault 1967 Murdunu Valley earthquake
Integrated Geology, Geophysics, Seismicity Hayward – Calaveras Intersection Model USGS (GUMP)
Integrated Geology, Geophysics, Seismicity Hayward – Calaveras Intersection Model USGS (GUMP)
Gravel Hills – Harper Lake – Calico faults Some Examples from California Blackwater fault Gravel Hills – Harper Lake Camp Rock fault Calico fault
Take Home Points: • Fault intersections at the surface are both simple and complex, both as mapped traces and in earthquake ruptures • How do changes in fault orientation effect the ability of ruptures to propagate? Do dynamic rupture models fit the observations? • Surface mapping is only one part of the story: Integration of geology, geophysics, and seismicity helps to define the 3-D geometry of fault intersections • Our current fault models are over-simplified, however we have very few constraints on the actually geometry for most faults.