2008 National Seismic Hazard Maps-Fault parameters
New Search
Fault Name State
West Cache fault, Clarkston section Utah
GEOMETRY
Dip (degrees) 40/60/50
Dip direction E
Sense of slip normal
Rupture top (km) 0
Rupture bottom (km) 15
Rake (degrees) -90
Length (km) 23
MODEL VALUES
Probability of activity 1
Minimum magnitude 6.5
Maximum magnitude 6.66
b-value 0.8
Assigned Dip Fault-Parallel Slip Rate Width Annual Rate a-value Branch Weight
40 0.62 23.3 9.21e-04 2.046 0.2
50 0.52 19.6 6.48e-04 1.894 0.6
60 0.46 17.3 5.07e-04 1.787 0.2
Comments
This part of the West Cache fault was added in the 2007 maps. Preferred vertical slip rate is consensus value reported by Lund (2005) based on original investigation by Black and others (2000). Dip of fault changed to 50? based on redefined regional default value (Lund, 2006).
Selected References
Black, B.D., Giraud, R.E., and Mayes, B.H., 2000, Paleoseismic investigation of the Clarkston, Junction Hills, and Wellsville faults, West Cache fault zone, Cache County, Utah: Utah Geological Survey Special Study 98, 23 p., http://ugspub.nr.utah.gov/publications/special_studies/SS-98.pdf.
Lund, W.R., 2005, Consensus preferred recurrence interval and vertical slip rate estimates—Review of Utah paleoseismic-trenching data by the Utah Quaternary Fault Parameters Working Group: Utah Geological Survey Bulletin 134, compact disk.
Lund, W.R., ed., 2006, Basin and Range Province Earthquake Working Group seismic-hazard recommendations to the U.S. Geological Survey National Seismic Hazard Mapping Program: Utah Geological Survey Open-File Report 477, 23 p, ugspub.nr.utah.gov/publications/open_file_reports/OFR-477.pdf.