2008 National Seismic Hazard Maps-Fault parameters
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Fault Name State
Beaverhead fault Idaho
GEOMETRY
Dip (degrees) 40/60/50
Dip direction SW
Sense of slip normal
Rupture top (km) 0
Rupture bottom (km) 15
Rake (degrees) -90
Length (km) 134
MODEL VALUES
Probability of activity 1
Minimum magnitude 6.5
Maximum magnitude 7.00
b-value 0.8
Assigned Dip Fault-Parallel Slip Rate Width Annual Rate a-value Branch Weight
40 0.19 23.3 1.856 0.2
50 0.16 19.6 1.704 0.6
60 0.14 17.3 1.597 0.2
Comments
The preferred vertical slip rate is based on geomorphic studies of multiple-earthquake scarps on early Pinedale-equivalent (25-30 ka) surfaces on two of the central segments of the fault (Haller, 1988) that suggest an average of 0.12 mm/yr. Assigned characteristic magnitude based on Borah Peak earthquake. Dip of fault changed to 50? based on redefined regional default value (Lund, 2006).
Selected References
Haller, K.M., 1988, Segmentation of the Lemhi and Beaverhead faults, east-central Idaho, and Red Rock fault, southwest Montana, during the late Quaternary: Boulder, University of Colorado, unpublished M.S. thesis, 141 p., 10 pls.
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.