2008 National Seismic Hazard Maps-Fault parameters
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Fault Name State
Centennial fault Montana
GEOMETRY
Dip (degrees) 50/40/60
Dip direction N
Sense of slip normal
Rupture top (km) 0
Rupture bottom (km) 15
Rake (degrees) -90
Length (km) 64
MODEL VALUES
Probability of activity 1
Minimum magnitude 6.5
Maximum magnitude 7.17
b-value 0.8
Assigned Dip Fault-Parallel Slip Rate Width Annual Rate a-value Branch Weight
40 1.40 23.3 9.81e-04 2.164 0.2
50 1.18 19.6 6.90e-04 2.011 0.6
60 1.04 17.3 5.40e-04 1.905 0.2
Comments
The preferred slip rate is based on long-term slip data reported by Sonderegger and others (1982), in which they indicate that the 2-Ma Huckleberry Ridge Tuff is offset 1.5-1.8 km. Dip of fault changed to 50? based on redefined regional default value (Lund, 2006).
Selected References
Witkind, I.J., 1975, Geology of a strip along the Centennial fault, southwestern Montana and adjacent Idaho: U.S. Geological Survey Miscellaneous Investigations Map I-890, 1 sheet, scale 1:62,500.
Sonderegger, J.L., Schofield, J.D., Berg, R.B., and Mannick, M.L., 1982, The upper Centennial Valley, Beaverhead and Madison Counties, Montana: Montana Bureau of Mines and Geology Memoir 50, 53 p., 4 pls.
Pierce, K.L., and Morgan, L.A., 1992, The track of the Yellowstone hot spot—Volcanism, faulting, and uplift, in Link, P.K., Kuntz, M.A., and Platt, L.B., eds., Regional geology of eastern Idaho and western Wyoming: Geological Society of America Memoir 179, p. 1-53, 1 pl.
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.