2008 National Seismic Hazard Maps-Fault parameters
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Fault Name State
Morgan fault Utah
GEOMETRY
Dip (degrees) 50/60/40
Dip direction W
Sense of slip normal
Rupture top (km) 0
Rupture bottom (km) 15
Rake (degrees) -90
Length (km) 17
MODEL VALUES
Probability of activity 1
Minimum magnitude 6.5
Maximum magnitude 6.52
b-value 0.8
Assigned Dip Fault-Parallel Slip Rate Width Annual Rate a-value Branch Weight
40 0.03 23.3 5.59e-05 0.970 0.2
50 0.03 19.6 3.93e-05 0.818 0.6
60 0.02 17.3 3.08e-05 0.711 0.2
Comments
Preferred vertical slip rate is consensus value reported by Lund (2005) based on original investigations by Sullivan and others (1988) and Sullivan and Nelson (1992). Dip of fault changed to 50? based on redefined regional default value (Lund, 2006).
Selected References
Sullivan, J.T., Nelson, A.R., LaForge, R.C., Wood, C.K., and Hansen, R.A., 1988, Central Utah regional seismotectonic study for USBR dams in the Wasatch Mountains: Bureau of Reclamation Seismotectonic Report 88-5, 269 p.
Sullivan, J.T., and Nelson, A.R., 1992, Late Quaternary displacement on the Morgan fault, a back valley fault in the Wasatch Range of northeastern Utah, in Gori, P.L., and Hays, W.W., eds., Assessment of regional earthquake hazards and risk along the Wasatch front, Utah: U.S. Geological Survey Professional Paper 1500, p. I1-I19.
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.