2008 National Seismic Hazard Maps-Fault parameters
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Fault Name State
Wallowa fault Oregon
GEOMETRY
Dip (degrees) 50
Dip direction NE
Sense of slip normal
Rupture top (km) 0
Rupture bottom (km) 15
Rake (degrees) -90
Length (km) 53
MODEL VALUES
Probability of activity 1
Minimum magnitude 6.5
Maximum magnitude 7.08
b-value 0.8
Assigned Dip Fault-Parallel Slip Rate Width Annual Rate a-value
50 0.18 19.6 1.21e-04 1.155
Comments
Assigned slip rate based on a minimum offset of 2200 m of Miocene Columbia River basalts (Zollweg and Wood, 1993; and Wood, 1999). Dip of fault changed to 50? based on redefined regional default value (Lund, 2006).
Selected References
Wood, S.H., 1999, Quaternary faulting in southwest Idaho and adjacent Oregon, in Quaternary geology of the northern Quinn River and Alvord Valleys, southeastern Oregon: Friends of the Pleistocene field trip guide, September 24-26, 1999, Appendix 9, p. 1-5.
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.
Zollweg, J.E., and Wood, S.H., 1993, Faulting relationships, seismicity, design earthquakes, and peak ground accelerations at hydroelectric facilities in Hells Canyon of the Snake River, Idaho-Oregon: Report prepared for Idaho Power Company, 158 p., 3 pls.