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.
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