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east-central Idaho, and Red Rock fault, southwest Montana, during the late Quaternary: Boulder, University of Colorado, unpublished M.S. thesis, 141 p., 10 pls.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.
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