Comments |
Assigned vertical slip rates based on combined displacement across basalt flow suggesting the displacement rate for the main strand of the fault is 0.30 mm/yr; the rate for the companion fault to the west is 0.16 mm/yr (Anderson and Christenson,1989). Dip of fault changed to 50? based on redefined regional default value (Lund, 2006). |
Selected References |
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. Anderson, R.E., and Christenson, G.E., 1989, Quaternary faults, folds, and selected volcanic features in the Cedar City 1° x 2° quadrangle, Utah: Utah Geological and Mineral Survey Miscellaneous Publication 89-6, 29 p., 1 pl., scale 1:250,000.
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