Comments |
The preferred vewrtical slip rate is based on scarps as high as 10 m (Love and Montagne, 1956) that formed on Bull Lake-equivalent glacial terrane (140 ka). Dip of fault changed to 50? based on redefined regional default value (Lund, 2006). |
Selected References |
Love, J.D., and Montagne, J.M., 1956, Pleistocene and recent tilting of Jackson Hole, Teton County, Wyoming: Wyoming Geological Association Guidebook, Eleventh Annual Field Conference, 169-178 p. 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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