2008 National Seismic Hazard Maps-Fault parameters
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Fault Name State
Coquille anticline Oregon
GEOMETRY
Dip (degrees) 60
Dip direction SW
Sense of slip reverse
Rupture top (km) 0
Rupture bottom (km) 15
Rake (degrees) 90
Length (km) 29
MODEL VALUES
Probability of activity 1
Minimum magnitude 6.5
Maximum magnitude 6.78
b-value 0.8
Assigned Dip Fault-Parallel Slip Rate Width Annual Rate a-value
60 0.28 17.3 2.54e-04 1.623
Comments
Assigned vertical slip rate based on measured vertical offset of 18-20 m of the 80-ka Whisky Run marine terrace at Coquille Point (McInelly and Kelsey, 1990; Witter and others, 1997; and Witter, 1999).
Selected References
McInelly, G.W., and Kelsey, H.M., 1990, Late Quaternary tectonic deformation in the Cape Arago-Bandon region of coastal Oregon as deduced from wave-cut platforms: Journal of Geophysical Research, v. 95, no. B5, p. 6699-6713.
Witter, R.C., Kelsey, H.M., and Hemphill-Haley, E., 1997, A paleoseismic history of the south-central Cascadia subduction zone—Assessing earthquake recurrence intervals and upper-pl. deformation over the past 6600 years at the Coquille River Estuary, southern Oregon: Technical report to U.S. Geological Survey, under Contract 1434-HQ-97-GR-03036, 54 p.
Witter, R.C., 1999, Late Holocene paleoseismicity, tsunamis and relative sea-level changes along the south-central Cascadia subduction zone, southern Oregon: University of Oregon, unpublished Ph.D. dissertation, 178 p.