Item talk:Q237072

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   "name": "Geodetic constraints on the 2014 M 6.0 South Napa earthquake",
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   "abstract": "On 24 August 2014, the\u00a0M\u00a06.0 South Napa earthquake shook much of the San Francisco Bay area, leading to significant damage in the Napa Valley. The earthquake occurred in the vicinity of the West Napa fault (122.313\u00b0\u00a0W, 38.22\u00b0\u00a0N, 11.3\u00a0km), a mapped structure located between the Rodger\u2019s Creek and Green Valley faults, with nearly pure right\u2010lateral strike\u2010slip motion (strike 157\u00b0, dip 77\u00b0, rake \u2013169\u00b0; http://comcat.cr.usgs.gov/earthquakes/eventpage/nc72282711#summary, last accessed December 2014) (Fig.\u00a01). The West Napa fault previously experienced an\u00a0M\u00a05 strike\u2010slip event in 2000 but otherwise exhibited no previous definitive evidence of historic earthquake rupture (Rodgers\u00a0et\u00a0al., 2008;\u00a0Wesling and Hanson, 2008).\u00a0Evans\u00a0et\u00a0al.\u00a0(2012)\u00a0found slip rates of \u223c9.5\u2009\u2009mm/yr along the West Napa fault, with most slip rate models for the Bay area placing higher slip rates and greater earthquake potential on the Rodger\u2019s Creek and Green Valley faults, respectively (e.g.,\u00a0Savage\u00a0et\u00a0al., 1999;\u00a0d\u2019Alessio\u00a0et\u00a0al., 2005;\u00a0Funning\u00a0et\u00a0al., 2007).",
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