Project Abstract 
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        To better understand the likely rupture paths and slip distribution in future earthquakes on the southern San Andreas fault, additional slip rate measurements are needed from the Mission-Mill Creek, Banning and Garnet Hill strands of the San Andreas fault in northern Coachella Valley.  Work is in progress at a new slip rate site on the Banning fault, where an ancient channel wall of Mission Creek has been offset 148 ± 9 m by the Banning fault.  During 2015, after a lengthy permitting process, permission was obtained to excavate dating pits, and three pits were excavated at the site in January 2016.  Two 2-m deep pits were excavated on the old fan surface into which Mission Creek incised, and one 1.5-m deep pit was excavated into the alluvial deposits that post-date the incision, but that have been offset out of the path of the modern channel.  Twelve samples for optically stimulated luminescence dating were collected by Dr. Lewis Owen (4 samples from each pit), as well as seven samples from each of the two deeper pits for Be-10 depth profiles. These are being processed at the Geochronology Laboratories at the University of Cincinnati under the direction of Lewis Owen. Twelve charcoal samples were also collected for radiocarbon dating.  Processing of these samples has begun, and dates are expected before the end of 2016.  The dates will constrain the age of incision of the offset channel wall, which can then be used to estimate the slip rate for this part of the Banning fault.     |