<?xml version='1.0' encoding='utf-8'?>
<oai_dc:dc xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:oai_dc="http://www.openarchives.org/OAI/2.0/oai_dc/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:schemaLocation="http://www.openarchives.org/OAI/2.0/oai_dc/ http://www.openarchives.org/OAI/2.0/oai_dc.xsd">
  <dc:contributor>Timothy E. Dawson</dc:contributor>
  <dc:contributor>Rebecca Flowers</dc:contributor>
  <dc:contributor>John C. Hamilton</dc:contributor>
  <dc:contributor>Gordon F. Heingartner</dc:contributor>
  <dc:contributor>James Kessler</dc:contributor>
  <dc:contributor>Laura Samrad</dc:contributor>
  <dc:creator>Thomas E. Fumal</dc:creator>
  <dc:date>2004</dc:date>
  <dc:description>&lt;p&gt;We present photomosaics and logs of the walls of trenches excavated for a paleoseismic study at Mill Canyon, one of two sites along the San Andreas fault in the Santa Cruz Mtns. on the Kelley-Thompson Ranch. This site was a part of Rancho Salsipuedes beginning in 1834. It was purchased by the present owner’s family in 1851. Remnants of a cabin/mill operations still exist up the canyon dating from 1908 when the area was logged. At this location, faulting has moved a shutter ridge across the mouth of Mill Canyon ponding Holocene sediment. Recent faulting is confined to a narrow zone near the break in slope.&lt;/p&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.3133/ofr03469</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>U.S. Geological Survey</dc:publisher>
  <dc:title>Photomosaics and logs of trenches on the San Andreas Fault at Mill Canyon near Watsonville, California</dc:title>
  <dc:type>reports</dc:type>
</oai_dc:dc>