<?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>Phillip R. Bowman</dc:contributor>
  <dc:creator>Jack E. Veenhuis</dc:creator>
  <dc:date>2002</dc:date>
  <dc:description>&lt;p&gt;In June 1977, the La Mesa&amp;nbsp;wildfire burned 15,270 acres in and&amp;nbsp;near Frijoles Canyon in Bandelier&amp;nbsp;National Monument (BNM) and the&amp;nbsp;adjacent Santa Fe National Forest,&amp;nbsp;New Mexico. In April 1996,&amp;nbsp;the Dome wildfire in BNM burned&amp;nbsp;16,516 acres in and near Capulin&amp;nbsp;Canyon&amp;nbsp;and the surrounding Dome&amp;nbsp;Wilderness area. Both Frijoles and&amp;nbsp;Capulin Canyon watersheds are characterized by archeological artifacts&amp;nbsp;that could be affected by increased&amp;nbsp;runoff and accelerated rates of&amp;nbsp;erosion, which typically occur after a&amp;nbsp;fire. In response to this concern, the&amp;nbsp;U.S. Geological Survey (USGS), in&amp;nbsp;cooperation with the National Park&amp;nbsp;Service, conducted a study to&amp;nbsp;monitor and document the wildfire&amp;nbsp;effects on streamflow after the 1996&amp;nbsp;Dome fire.&lt;/p&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.3133/fs14102</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>U.S. Geological Survey </dc:publisher>
  <dc:title>Effects of wildfire on the hydrology of Frijoles and Capulin canyons in and near Bandelier National Monument, New Mexico</dc:title>
  <dc:type>reports</dc:type>
</oai_dc:dc>