<?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>John P. Mason</dc:contributor>
  <dc:creator>Kirk A. Miller</dc:creator>
  <dc:date>2000</dc:date>
  <dc:description>The water-surface profile and flood boundaries for the computed 100-year flood were determined for a part of the lower Salt River in Lincoln County, Wyoming. Channel cross-section data were provided by Lincoln County. Cross-section data for bridges and other structures were collected and compiled by the U.S. Geological Survey. Roughness coefficients ranged from 0.034 to 0.100. The 100-year flood was computed using standard methods, ranged from 5,170 to 4,120 cubic feet per second through the study reach, and was adjusted proportional to contributing drainage area. Water-surface elevations were determined by the standard step-backwater method. Flood boundaries were plotted on digital basemaps.</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.3133/ofr00201</dc:identifier>
  <dc:language>en</dc:language>
  <dc:title>Water-surface profile and flood boundaries for the computed 100-year flood, lower Salt River, Lincoln County, Wyoming</dc:title>
  <dc:type>reports</dc:type>
</oai_dc:dc>