<?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>C.T. Sunsion</dc:contributor>
  <dc:contributor>G. W. Sandberg</dc:contributor>
  <dc:creator>L.J. Bjorklund</dc:creator>
  <dc:date>1978</dc:date>
  <dc:description>The Parowan-Cedar City drainage basin, Iron County, Utah, includes about 1,100 mi&lt;sup&gt;2&lt;/sup&gt; (square miles)(2,800 km&lt;sup&gt;2&lt;/sup&gt; [square kilometers])--520 mi&lt;sup&gt;2&lt;/sup&gt; (1,300 km&lt;sup&gt;2&lt;/sup&gt;) in the Parowan basin and 580 mi&lt;sup&gt;2&lt;/sup&gt; (1,500 km&lt;sup&gt;2&lt;/sup&gt;) in the Cedar City basin. Parowan and Cedar City Valleys are structural depressions formed by northeast-trending faults. Parowan Valley is essentially a closed basin, whereas Cedar City Valley is drained by two gaps in the mountains bordering the west side of the valley, and a small part of Cedar City Valley is drained at a gap at the south end. Water flowing into the basin from the highlands to the east is used to irrigate lands near Cedar City, Parowan, Paragonah, and Summit. The surface-water outflow from the basin is negligible.</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:language>en</dc:language>
  <dc:publisher>Utah Department of Natural Resources, Division of Water Rights</dc:publisher>
  <dc:title>Ground-water resources of the Parowan-Cedar City drainage basin, Iron County, Utah</dc:title>
  <dc:type>reports</dc:type>
</oai_dc:dc>