<?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:creator>R. W. Mower</dc:creator>
  <dc:date>1963</dc:date>
  <dc:description>&lt;p&gt;Ground water occurs in a shallow (unconfined) aquifer and in at least two artesian (confined) aquifers in the unconsolidated alluvial material composing the valley fill near Sugarville, Utah. No wells are known to withdraw water from the unconfined aquifer, and this report is limited to a discussion of the effects of pumping a well tapping one artesian aquifer on the piezometric surfaces of the water in both artesian aquifers.&lt;/p&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:language>en</dc:language>
  <dc:publisher>Utah State Engineer's Office</dc:publisher>
  <dc:title>Effects on the shallow artesian aquifer of withdrawing water from the deep artesian aquifer near Sugarville, Millard County, Utah</dc:title>
  <dc:type>reports</dc:type>
</oai_dc:dc>