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<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>Charles Avery</dc:creator>
  <dc:date>1986</dc:date>
  <dc:description>&lt;p&gt;This study is one of a series of studies appraising the waterbearing properties of the Navajo Sandstone and associated formations in southern Utah. &amp;nbsp;The stu&amp;lt;¥ area is al:x&amp;gt;dy area is about 4,600 square miles, extending from the Utah-Arizona State line northward to the San Juan-Grand County line and westward from the Utah-Colorado State line to the longitude of about 109°50'.&lt;/p&gt;&lt;p&gt;Some of the water-yielding formations are grouped into aquifer systems. The C aquifer is comprised of the DeChelly Sandstone Member of the Cutler Formation. &amp;nbsp;The P aquifer is comprised of the Cedar Mesa Member of the Cutler Formation and the undifferentiated Cutler Formation. The N aquifer is comprised of the sedimentary section that includes the Wingate Sandstone, Kayenta Formation, Navajo Sandstone, Carmel Formation, and Entrada sandstone. &amp;nbsp;The M aquifer is comprised of the Bluff Sandstone Member and other sandstone units of the Morrison Formation. &amp;nbsp;The D aquifer is comprised of the Burro Canyon Formation and Dakota Sandstone. &amp;nbsp;Discharge from the ground-water reservoir to the San Juan River between gaging stations at Four Corners and Mexican Hat is about 66 cubic feet per second.&lt;/p&gt;&lt;p&gt;The N aquifer is the main aquifer in the study area. Recharge by infiltration of precipitation is estimated to be 25,000 acre-feet per year. &amp;nbsp;A major ground-water divide exists under the broad area east of Monticello. &amp;nbsp;The thickness of the N aquifer, where the sedimentary section is fully preserved and saturated, generally is 750 to 1,250 feet. &amp;nbsp;&amp;nbsp;Hydraulic conductivity values obtained from aquifer tests range from 0.02 to 0.34 foot per day. &amp;nbsp;The total volume of water in transient storage is about 11 million acre-feet. Well discharge somewhat exceeded 2,340 acre-feet during 1981.&amp;nbsp; Discharge to the San Juan River from the N aquifer is estimated to be 6.9 cubic feet per second. Water quality ranges from a calcium bicarbonate to sodium chloride type water&lt;/p&gt;</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>Bedrock aquifers of eastern San Juan County, Utah</dc:title>
  <dc:type>reports</dc:type>
</oai_dc:dc>