<?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.J. Schneider</dc:creator>
  <dc:date>1962</dc:date>
  <dc:description>&lt;p&gt;&lt;span&gt;Precise measurements of fluctuations of ground-water temperature based on monthly readings&amp;nbsp;&lt;/span&gt;&lt;span class="ScopusTermHighlight"&gt;in&lt;/span&gt;&lt;span&gt;&amp;nbsp;shallow&amp;nbsp;&lt;/span&gt;&lt;span class="ScopusTermHighlight"&gt;glacial&lt;/span&gt;&lt;span&gt;-outwash aquifers may be used to&amp;nbsp;&lt;/span&gt;&lt;span class="ScopusTermHighlight"&gt;study&lt;/span&gt;&lt;span&gt;&amp;nbsp;ground-water movement and recharge. An increase&amp;nbsp;&lt;/span&gt;&lt;span class="ScopusTermHighlight"&gt;in&lt;/span&gt;&lt;span&gt;&amp;nbsp;storage&amp;nbsp;&lt;/span&gt;&lt;span class="ScopusTermHighlight"&gt;in&lt;/span&gt;&lt;span&gt;&amp;nbsp;the shallow basin of Okabena Lake,&amp;nbsp;&lt;/span&gt;&lt;span class="ScopusTermHighlight"&gt;Worthington&lt;/span&gt;&lt;span&gt;,&amp;nbsp;&lt;/span&gt;&lt;span class="ScopusTermHighlight"&gt;Minnesota&lt;/span&gt;&lt;span&gt;, permits the water to cover a much larger area and probably increases the opportunity for infiltration of lake water into aquifers connected with the lake.&amp;nbsp;&lt;/span&gt;&lt;span class="ScopusTermHighlight"&gt;In&lt;/span&gt;&lt;span&gt;&amp;nbsp;a shallow artesian aquifer confined by relatively impervious&amp;nbsp;&lt;/span&gt;&lt;span class="ScopusTermHighlight"&gt;glacial&lt;/span&gt;&lt;span&gt;&amp;nbsp;till, water moves toward the land surface&amp;nbsp;&lt;/span&gt;&lt;span class="ScopusTermHighlight"&gt;in&lt;/span&gt;&lt;span&gt;&amp;nbsp;response to steep temperature gradients&amp;nbsp;&lt;/span&gt;&lt;span class="ScopusTermHighlight"&gt;in&lt;/span&gt;&lt;span&gt;&amp;nbsp;the winter, and cool water descends to the aquifer when the upward temperature gradient is lowered or eliminated.&amp;nbsp;&lt;/span&gt;&lt;span class="ScopusTermHighlight"&gt;Thermometry&lt;/span&gt;&lt;span&gt;&amp;nbsp;may also be used&amp;nbsp;&lt;/span&gt;&lt;span class="ScopusTermHighlight"&gt;in&lt;/span&gt;&lt;span&gt;&amp;nbsp;&lt;/span&gt;&lt;span class="ScopusTermHighlight"&gt;hydrogeologic&lt;/span&gt;&lt;span&gt;&amp;nbsp;&lt;/span&gt;&lt;span class="ScopusTermHighlight"&gt;studies&lt;/span&gt;&lt;span&gt;&amp;nbsp;of limestone terrane.&lt;/span&gt;&lt;/p&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.1130/0016-7606(1962)73[1305:UOTIHS]2.0.CO;2</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>Geological Society of America</dc:publisher>
  <dc:title>Use of thermometry in hydrogeologic studies of glacial deposits at Worthington, Minnesota</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>