<?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>D. O. Gregg</dc:creator>
  <dc:date>1966</dc:date>
  <dc:description>&lt;p&gt;&lt;span&gt;The tidal efficiencies of wells tapping the principal artesian aquifer&amp;nbsp;&lt;/span&gt;in&lt;span&gt;&amp;nbsp;&lt;/span&gt;Glynn&lt;span&gt;&amp;nbsp;&lt;/span&gt;County&lt;span&gt;,&amp;nbsp;&lt;/span&gt;Georgia&lt;span&gt;&amp;nbsp;decrease with distance from the influencing tidal body and also decrease with well depth. Although the magnitude of&amp;nbsp;&lt;/span&gt;water&lt;span&gt;‐level&amp;nbsp;&lt;/span&gt;fluctuation&lt;span&gt;&amp;nbsp;of these wells is largely dependent upon the distance to a large tidal body, the time of a high or a low&amp;nbsp;&lt;/span&gt;water&lt;span&gt;&amp;nbsp;level&amp;nbsp;&lt;/span&gt;in&lt;span&gt;&amp;nbsp;the wells is mainly dependent upon the time of a high or a low&amp;nbsp;&lt;/span&gt;tide&lt;span&gt;&amp;nbsp;&lt;/span&gt;in&lt;span&gt;&amp;nbsp;a small, nearby tidal body. A modified formula for computing tidal efficiency is developed: (Formula Presented.) From this formula, tidal efficiency can be calculated rapidly and easily.&amp;nbsp;&lt;/span&gt;&lt;/p&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.1111/j.1745-6584.1966.tb01603.x</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>Wiley Blackwell</dc:publisher>
  <dc:title>An analysis of ground‐water fluctuations caused by ocean tides in Glynn County, Georgia</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>