<?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>T.A. Simpson</dc:contributor>
  <dc:creator>W.B. Hopkins</dc:creator>
  <dc:date>1960</dc:date>
  <dc:description>&lt;p&gt;&lt;span&gt;A recent paper by daCosta [1959] reported&amp;nbsp;&lt;/span&gt;&lt;span class="ScopusTermHighlight"&gt;water&lt;/span&gt;&lt;span&gt;‐level fluctuations caused by the&amp;nbsp;&lt;/span&gt;&lt;span class="ScopusTermHighlight"&gt;Montana&lt;/span&gt;&lt;span&gt;&amp;nbsp;&lt;/span&gt;&lt;span class="ScopusTermHighlight"&gt;earthquake&lt;/span&gt;&lt;span&gt;&amp;nbsp;of August 18, 1959, and mentioned the fluctuations registered&amp;nbsp;&lt;/span&gt;&lt;span class="ScopusTermHighlight"&gt;in&lt;/span&gt;&lt;span&gt;&amp;nbsp;three&amp;nbsp;&lt;/span&gt;&lt;span class="ScopusTermHighlight"&gt;mine&lt;/span&gt;&lt;span&gt;‐&lt;/span&gt;&lt;span class="ScopusTermHighlight"&gt;water&lt;/span&gt;&lt;span&gt;&amp;nbsp;&lt;/span&gt;&lt;span class="ScopusTermHighlight"&gt;pools&lt;/span&gt;&lt;span&gt;&amp;nbsp;of the Northern anthracite field&amp;nbsp;&lt;/span&gt;&lt;span class="ScopusTermHighlight"&gt;in&lt;/span&gt;&lt;span&gt;&amp;nbsp;northeastern&amp;nbsp;&lt;/span&gt;&lt;span class="ScopusTermHighlight"&gt;Pennsylvania&lt;/span&gt;&lt;span&gt;, ten miles north of Wilkes‐Barre. This paper will discuss the&amp;nbsp;&lt;/span&gt;&lt;span class="ScopusTermHighlight"&gt;water&lt;/span&gt;&lt;span&gt;‐level phenomena of these&amp;nbsp;&lt;/span&gt;&lt;span class="ScopusTermHighlight"&gt;pools&lt;/span&gt;&lt;span&gt;&amp;nbsp;&lt;/span&gt;&lt;span class="ScopusTermHighlight"&gt;in&lt;/span&gt;&lt;span&gt;&amp;nbsp;more detail. Most of the coal mines near Wilkes‐Barre are idle, and ground&amp;nbsp;&lt;/span&gt;&lt;span class="ScopusTermHighlight"&gt;water&lt;/span&gt;&lt;span&gt;&amp;nbsp;is forming extensive&amp;nbsp;&lt;/span&gt;&lt;span class="ScopusTermHighlight"&gt;mine&lt;/span&gt;&lt;span&gt;‐&lt;/span&gt;&lt;span class="ScopusTermHighlight"&gt;water&lt;/span&gt;&lt;span&gt;&amp;nbsp;&lt;/span&gt;&lt;span class="ScopusTermHighlight"&gt;pools&lt;/span&gt;&lt;span&gt;&amp;nbsp;&lt;/span&gt;&lt;span class="ScopusTermHighlight"&gt;in&lt;/span&gt;&lt;span&gt;&amp;nbsp;the underground&amp;nbsp;&lt;/span&gt;&lt;span class="ScopusTermHighlight"&gt;mine&lt;/span&gt;&lt;span&gt;&amp;nbsp;openings. Some of the&amp;nbsp;&lt;/span&gt;&lt;span class="ScopusTermHighlight"&gt;pools&lt;/span&gt;&lt;span&gt;&amp;nbsp;are interconnected by boreholes, tunnels, and other openings through the barrier pillars between adjacent mines.&lt;/span&gt;&lt;/p&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.1029/TR041i003p00435</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>American Geophysical Union</dc:publisher>
  <dc:title>Montana earthquakes noted in pennsylvania mine‐water pools</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>