<?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>R.W. Harper</dc:contributor>
  <dc:contributor>H.G. Sisco</dc:contributor>
  <dc:creator>R.L. Whitehead</dc:creator>
  <dc:date>1985</dc:date>
  <dc:description>Significant hydrologic changes were observed after the magnitude 7.3 earthquake that occurred on October 28, 1983, in central Idaho. Groundwater levels rose by as much as 3 meters near the epicenter. Discharge in many streams and springs increased, in some instances by more than 100%. One warm spring ceased flowing for several days; the flow then resumed and peaked at about nine times its original rate. Available data show no significant changes in water quality following the earthquake. ?? 1985 Birkha??user Verlag.</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.1007/BF00874599</dc:identifier>
  <dc:language>en</dc:language>
  <dc:title>Hydrologic changes associated with the October 28, 1983, Idaho earthquake</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>