<?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>C. D. Farrar</dc:contributor>
  <dc:contributor>D. L. Galloway</dc:contributor>
  <dc:contributor>S. N. Hamlin</dc:contributor>
  <dc:contributor>R. J. Laczniak</dc:contributor>
  <dc:contributor>E.A. Roeloffs</dc:contributor>
  <dc:contributor>M.L. Sorey</dc:contributor>
  <dc:contributor>D.E. Woodcock</dc:contributor>
  <dc:creator>E.G. Quilty</dc:creator>
  <dc:date>1995</dc:date>
  <dc:description>&lt;p&gt;This report compiles hydrologic observations in southern California associated with the 1994 Mw = 6.7 Northridge, California earthquake. In southern California, the largest ground water level change was a drop of 52 cm at Crystalaire. Most of the steplike water-level changes recorded following the Northridge earthquake agreed in direction with the sign of the calculated coseismic volume strain field. A spring discharge increase at Southern Pacific Springs was reported to have preceded the earthquake by several days. Outside of southern California, water-level changes were also observed, but are not consistent in sign or size with the static strain field of the earthquake sequence.&lt;/p&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.3133/ofr95813</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>U.S. Geological Survey</dc:publisher>
  <dc:title>Hydrologic effects associated with the January 17, 1994 Northridge, California, earthquake</dc:title>
  <dc:type>reports</dc:type>
</oai_dc:dc>