<?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>Charles R. Austin</dc:creator>
  <dc:date>1960</dc:date>
  <dc:description>New Jersey is fortunate to be situated in a region that is relatively stable, geologically. 
For this reason scientists believe, on the basis of the best scientific evidence available, that the 
chances of New Jersey experiencing a major earthquake are very small. The last major earthquake 
on the east coast occurred at Charleston, S. C., in 1886. Minor shocks have been felt in New Jersey, 
however, from time to time. Reports of dishes being rattled or even of plaster in buildings being 
cracked are not uncommon. These minor disturbances are generally restricted to relatively small 
areas.</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:language>en</dc:language>
  <dc:publisher>State of New Jersey, Dept. of Conservation and Economic Development, Division of Water Policy and Supply</dc:publisher>
  <dc:title>Earthquake fluctuations in wells in New Jersey</dc:title>
  <dc:type>reports</dc:type>
</oai_dc:dc>