<?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>Henry Spall</dc:creator>
  <dc:date>1982</dc:date>
  <dc:description>&lt;p&gt;Earthquakes can be measured in terms of either the amount of energy they release (magnitude) or the degree of ground shaking they cause at a particular locality (intensity). &amp;nbsp;Although magnitude and intensity are basically different measures of an earthquake, they are frequently confused by the public and new reports of earthquakes. &amp;nbsp;Part of the confusion probably arises from the general similarity of scales used express these quantities. &amp;nbsp;The various magnitude scales represent logarithmic expressions of the energy released by an earthquake. &amp;nbsp;Magnitude is calculated from the record made by an earthquake on a calibrated seismograph. &amp;nbsp;There are no upper or lower limits to magnitude, although no measured earthquakes have exceeded magnitude 8.9.&lt;br&gt;&lt;/p&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:language>en</dc:language>
  <dc:publisher>U.S. Geological Survey</dc:publisher>
  <dc:title>Magnitude and intensity: Measures of earthquake size and severity</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>