<?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>Patricia Lockridge</dc:creator>
  <dc:date>1985</dc:date>
  <dc:description>&lt;p&gt;Although tsunamis occur most often in the Pacific Ocean, they can be generated by major earthquakes in other areas.&amp;nbsp; The most frequent cause of tsunamis&amp;hellip;is crustal movement along a fault: a large mass of rock drops or rises and displaces the column of water above it.&amp;nbsp; This column of water &amp;ndash; a tsunami &amp;ndash; travels outward from the source at the fantastic speed of 500 mph or more.&amp;nbsp; When an earthquake occurs in the Pacific Ocean Basin, authorities must quickly decide on a course of action.&lt;/p&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:language>en</dc:language>
  <dc:publisher>U.S. Government Printing Office</dc:publisher>
  <dc:title>Tsunamis – Scourge of the Pacific</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>