<?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>Marvin R. Couchman</dc:contributor>
  <dc:contributor>Seth C. Moran</dc:contributor>
  <dc:contributor>Andrew B. Lockhart</dc:contributor>
  <dc:contributor>Kelly J. Swinford</dc:contributor>
  <dc:contributor>Richard G. LaHusen</dc:contributor>
  <dc:contributor>David R. Sherrod</dc:contributor>
  <dc:contributor>William E. Scott</dc:contributor>
  <dc:contributor>Peter H. Stauffer</dc:contributor>
  <dc:creator>Patrick J. McChesney</dc:creator>
  <dc:date>2008</dc:date>
  <dc:description>The instruments in place at the start of volcanic unrest at 
Mount St. Helens in 2004 were inadequate to record the large 
earthquakes and monitor the explosions that occurred as the 
eruption developed. To remedy this, new instruments were 
deployed and the short-period seismic network was modified. 
A new method of establishing near-field seismic monitoring 
was developed, using remote deployment by helicopter. The 
remotely deployed seismic sensor was a piezoelectric accelerometer mounted on a surface-coupled platform. Remote 
deployment enabled placement of stations within 250 m of 
the active vent.</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.3133/pp17507</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>U.S. Geological Survey</dc:publisher>
  <dc:title>Seismic-monitoring changes and the remote deployment of seismic stations (seismic spider) at Mount St. Helens, 2004-2005</dc:title>
  <dc:type>reports</dc:type>
</oai_dc:dc>