<?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>Evelyn Roeloffs</dc:contributor>
  <dc:contributor>Nick M. Beeler</dc:contributor>
  <dc:contributor>James E. Quick</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>Larry G. Mastin</dc:creator>
  <dc:date>2008</dc:date>
  <dc:description>During the ongoing eruption at Mount St. Helens, Washington, lava has extruded continuously at a rate that decreased 
from ~7-9 m&lt;sup&gt;3&lt;/sup&gt;
/s in October 2004 to 1-2 m&lt;sup&gt;3&lt;/sup&gt;
/s by December 
2005. The volume loss in the magma reservoir estimated from 
the geodetic data, 1.6-2.7×10
&lt;sup&gt;7&lt;/sup&gt;
 m3
, is only a few tens of percent 
of the 7.5×10
7
 m&lt;sup&gt;3&lt;/sup&gt;
 volume that had erupted by the end of 2005.</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.3133/pp175022</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>U.S. Geological Survey</dc:publisher>
  <dc:title>Constraints on the size, overpressure, and volatile content of the Mount St. Helens magma system from geodetic and dome-growth measurements during the 2004-2006+ eruption</dc:title>
  <dc:type>reports</dc:type>
</oai_dc:dc>