<?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>Cole G. Kingsbury</dc:contributor>
  <dc:contributor>Michael P. Poland</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>Jon J. Major</dc:creator>
  <dc:date>2008</dc:date>
  <dc:description>Oblique, terrestrial imagery from a single, fixed-position 
camera was used to estimate linear extrusion rates during 
sustained exogenous growth of the Mount St. Helens lava 
dome from November 2004 through December 2005. During 
that 14-month period, extrusion rates declined logarithmically 
from about 8-10 m/d to about 2 m/d. The overall ebbing of 
effusive output was punctuated, however, by episodes of fluctuating extrusion rates that varied on scales of days to weeks. 
The overall decline of effusive output and finer scale rate 
fluctuations correlated approximately with trends in seismicity 
and deformation. Those correlations portray an extrusion that 
underwent episodic, broad-scale stick-slip behavior superposed on the finer scale, smaller magnitude stick-slip behavior 
that has been hypothesized by other researchers to correlate 
with repetitive, nearly periodic shallow earthquakes.</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.3133/pp175012</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>U.S. Geological Survey</dc:publisher>
  <dc:title>Extrusion rate of the Mount St. Helens lava dome estimated from terrestrial imagery, November 2004-December 2005</dc:title>
  <dc:type>reports</dc:type>
</oai_dc:dc>