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<title mode="escaped" type="text/html">Guagua Pichincha volcano - Ecuador</title>
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<modified>2006-03-21T19:21:18Z</modified>
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<link href="https://www.blogger.com/atom/15392548/112395711250932207" rel="service.edit" title="Evidence of a tilted volcanic conduit?" type="application/atom+xml"/>
<author>
<name>Darwin</name>
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<issued>2005-08-13T11:18:32-07:00</issued>
<modified>2005-08-13T18:36:21Z</modified>
<created>2005-08-13T18:18:32Z</created>
<link href="http://darkwing.uoregon.edu/~dvillago/guagua/2005/08/evidence-of-tilted-volcanic-conduit.html" rel="alternate" title="Evidence of a tilted volcanic conduit?" type="text/html"/>
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<title mode="escaped" type="text/html">Evidence of a tilted volcanic conduit?</title>
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<div xmlns="http://www.w3.org/1999/xhtml">This is my <a href="http://darkwing.uoregon.edu/~dvillago/guagua/pichincha.ppt">AGU 03 presentation</a> about the precursory seismicity of the 1999 eruption. Hypocenters of deep LP events (2-12 km depth) suggest that there is an inclined conduit that feeds a magma chamber located about 4 km depth beneath the caldera. Deep LP events were the first seismic signs of an eruption, preceding magmatic activity by ~2 years.</div>
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