<?xml version="1.0" encoding="ISO-8859-1"?><?xml-stylesheet type="text/xsl" href="/includes/cap_alert.xsl"?><cap:alert xmlns:cap="http://www.incident.com/cap/1.0"><identifier>DOI-USGS-HVO-2012-10-08T07:32:33-10:00</identifier>
<sender>HawaiianVolcanoObservatory@vulcan4.</sender>
<sent>2012-10-08 07:32:29</sent>
<status>Actual</status>
<msgType>Update</msgType>
<scope>Public</scope>
<references></references>
<info>
<category>Geo</category>
<event>Seismicity - Deformation - Gas emission</event>
<urgency>Unknown</urgency>
<severity>Minor</severity>
<certainty>Unlikely</certainty>
<effective>2012-10-08 07:32:29</effective>
<expires>2012-10-09 07:32:29</expires>
<senderName>Hawaiian Volcano Observatory</senderName>
<headline>Mauna Loa Monthly Update</headline>
<description>Mauna Loa is not inflating. Seismicity rates were low.

&lt;b&gt;Deformation:&lt;/b&gt; is occurring at slow rates, dominated by southeasterly motion of the southeast flank. If any inflation is occurring, it is at a very low rate. Upgrades of many Mauna Loa sites in late 2011 produced some apparent data offsets that will be corrected once a longer post-upgrade time series is available for analysis. 

&lt;b&gt;Seismicity:&lt;/b&gt; There was no unusual seismicity. HVO seismic networks detected 1 shallow event to the north and west of the summit, 4 shallow events within the upper southwest rift, 4 shallow event within the lower southwest rift, and 4 shallow events within the NW rift.

&lt;b&gt;Gas&lt;/b&gt;: No significant changes in SO2, CO2 were recorded by the Mokuaweoweo gas and temperature monitors during the month. Fumarole temperature, after 5 months of slow decline totaling about 4 degrees C, reached 71 degrees C. 
&lt;b&gt;Background:&lt;/b&gt; Re-inflation of Mauna Loa&#039;s shallow magma storage reservoirs started immediately following the most recent eruption in 1984, then turned to deflation for almost a decade. In mid-2002, inflation started again, just after a brief swarm of deep long-period (LP) earthquakes. A more intense swarm of several thousand deep Long Period (LP) earthquakes occurred in late 2004, immediately preceding a dramatic increase in inflation rate. Inflation slowed again in 2006, ceased altogether in late 2009, and resumed slowly in late 2010.

Rising gradually to more than 4 km above sea level, Mauna Loa is the largest volcano on our planet. Its long submarine flanks descend to the sea floor an additional 5 km, and the sea floor in turn is depressed by Mauna Loa&#039;s great mass another 8 km. This makes the volcano&#039;s summit about 17 km (56,000 ft) above its base! The enormous volcano covers half of the Island of Hawai`i and by itself amounts to about 85 percent of all the other Hawaiian Islands combined.

Mauna Loa is among Earth&#039;s most active volcanoes, having erupted 33 times since its first well-documented historical eruption in 1843. Its most recent eruption was in 1984.</description>
<web>http://hvo.wr.usgs.gov</web>
<contact>askHVO@usgs.gov</contact>
<parameter>Volcano Alert Level=NORMAL</parameter>
<parameter>Aviation Color Code=GREEN</parameter>
<area>
<areaDesc>Mauna Loa volcano Hawaii and Pacific Ocean HI 19.475 -155.608</areaDesc>
<geocode>CAVW=1302-02=</geocode>
</area>
</info></cap:alert>