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FVAG01 SABM 120100 VA ADVISORY DTG: 20100312/0100Z VAAC: BUENOS AIRES VOLCANO: VILLARRICA 1507-12 PSN: S3925 W07156 AREA:CHILE SUMMIT ELEVATION: 2947M ADVISORY NUMBER: 2010/001 INFORMATION SOURCE: WEBCAM DGAC ERUPTION DETAILS: N/A OBS ASH DATE/TIME: 12/0020Z OBS ASH CLOUD: VA NOT IDENTIFIABLE FROM SATELLITE DATA FCST ASH CLD +06HR: 120700Z FCST ASH CLD +12HR: 121300Z FCST ASH CLD +18HR: 121900Z REMARKS: VA CLOUD NOT IDENTIFIABLE FROM SATELLITE DATA HOWEVER WEBCAM SHOWS A THIN PLUME OF GAS/ASH EXTENDED NEAR TO THE SUMMIT NEXT ADVISORY: NO FURTHER ADVISORIES. FURTHER INFORMATION WILL BE ISSUED IF ANY ASH CLOUD IS DETECTED/OBSERVED
SERNAGEOMIN reported that on 4 March seismicity from Llaima increased. During an overflight that same day, scientists observed emissions of gas and steam from the main crater. Images taken that day were compared to those taken on 21 February and showed no significant changes in morphology. The rate of sulfur dioxide emissions had increased, however. Scientists also noted deposits from a large rockfall along with fracturing of the glacier, especially on the upper N and NW flanks. Those observations in addition to the increased seismicity prompted SERNAGEOMIN to raise the Alert Level to Yellow, Level 4.
Mount St. Helens ’spiders’ will get tryout on Chilean volcano (The Oregonian) – Geological ’spiders’ packed with instruments to monitor the heaves, sighs and belches of Mount St. Helens, are expected to migrate south this month. Two of the contraptions are headed to Chaiten, a volcano in Chile that began erupting in 2008 after about 9,000 years of dormancy. … The machines helped give the USGS sufficient information to declare in January 2008 that Mount St. Helens recent eruptive phase was over. That kind of certainty is needed at Chaiten, said John Ewert, a volcanologist in the Volcano Disaster Assistance Program. “It’s always hard enough to know when they’ll start erupting,” said Ewert, part of the team that visited the Chilean volcano in January. “It’s even harder to tell when they’ll stop.”‘
Originally posted by PuterMan
Whilst wilfing around the volcano blogs I came across this:
Mount St. Helens ’spiders’ will get tryout on Chilean volcano (The Oregonian) – Geological ’spiders’ packed with instruments to monitor the heaves, sighs and belches of Mount St. Helens, are expected to migrate south this month. Two of the contraptions are headed to Chaiten, a volcano in Chile that began erupting in 2008 after about 9,000 years of dormancy. … The machines helped give the USGS sufficient information to declare in January 2008 that Mount St. Helens recent eruptive phase was over. That kind of certainty is needed at Chaiten, said John Ewert, a volcanologist in the Volcano Disaster Assistance Program. “It’s always hard enough to know when they’ll start erupting,” said Ewert, part of the team that visited the Chilean volcano in January. “It’s even harder to tell when they’ll stop.”‘
This is the source page
During the last 10,000 years Shasta has erupted an average of every 800 years but in the past 4,500 years the volcano has erupted an average of every 600 years. The last significant eruption on Shasta may have occurred 200 years ago
Soufrière Hills: major dome collapse, resulting ash plume reaches 15.2 km altitude
Eyjafjallajökull volcano in southern Iceland has erupted after an extended period of seismic restlessness. The volcano began to erupt around midnight local time 20/21 March 2010. Civil protection authorities report that no-one is in immediate danger, but between 500 and 600 people have been evacuated from their homes. Pictures and reports indicate fissure eruption. Lava flows and ashfall have been reported and roads have been closed. University of Iceland geologist Tumi Gudumundsson is quoted by ABC News as saying that the eruption is located beneath an ice-free portion of the volcano, lessening the chances of a glacial flood being caused by melted ice. This could change, however, as the eruption develops.
Eyjafjöll (also known as Eyjafjallajökull) is located immediately west of Katla volcano. Eyjafjöll consists of an E-W-trending, elongated ice-covered basaltic-andesite stratovolcano with a 2.5-km-wide summit caldera. Fissure-fed lava flows occur on both the eastern and western flanks of the volcano, but are more prominent on the western side. Although the 1666-m-high volcano has erupted during historical time, it has been less active than other volcanoes of Iceland's eastern volcanic zone, and relatively few Holocene lava flows are known. The sole historical eruption of Eyjafjöll, during December 1821 to January 1823, produced intermediate-to-silicic tephra from the central caldera.
I translated the Sernageomin link to swedish, and as I understand it they had detected the EQs from the Chaiten seismic network. Interestingly the origin of the earthquakes actually wasn´t from Chaiten but instead from the Melimoyu volcano! It is probably a nearby volcano. They also write that they are making an expedition right now to put up a seismic station at Melimoyu.
Melimoyu is a stratowolcano with a 8 km wide icecovered caldera. And guess what.... It hasn´t erupted since 200AD!