Poás Volcano: Impact of Rockslides

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Poás Volcano: Widespread rockslides triggered by 6.2 earthquake.
From: Eliecer Duarte <eduarte@xxxxxxxxx>
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Fieldwork was carried out yesterday (Feb. 11, 2009) to assess and
document impact of rockslides within and around Poás Volcano active
crater.
Hundreds of rockslides (all sizes) were drawn and explained in a field
report, one month after the Cinchona earthquake shook the summit and
surroundings. Previously unstable areas (subject to gravity) were the
most affected 360 degrees around the intracrater area. Many other
rockslides occurred along walls supposedly stable.

Although no augmented activity is related to massive falling of
material, eventually fine sediments will end up at the bottom of the
hot, acidic lake.
A previous unstable area, east and near the lake, fell almost
completely, burying a fumarolic axis that acted as a subaerial release
for some 9 years. It seems that the vigorous degassing activity
returned entirely to the dome and the hot lake. Hence the lake shows
heavy curtains of gas and vapor. Fumarolic activity from the dome
looks stronger and sustained, compared to recent years.

More details (Spanish) available in the field report, at:
http://www.ovsicori.una.ac.cr/informes_prensa/2009/deslizampoas12022009.pdf

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