Tall Plumes From Turrialba Volcano, Costa Rica

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From: Eliecer Duarte <eduarte@xxxxxxxxx>
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Observatorio Vulcanológico y Sismológico de Costa Rica.
OVSICORI-UNA

Turrialba Volcano: Tall gas and vapor columns correlate with
acute external changes.
(Fieldwork report, December 05, 2007)

An early alert was raised by media and neighbours of Turrialba volcano
at early hours of December 5th, 2007. A tall column ( taller than 2kms above the
summit) was observed from different areas in the Central Valley (Fig 1). Despite
several reports about the dark color of such column, it was determined that this
was due to an optical effect given the sunlight and the position of observers.
Color was white typical of an impulsive discharge of gases and vapor.
A team from OVSICORI-UNA conveyed to the area to confirm several
facts. Neighbours were preoccupied due to the vigorosity and height of the
plume. Nonetheless there was no ash or dust involved in the incident. An
abnormal output of gas along the south outer wall of the volcano was confirmed.
Several well defined fumaroles, located on the outer south wall, grow above the
summit rim provoking an acute effect on the perception of park rangers, settlers
and visitors (Fig 5).

Areas burned by acute acidification have extended in the last month. (Fig
2). Sectors towards the south and southeast show deep impact on
pasture, native and exotic trees. Birch patches along most drainages
have been completely
defoliated. The yellowish appearance of pasture land increases as the areas get
closer to the upper areas (Fig 4). Towards the southwest, effects on native
vegetation, pasture, and potato fields have extended dramatically to
lowerlands.(Fig 3).

A rapid inspection of changes intra caldera gives some elements that
correlate with the tall columns observed. Temperature of some fumaroles inside
crater W have reached 280ºC, some of them make a sharp noise of high pressure
valve. Melting native sulphur is still an undergoing process. Finally,
toward the
east of the caldera the decaying impact of acidification is evident
(Fig 6). Here
most species have died due to rapid burning occurring, even under rainy
conditions. It is to be expected greater effects in the coming months due to the
strengthening of trade winds and reduction of rain.

Details and photos can be found at:
http://www.ovsicori.una.ac.cr/pdf/2007/FieldreportTurri51207.pdf

or

http://www.ovsicori.una.ac.cr/vulcanologia/Volcan_Turrialba.htm#


Report and fieldwork: E. Duarte, E. Fernández, A. Tellez y Francois Robichaud.
(OVSICORI-UNA).

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