EGU 2008: EXPLOSIVE ACTIVITY AT BASALTIC VOLCANOES

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From: Jacopo Taddeucci <taddeucci@xxxxxxx>
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Dear Colleagues,

As the deadline for the 2008 EGU meeting approaches, we would like to
invite you to submit your contributions to the

EXPLOSIVE ACTIVITY AT BASALTIC VOLCANOES, GMPV23, session.

If you work on explosive eruptions, if mafic volcanoes are within your area
of interest, then this is your session.

Please find below a more complete description of the session.

Sincerely yours,

Jacopo Taddeucci and Oliver Spieler


Explosive eruptions of mafic to intermediate magmas possibly represent the
most frequent type of volcanic activity worldwide. Due t its specific
physic-chemical properties, mafic magmas produce specific eruptive
scenarios in respect to its more felsic counterpart, including the bursting
of gas slugs, multifarious explosive interaction external fluids, annular
gas flow, and fast foaming of volatile-saturated melt. From an
observational and monitoring point of view, basaltic explosive activity is
relatively accessible, and an important challenge for the future is how
multiparametric records from well-observed basaltic explosions may provide
a basis for volcanic explosion theories that apply also to less accessible
eruptions. Finally, from an hazard-related point of view, specific hazards
are associated with low-intensity basaltic activity, with harmful events
like the fallout of ballistic ejecta, paroxysmal explosions, and violent
magma-water interaction that often, and unexpectedly, punctuate relatively
harmless and prolonged low-level Strombolian and lava flow activity. Here
we propose an interdisciplinary session to cover the above (and possibly
other) aspects proper of explosive activity at basaltic volcanoes, with
particular emphasis to works that integrate different field, experimental,
and analytical approaches as well as novel technologies.

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