LAST REMINDER: IAVCEI 2008 Volcanic Sector Collapse (2-k)

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From: Benjamin van Wyk de Vries <B.vanwyk@xxxxxxxxxxxxxxxxxxxxxxx>
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LAST REMINDER IAVCEI Volcanic Sector Collapse

2-k  Volcanic sector collapse: Origin, transformation to debris flows
and tsunami

Last chance for all the submitters to IAVCEI, who may be late, to not
miss sending their abstracts to this session. *We are considering
organising a special issue to follow on from this session. *

Conveners:
B. van Wyk de Vries, Magma and Volcanoes Laboratory,
Clermont-Ferrand, b.vanwyk@xxxxxxxxxxxxxxxxxxxxxxx
A. M. Lagmay, National Institute of Geological Sciences,
Manilla, mlagmay@xxxxxxxxxxxxxxx
J. Clavero, SERNAGEOMIN, Santiago, jclavero@xxxxxxxxxxxxxx
L. Siebert, GVP, Smithsonian Institution, Washington, siebertl@xxxxxx


Sector collapse is common at all types of volcanoes and is a major hazard.
The origin and trigger of collapse is a growing field of study and more
field data and physical models are becoming available. Collapse
generally generates a rockslide-debris avalanche, which is also the
subject of intense field study and modelling. Such events are important
as they are highly destructive, and can spawn even more hazardous debris
flows and tsunamis. In this session we wish to integrate discussion on
studies starting before collapse origin, going though to the far- field
effects. A broad mix of research from field studies and laboratory
studies to modelling of collapse and associated effects is welcomed.

This session will focus on:
- The evidence: field and laboratory description of volcanoes, deposits
and their significance, failure mechanics and transport processes
- Volcano-tectonic interactions leading to slope failure
- The role of the magmatic and hydrothermal system in developing failure
- Mechanisms in the transformation from unstable slope to
rockslide-avalanche
- Mechanisms in the transformation from rockslide-avalanche to debris flow
- Rockslide-avalanche and tsunami relationships
- Numerical and analogue modelling of initiation, transport and
transformation

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