VOLCANO: EGU 2016. NH3.2: Assessing runout and rheology of complex hazardous flow through numerical and experimental models

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EGU 2016. NH3.2: Assessing runout and rheology of complex hazardous flow through numerical and experimental models
From: "Irène Manzella" <Irene.Manzella@xxxxxxxx>
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Sorry for cross-posting.

We would like to draw your attention to the following session at the next EGU General Assembly (17–22 April 2016); abstract submission deadline 13th of January 2016.

We welcome the contribution of those of you interested.


NH3.2: Assessing runout and rheology of complex hazardous flow through numerical and experimental models


Rapid, massive geophysical gravitational flows such as lahars, debris flows and rock avalanches are among the most hazardous phenomena at mountains and volcanoes. Among all geophysical gravitational flow phenomena, these are the most lethal and destructive: they can travel for several kilometres along volcanoes and mountains slopes and valleys. Their speed usually exceeds 100 km/hr and their volume is greater than a million cubic metres. The large quantity of mass in movement can develop a considerable energy, greater than the one developed by an earthquake of magnitude 6. This enormous energy developed in a short time has tremendous power of destruction that can cause irreparable damage, changes in the landscape and a large number of fatalities, destroying entire villages and burying thousands of people.
At present time the mechanisms involved in these phenomena are still for most part unknown. Several theories have been put forward to explain their large travel distance but despite the big effort done internationally, no general agreement on a comprehensive rheological law has been yet achieved and many questions remain to be answered.
We invite contributions to this session from numerical and experimental modellers on studies of the rheological behaviour and on the propagation and emplacement of these types of movements. This can include development of new codes or improvement of existing ones, physical modelling, back-analysis and benchmark exercises on historic field event and/or laboratory experiments.

Conveners: Irene Manzella1, Marina Pirulli2, Giovanni Crosta3, Michel Jaboyedoff4

1University of Geneva, Department of Earth Sciences, irene.manzella@xxxxxxxx

2Politecnico di Torino, Department of Structural, Geotechnical and Building Engineering, Italy

3 Università degli studi di Milano Bicocca, Scienze Geologiche e Geotecnologie, Dept. of Earth and Environmental Sciences, Italy

4 University of Lausanne, Institute of Earth Sciences, Switzerland




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