WLF6 Session: Landslides in Subaerial and Subaqueous Volcanic Environments

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From: Lauren Schaefer <lauren.n.schaef@xxxxxxxxx>


Please consider submitting an abstract to the following session in the
6th World
Landslide Forum (WLF6)
<https://urldefense.com/v3/__https://wlf6.org/__;!!IKRxdwAv5BmarQ!Z0oNrUxaKY_OQIS61JPGQ1353BUFhfMO3A_7ArpqCicXhjgSTch_MdNHMFmjP-E0t94PHtdsgs7C8ERh6QtlVMxd$>,
to be hosted in Florence, Italy from 14-17 November 2023:

Landslides in Subaerial and Subaqueous Volcanic Environments
<https://urldefense.com/v3/__https://wlf6.org/forum-themes/*section-6322ba0-6__;Iw!!IKRxdwAv5BmarQ!Z0oNrUxaKY_OQIS61JPGQ1353BUFhfMO3A_7ArpqCicXhjgSTch_MdNHMFmjP-E0t94PHtdsgs7C8ERh6XEJgLL7$>
Onshore and subaqueous landslides in volcanic environments range from large
lateral collapses to shallow debris remobilizations, which vary from slow
and continuous to sudden and catastrophic. These events and their cascading
effects can extend to the volcano periphery, affecting areas and
populations far from the volcanic center. For example, rock or debris
avalanches and lahars can devastate vast areas, resulting in fatalities,
damage, and changes to the landscape and sudden flank failures in island,
coastal, or submarine volcanoes can generate tsunamis that can reach
coastal areas tens of kilometers away from the source. These large events
are low in frequency but high in intensity which make them difficult to
study and can result in significant local and regional hazards, often with
catastrophic consequences. In volcanic areas slope instability is
influenced by the complex interactions between tectonics, magmatic fluids,
meteorological conditions, material alteration, eruptive events, and
gravitational processes, leading to significant changes in flow rheology
along the slope and to complicated cascading processes which are
challenging to understand and predict. As a consequence, successful
strategies for landslide hazard assessments in volcanic environments need
to involve integrated methodologies for detection, mapping, monitoring, and
modelling that are able to capture their complex nature. This session
encourages multidisciplinary contributions that integrate onshore and
offshore investigations, field-based geological studies, geomorphological
mapping, volcanic rocks and deposits characterization, geophysical
investigations, remote sensing, and analytical, numerical and analogical
modelling to tackle the challenging and fascinating study of these
processes.

CONVENERS:
Federico Di Traglia, National Institute of Oceanography and Applied
Geophysics (OGS), Italy
Lorenzo Borselli, Universidad Autonoma de San Luis Potosi (UASLP),
Instituto de Geologia, Facultad De Ingenieria, Mexico
Irene Manzella, Department of Applied Earth Sciences (AES), Faculty of
Geo-Information Science and Earth Observation (ITC), University of Twente,
Netherland
Lauren N. Schaefer, Geologic Hazards Science Center, U.S. Geological
Survey, Colorado, USA
Morelia Urlaub, GEOMAR Helmholtz Centre for Ocean Research, Kiel, Germany

The abstract submission deadline is *28 February 2023*.


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