vEGU21-GM9.11: Volcano Geomorphology and Society: From observations, monitoring, and modeling of tectonic and gravity driven processes to disaster risk reduction

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From: Alessandro Bonforte <alessandro.bonforte@xxxxxxx>


Dear colleagues,

We'd like to invite you to submit your abstract to the session: "Volcano
Geomorphology and Society: From observations, monitoring, and modeling of
tectonic and gravity-driven processes to disaster risk reduction" at
EGU2021.

https://meetingorganizer.copernicus.org/EGU21/session/40276
<https://meetingorganizer.copernicus.org/EGU21/session/40276?fbclid=IwAR0butS88yCI59BEfv7rjzVWSMlyGfTbw7eajcHxVS0bdxrPU-QS9ich4nQ>

The deadline for submitting abstracts is *January 13, 2021 at 13:00 CET*.

GM9.11 *EDI* *Volcano Geomorphology and Society: From observations,
monitoring, and modeling of tectonic and gravity driven processes to
disaster risk reduction*
Co-organized by GMPV9/NH2
Convener: Federico Di Traglia | Co-conveners: Rosanna Bonasia, Alessandro
Bonforte, Felix GrossECS, Irene Manzella Volcanic complexes are among the
worldâ??s most active geological systems. They represent tectonic and
geomorphological systems that are highly responsive to both exogenous
dynamics and endogenous forcing. While external (gravitational) processes
lead to a shift of material from steeper slopes to areas with lower
gradients (erosion and moderate to large-scale mass-wasting), magmatic and
tectonic activity can be either constructive (resulting in accumulation) or
destructive (triggering caldera collapses and/or flank collapses). Mass
reorganization and wasting in volcanic environments, both onshore and in
the subaqueous domain, comprises a wide spectrum of phenomena, from
widespread spreading and lateral collapse to shallow, localized debris
remobilization, which represent a major threat for communities and
infrastructure. In many cases, volcano slopes continue below sea level.
Those subaqueous volcano flanks are also affected by the building-up and
activity of the terrestrial volcano and can be prone to mass wasting. This
wide spectrum of phenomena can have an impact on local and regional
communities even far from the eruptive centres, directly or through
secondary and cascading events like tsunamis and floods. As these events
can rapidly evolve into disasters, the implementation of disaster risk
reduction (DRR) strategies is essential for reducing their impact on
communities and entire societies. Holistic analysis, monitoring, early
warning frameworks, and communication are paramount for increasing societal
awareness and preparedness for volcano-related hazards. These holistic
approaches include investigating geomorphological changes and tectonic
activity, the detection of which must integrate different methodologies for
mapping and monitoring â?? integrating field-based studies, geomorphological
mapping, remote sensing data, geophysical investigations, and/or numerical
modeling. Scientists and non-academic stakeholders working in the fields of
hazard mapping, modelling, monitoring, early warning, and hazard
communication are invited to present their recent advances in research and
engagement in dialogue with practitioners and decision-makers. We encourage
multi- and transdisciplinary contributions that integrate field studies,
geomorphological mapping, geophysical investigations, remote sensing, and
analytical, numerical, and analog modelling of geomorphological and
tectonic processes as well as their communication in volcanic areas.


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