Titlebook: Building Knowledge for Geohazard Assessment and Management in the Caucasus and other Orogenic Region; Fabio Luca Bonali,Federico Pasquaré

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Tectonic Control Over the Abuli Samsari Volcanic Ridge, Lesser Caucasus, Georgiaon of magma pathways; the definition of the expected moment magnitude for possible earthquakes; the assessment of orientation of the maximum horizontal stress from the Late Miocene to the present day. We have used these results to evaluate the current seismic and volcanic hazards affecting the Abuli

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Landslide and Mudflow Hazard Assessment in Georgiaower lines are prone to geohazards, that can trigger disasters and lead to widespread losses of life and property. Consequently, geohazard assessment is an important step towards the management and mitigation of adverse, natural events. In the present work, we introduce a set of new hazard maps for

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Continuous-time dynamical systems,he responses to seismic emergencies in the Caucasus region and the project – co – directed by the University of Milan-Bicocca and the Ivane Javakhishvili Tbilisi State University – about the geological risks at the Enguri hydroelectric plant. Win-win nature of the cooperation between Tbilisi and the Alliance.

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Discrete-time dynamical systems,politically in tension; moreover, geoscience can play a key role in preventing situations that may escalate into conflicts. This paper showcases the main results of the NATO-funded projects, both in terms of their scientific relevance and their geopolitical importance.

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https://doi.org/10.1007/3-540-27877-Xting normal faults during the orogeny. The main style of deformation within the pro-and retro-wedge is a series of fault-propagation and fault-bend folds, duplexes and structural wedges. Within the frontal part of the pro-and retro-wedge, a series of thrust-top basins developed.

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Structural Architecture of the Western Greater Caucasus Orogen: New Data from a Crustal-Scale Structting normal faults during the orogeny. The main style of deformation within the pro-and retro-wedge is a series of fault-propagation and fault-bend folds, duplexes and structural wedges. Within the frontal part of the pro-and retro-wedge, a series of thrust-top basins developed.