Deep-seated Gravitational Slope Deformations (DGSDs) are not considered hazardous phenomena, because they evolve very slowly. However, they must not be neglected when defining slope instability in a territory, and the related hazard implications. Despite their slow deformation rates, DGSDs may cause damage to surface and underground (e.g., tunnels) structures. In addition, the may evolve into faster mass movements, or favour collateral landslide processes.

Deep-seated gravitational slope deformations (DGSDs) are not considered hazardous phenomena because they evolve very slowly. However, they must not be neglected when defining slope instability in a territory and the related hazard implications. Despite their slow deformation rates, DGSDs may cause damage to surface and underground (e.g., tunnels) structures. In addition, they may evolve into faster mass movements or favor collateral landslide processes.

Deep-seated gravitational slope deformation / Soldati, M.. - STAMPA. - (2013), pp. 151-155. [10.1007/978-1-4020-4399-4_86]

Deep-seated gravitational slope deformation

Soldati M.
2013

Abstract

Deep-seated gravitational slope deformations (DGSDs) are not considered hazardous phenomena because they evolve very slowly. However, they must not be neglected when defining slope instability in a territory and the related hazard implications. Despite their slow deformation rates, DGSDs may cause damage to surface and underground (e.g., tunnels) structures. In addition, they may evolve into faster mass movements or favor collateral landslide processes.
2013
no
https://link.springer.com/referencework/10.1007/978-1-4020-4399-4
Encyclopedia of Natural Hazards
P.T. Bobrowsky
151
155
9789048186990
Springer
PAESI BASSI
Dordrecht
Inglese
Deep-seated Gravitational Slope Deformations (DGSDs) are not considered hazardous phenomena, because they evolve very slowly. However, they must not be neglected when defining slope instability in a territory, and the related hazard implications. Despite their slow deformation rates, DGSDs may cause damage to surface and underground (e.g., tunnels) structures. In addition, the may evolve into faster mass movements, or favour collateral landslide processes.
Deep-Seated Gravitational Slope Deformation; Sackung; lateral spreading; hazard implications
Goal 11: Sustainable cities and communities
Deep-seated gravitational slope deformation / Soldati, M.. - STAMPA. - (2013), pp. 151-155. [10.1007/978-1-4020-4399-4_86]
Soldati, M.
Contributo su VOLUME::Voce in Dizionario o Enciclopedia
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Utilizza questo identificativo per citare o creare un link a questo documento: https://hdl.handle.net/11380/1320246
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