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Evaluation of shallow landslide-triggering scenarios through a physically based approach: an example of application in the southern Messina area (northeastern Sicily, Italy)

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Academic year: 2017

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Figure 1. (a) Extent of the study area (red line). The upper left sketch shows the location of the area, represented by the red square; (b) aerial view of the Giampilieri area a few days after the 1 October 2009 event.
Figure 3. Different types of shallow landslides which occurred on 1 October 2009: (a) debris flows, (b) debris slides and (c) debris avalanches.
Figure 5. Summary of the back analysis process used for the 2009 event.
Figure 6. Conceptual sketch of the hydrological model in TRIGRS simulating tension-saturated (a) and unsaturated (b) soil conditions (modified from Baum et al., 2010).
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