2017
DOI: 10.1016/j.geomorph.2017.07.011
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Unsteady sediment discharge in earth flows: A case study from the Mount Pizzuto earth flow, southern Italy

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Cited by 32 publications
(23 citation statements)
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“…The displacement field of Figure 4b depicts a typical condition for this kind of landslide with velocity variations related to the width of the landslide corridor and to the distance from the toe. Specifically, as the width of the landslide corridor decreases, velocity increase and vice versa [40]. In addition, the proposed coded procedure seems to be able to recognize (lateral) spreading occurring at the toe of the slide and velocity reduction at cross-section edges.…”
Section: Discussion and Validationmentioning
confidence: 93%
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“…The displacement field of Figure 4b depicts a typical condition for this kind of landslide with velocity variations related to the width of the landslide corridor and to the distance from the toe. Specifically, as the width of the landslide corridor decreases, velocity increase and vice versa [40]. In addition, the proposed coded procedure seems to be able to recognize (lateral) spreading occurring at the toe of the slide and velocity reduction at cross-section edges.…”
Section: Discussion and Validationmentioning
confidence: 93%
“…Once the displacement field is obtained, this is validated using a comparison with available local velocity data and considering the expected earthflow and glacier spatial kinematics [16,30,[39][40][41].…”
Section: Methodsmentioning
confidence: 99%
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“…In these conditions, the combination of multiple perspectives derived by the analysis of aerial imagery and the direct observation in the field is often the key to accurately report a landslide and its mesoscopic features in a map (e.g. Ardizzone et al, 2012;Calista et al, 2016;Guerriero et al, 2013;Guerriero et al, 2016;Guerriero et al, 2017a;Revellino, Grelle, Donnarumma, & Guadagno, 2010;Santangelo, Gioia, Cardinali, Guzzetti, & Schiattarella, 2015). Conversely, in urban areas, landslide identification is not always possible due to the masking action of urban settlements.…”
Section: Introductionmentioning
confidence: 99%
“…On 15 October 2015, a destructive overflow of the Tammaro and Calore rivers hit the town of Benevento in southern Italy, and the central sector of its province, already known for other natural hazards like landslides and earthquakes (e.g. Guerriero et al, 2016;Guerriero et al, 2017;Maresca, Castellano, De Matteis, Saccorotti, & Vaccariello, 2003;Revellino, Grelle, Donnarumma, & Guadagno, 2010). The event caused two deaths and severe damage to infrastructure, buildings and local agriculture.…”
Section: Introductionmentioning
confidence: 99%