2021
DOI: 10.1016/j.enggeo.2021.106345
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Monitoring and analysis of the exceptional displacements affecting debris at the top of a highly disaggregated rockslide

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Cited by 18 publications
(19 citation statements)
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“…Furthermore, it can be subdivided in two scarps: the upper one is a sub-vertical rock cliff of about 30 m in height, while the lower one is characterized by a more widespread debris cover (Figure 1). Over the years, a large lobe of chaotic debris has propagated towards the valley bottom, giving origin to secondary mass wasting processes in the form of rockfalls, debris flows, and shallow slumps (Carlà et al, 2021).…”
Section: Landslide Of Interestmentioning
confidence: 99%
“…Furthermore, it can be subdivided in two scarps: the upper one is a sub-vertical rock cliff of about 30 m in height, while the lower one is characterized by a more widespread debris cover (Figure 1). Over the years, a large lobe of chaotic debris has propagated towards the valley bottom, giving origin to secondary mass wasting processes in the form of rockfalls, debris flows, and shallow slumps (Carlà et al, 2021).…”
Section: Landslide Of Interestmentioning
confidence: 99%
“…Most of the instrumentation installed on the slide area (mainly wire extensometers and borehole inclinometers) was therefore progressively damaged, leaving the GB-InSAR system as the sole operational tool for quantifying the slope displacements in space and time. This large set of data was exploited to directly or indirectly derive an updated assessment of the thickness of upper debris affected by greater deformation; the differences in deformation behaviour at different slide locations and depths; and the nature of hydrological forcing behind the recent reactivation phases (Carlà et al 2021). In particular, slope displacements were combined with groundwater level measurements from two standpipe piezometers located behind the upper limit of the slide area.…”
Section: Wp1mentioning
confidence: 99%
“…The case study chosen for the work was the Ruinon landslide (Figure 1 andFigure 2) in the Upper Valtellina, Northern Italy. It is one of the most active slope failures in Italy, also very well monitored and studied (Del Piccolo, 1999;Agliardi et al, 2001;Tarchi et al, 2003;Del Ventisette et al, 2012;Carlà et al, 2021). The landslide can be characterized as a "translational rock-debris slide" sitting at the base of deep-seated gravitational slope deformation which is affecting the entire slope.…”
Section: Case Studymentioning
confidence: 99%