Geofluids / 2018 / Article / Fig 5

Research Article

Preferential Water Infiltration Path in a Slow-Moving Clayey Earthslide Evidenced by Cross-Correlation of Hydrometeorological Time Series (Charlaix Landslide, French Western Alps)

Figure 5

Surface deformation. (a) Interpolated map of surface displacement rates between March 2016 and June 2017. The red arrow corresponds to the topographic profile in Figure 5(b). (b) Topographic cross section, surface displacement rates measured at geodetic stations, and supposed location of the shear surface at around 10 m depth. (c) Time series of cumulated total displacements (XYZ) for stations r01 and r02 between late November 2014 and late June 2017 and for station r03 between mid-March 2016 and late June 2017 (location in Figure 5(a)).

Article of the Year Award: Outstanding research contributions of 2020, as selected by our Chief Editors. Read the winning articles.