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

<div>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 <a href="../fig5/#b">5(b)</a>. (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 <a href="../fig5/#a">5(a)</a>).</div>

Geofluids

fig5

Figure 5

Figure 5: 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 | Preferential Water Infiltration Path in a Slow-Moving Clayey Earthslide Evidenced by Cross-Correlation of Hydrometeorological Time Series (Charlaix Landslide, French Western Alps) 