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

<div>Synthetic geological and geotechnical cross section and conceptual model for water infiltration. The shear surface in red corresponds to the shear surface above which the deepest water table is studied in this work.</div>

Geofluids

fig11

Figure 11

Figure 11: Preferential Water Infiltration Path in a Slow-Moving Clayey Earthslide Evidenced by Cross-Correlation of Hydrometeorological Time Series (Charlaix Landslide, French Western Alps) 

Figure 11 | Preferential Water Infiltration Path in a Slow-Moving Clayey Earthslide Evidenced by Cross-Correlation of Hydrometeorological Time Series (Charlaix Landslide, French Western Alps) 