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

<div>Water infiltration tests w1 and w2 (location in Figures <a href="../fig2/#b">2(b)</a> and <a href="../fig3/">3</a>) and saturated hydraulic conductivity.</div>

Geofluids

fig4

Figure 4

Figure 4: Preferential Water Infiltration Path in a Slow-Moving Clayey Earthslide Evidenced by Cross-Correlation of Hydrometeorological Time Series (Charlaix Landslide, French Western Alps) 

Figure 4 | Preferential Water Infiltration Path in a Slow-Moving Clayey Earthslide Evidenced by Cross-Correlation of Hydrometeorological Time Series (Charlaix Landslide, French Western Alps) 