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

<div>Inclinometer data for (a) i1 and (b) i2. (c) and (d) Extraction of cumulated displacements at 4 m to 5 m depth for i1 and i2, respectively. The blue and white bands correspond to the autumn-winter season (November to March) and to the spring-summer season (April to October), respectively. Values inside the graphs correspond to the average velocity, in cm/yr, for each period.</div>

Geofluids

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Figure 6

Figure 6: Preferential Water Infiltration Path in a Slow-Moving Clayey Earthslide Evidenced by Cross-Correlation of Hydrometeorological Time Series (Charlaix Landslide, French Western Alps) 

Figure 6 | Preferential Water Infiltration Path in a Slow-Moving Clayey Earthslide Evidenced by Cross-Correlation of Hydrometeorological Time Series (Charlaix Landslide, French Western Alps) 