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

Table 2

Geotechnical parameters used for stability computations.

Unit	Depth range	Weight	Cohesion	Friction angle
	(m)	(kN/m^3)	(kPa)	(°)
Moraines	0 to 3–5	20	0	30
Upper laminated clays	3–5 to 8–12	19	2	19
Lower laminated clays	>12	19	4	20