Geoelectrical Tomography as an Operative Tool for Emergency Management of Landslide: An Application in Basilicata Region, Italy
Figure 3
(a) Comparison between AA′ ERT, carried out with longitudinal direction to the landslide body, and S1 and S2 stratigraphical data; (b) comparison between BB′ ERT and S1 stratigraphical data. The horizontal resistivity contrast, highlighted with white dashed line in both the ERT, corresponds to the contact between detrital material (slide material) and argillite material.
