The Pays de Herve region in East Belgium is characterised by widespread slope instability. Some of these Quaternary paleo-landslides are still active, showing subsidence phenomena that can be related to the presence of weak subsurface materials such as clays (locally topped by weathered chalk) overlying a discontinuous sand-silt layer. This study provides a detailed characterisation of three active landslides in the area, with...

The characterization by means of geophysical techniques of agricultural soils subjected to continuous irrigation cycles makes it possible to study the heterogeneity of a soil and the preferential pathways of water flows without disturbing soil and plants. A better knowledge of soil heterogeneity enables optimal water resource management in terms of crop, yield, and sustainability. In this study, time-lapse monitoring using ele...

Back analysis is the most common method to study landslide movements after the event, and it allows us to understand how a landslide evolved along the slope. This paper presents the back-analysis of the Pomarico landslide (Basilicata, Italy) that occurred on January 25th, 2019, on the southwestern slope of the Pomarico hill. The landslide, of rotational clayey retrogressive type—planar sliding, evolved in different phases unti...