“…Most landslides occur in wet, partially saturated soils due to prolonged or intense rainfall, snowmelt, or seismic activity (Leonarduzzi et al, 2017;Schuster and Wieczorek, 2018). An increasing water content in the soil induces a reduction of soil shear strength leading to the failure of soil material within a shear band, usually situated at the interface of below-ground discontinuities such as between soil and bedrock (Catani et al, 2010;Zhang et al, 2017;Xiao et al, 2023) or between different soil horizons (Li et al, 2013;Ali et al, 2014;Ran et al, 2018;Chinkulkijniwat et al, 2019). This boundary defines the failure plane of shallow landslides and is as such implemented in physically-based models (Ran et al, 2018).…”