Geological structures such as folds, faults, and discontinuities play a critical role in the
stability and behaviour of both natural and engineered rock slopes. Although engineering …

Deep-seated gravitational slope deformations (DSGSDs) are slow moving, hillslope-scale
mass movements featuring characteristic landforms such as double-crested ridges and …

Faults play a crucial role in shaping the formation and damage patterns of landslides in the
mountainous region, particularly in Qinling-Daba (Qinba) area in China. On 6 October 2022 …

Preliminary knowledge of the surface movement and internal structure of a landslide is
essential to improve the understanding of landslide behavior as an initial step to develop …

Quantifying the velocity, volume, and rheology of deep, slow‐moving landslides is essential
for hazard prediction and understanding landscape evolution, but existing field‐based …

The large-scale deformation of high mountain slopes finds its origin in many phenomena
(inherent parameters, external stresses) with very different time constants (instantaneous to …

Deep-seated rock slides (DSRSs), recognised as one of the most important mass wasting
processes worldwide, involve large areas and cause several consequences in terms of …

Deep-seated rockslides, which are characterised by slow to extremely slow rates of
movement, frequently occur in foliated metamorphic rock masses (schists, phyllites …

The geometry of the bedrock, internal layers and shear surfaces/bands controls the
deformation pattern and the mechanisms of landslides. A challenge to progress in the …

Studying long term-evolution of gravitational slope evolution is a key to understanding deep-
seated landslide processes. This paper deals with three large Deep-Seated Landslides …