Large rock slope failures are temporal processes which act to modify the landscape after glacial retreat. The failure process often shows a lag time of thousands years deglaciation, with multiple events possible. While global datasets constrain this from extensive mapping and dating paraglacial avalanches, timeline is poorly refined in northern Norway. We present case study multiphase at Skredk...

Slope stability is one of the most important topics engineering geology with a background more than 300 years. So far, various assessment techniques have been developed which include range simple evaluations, planar failure, limit state criteria, equilibrium analysis, numerical methods, hybrid and high-order approaches are implemented in two-dimensional (2D) three-dimensional (3D) space. In mea...