Das vermeintliche» Ende der Geschichte «hat sich längst vielmehr als ein Ende der
Gewissheiten entpuppt. Mehr denn je stellt sich nicht nur die Frage nach der jeweiligen» …

The geological structure of the Three-rivers Basin is complex, with active tectonic
movements and frequent earthquakes, resulting in fragile geological circumstances …

Rock glaciers are receiving increased attention as a potential source of water and indicator
of climate change in periglacial landscapes. They consist of an ice‐debris mixture, which …

Ambient vibration measurements can detect resonance frequency changes related to rock
slope instability damage or boundary condition changes during progressive failure …

Accurate assessments of the internal structure and boundary conditions of unstable rock
slopes are imperative for evaluating landslide hazard scenarios. However, instability …

The anticipation of massive rock slope failures is a key mitigation strategy in a changing
climate and environment requiring a precise understanding of pre-failure process dynamics …

The study of the deformation of rock masses in response to near-surface thermal stresses is
nowadays considered crucial in the field of geological risk mitigation. The superposition of …

Massive sediment pulses in catchments are a key alpine multi-risk component. Substantial
sediment redistribution in alpine catchments frequently causes flooding, river erosion, and …

Seismic resonance and surface displacement measurements can be implemented in
tandem to improve landslide characterization and progressive failure monitoring. Crack …

Monitoring and early warning systems based on process dynamics gain importance to cope
with an increasing number of alpine hazards. The imminent Hochvogel rock slope failure (up …