Earth-surface processes operate across erosionally dominated landscapes and deliver
sediment to depositional systems that can be preserved over a range of timescales. The …

Two twin short gravity cores and a long piston core recovered from the deepest part of
proglacial Lake Bramant (Grandes Rousses Massif, French Alps), under and overlying a …

Understanding the long‐term earthquake recurrence pattern at subduction zones requires
continuous paleoseismic records with excellent temporal and spatial resolution and stable …

Central Switzerland lies tectonically in an intraplate area and recurrence rates of strong
earthquakes exceed the time span covered by historic chronicles. However, many lakes are …

Seismically‐induced event deposits embedded in the sedimentary infill of lacustrine basins
are highly useful for palaeoseismic reconstructions. Recent, well‐documented, great …

Some of the largest mass movements in the Alps cluster spatially in the Tyrol (Austria). Fault-
related valley deepening and coalescence of brittle discontinuities structurally controlled the …

Understanding the seismic hazard posed by large earthquakes requires paleoseismic
investigation because most faults have not ruptured repeatedly during the period of historic …

Accurate probabilistic seismic hazard analysis requires a good knowledge of the recurrence
parameters of the strongest earthquakes in a region. Due to the typical short temporal span …

Palaeoflood hydrology is an expanding field as the damage potential of flood and flood-
related processes are increasing with the population density and the value of the …

The hazard of any natural process can be expressed as a function of its magnitude and the
annual probability of its occurrence in a particular region. Here we expand on the hypothesis …