Long paleoseismic records on mature faults suggest potentially chaotic recurrence patterns
with cycles of strain accumulation and release that challenge simple slip-or time-predictable …

Surface-rupturing earthquakes can produce fault displacements that abruptly alter the
established course of rivers. Several notable examples of fault rupture–induced river …

The estimation of the maximum expected magnitude is crucial for seismic hazard
assessment. It is usually inferred via Bayesian analysis; alternatively, the size of the largest …

A physics-based earthquake simulator should reproduce first-order empirical power-law
behaviors of magnitudes and clustering. These laws have emerged spontaneously in either …

Strike-slip fault ruptures have a limited capacity to generate vertical deformation, and for this
reason they are usually dismissed as potential destructive tsunami sources. At the western …

Physics‐based earthquake simulators have been developed to overcome the relatively short
duration and incompleteness of historical earthquake and paleoseismic records …

Introduced trout can induce trophic cascades, however, a lack of pre-introduction data limits
knowledge on their impact in many lakes. Traditional paleolimnological approaches have …

Fault zones along active tectonic block boundaries are a significant source of devastating
continental earthquakes. Strong earthquakes produce disruptions of sediment and induce …

Introduction Research has shown that tourists are vulnerable to natural hazards during their
travels. For this reason, communicating potential natural hazard risks to tourists prior to, and …

We examined the stratigraphy of alluvial fans formed at the steep range front of the Southern
Alps at Te Taho, on the north bank of the Whataroa River in central West Coast, South …