Climate effects on landscape evolution during the Late Pleistocene–Holocene transition (∼
14.6–8 ka) in southwestern North America traditionally are linked to the activity of the North …

Many debris flows increase in volume as they travel downstream, enhancing their mobility
and hazard. Volumetric growth can result from diverse physical processes, such as channel …

Fine sediment supply has been identified as an important factor contributing to the initiation
of runoff-generated debris flows after fire. However, despite the significance of fines for post …

The aim of this study is to improve the assessment of hazard posed by debris flows to the
people and settlements of Northwest Iceland by studying very recent examples from above …

The significance of debris flows for the morphogenesis of the medium–high mountains of
Central Europe has long been neglected. Herein we provide evidence from the …

Abstract The Middle Pleistocene–Holocene Sardinian stratigraphy has been revised to
identify the roles played by sea and climate changes in controlling sedimentation. The …

Temporal and spatial variations of tectonic rock uplift are generally thought to be the main
controls on long-term erosion rates in various landscapes. However, rivers continuously …

The Quaternary deposits of tectonically stable areas are a powerful tool to investigate high‐
frequency climate variations (< 10 ka) and to distinguish allogenic and autogenic factors …

The fault history of the Mill Creek strand of the San Andreas fault (SAF) in the San Gorgonio
Pass region, along with the reconstructed geomorphology surrounding this fault strand …

Abstract The High Tatras Mountains are known for frequent occurrences of hazardous
geomorphic processes. Many occur at the same localities. This similarity of occurrence is …