Alluvial and fluvial fans are the most widespread depositional landforms bordering the
margins of long-lived highland regions and actively subsiding continental basins, across a …

Debris flows are among the most catastrophic natural phenomena, attracting the interest of
researchers, engineers and government agencies. The complexity of the physical process …

Geomorphic mass flows are often complex in terms of material composition and its evolution
in space and time. The simulation of those hazardous phenomena would strongly benefit …

Debris flows are water-laden masses of sediment that move rapidly through channel
networks and over alluvial fans, where they can devastate people and property. Episodic …

Debris flows can grow greatly in size by entrainment of bed material, enhancing their runout
and hazardous impact. Here, we experimentally investigate the effects of debris‐flow …

Understanding the physics of phase separation between solid and fluid phases as a mixture
mass moves down-slope is a long-standing challenge. Here, we propose an extension of a …

Abstract In the northern Iberian Peninsula, the Pyrenean-Cantabrian orogenic belt extends
EW for ca. 1000 km between the Atlantic Ocean and Mediterranean Sea. This orogen …

We report on a multi-proxy study of the Carnian Pluvial Episode in the continental Argana
Basin (Morocco) based on mineralogy, geochemistry, paleosols and sedimentary features …

Predicting the spatial impact of debris flows on fans is challenging due to complex runout
behaviour. Debris flow mobility is highly variable and flows can sporadically avulse the …

Submarine fans are formed by sediment‐laden flows shed from continental margins into
ocean basins. Their morphology represents the interplay of external controls such as …