The movement of sediment from mountainous uplands to continental margins, i.e. the sediment cascade, modifies the terrestrial surface and eventually drives the rate of topographic evolution. Understanding the pattern and rates of geomorphic mechanisms involved in the sediment cascade is of crucial importance to constrain biogeochemical cycles, long-term landscape evolution and potential feedbacks between tectonics, erosion and climate. Sediment cascading systems are still poorly constrained, as sediment budgets and connectivity can be highly variable in space and time due to the stochastic character of geomorphic processes. In an effort to improve our quantitative understanding of the sediment cascade in landslide-prone environments, this d...
Alpine water and sediment supply influence the sediment budget of many important European fluvial sy...
International audienceWe used concentrations of in situ cosmogenic 10Be from riverine sediment to qu...
A hydrology–sediment modelling framework based on the model Topkapi‐ETH combined with basin geomorph...
Tectonic and geomorphic processes drive landscape evolution over different spatial and temporal scal...
To constrain the timing of the sediment cascade, the inherent stochastic nature of sediment and tran...
Tectonic and geomorphic processes drive landscape evolution. In mountainous environments, river inci...
Accurately assessing geo-hazards and quantifying landslide risks in mountainous environments are gai...
The coupling relationships between hillslope and channel network are fundamental for the understandi...
Quantification of the volumes of sediment removed by rock–slope failure and debris flows and identif...
International audienceLandscape dynamics are determined by interactions amongst geomorphic processes...
Rates of sediment supply by landsliding to an alluvial channel in a small catchment in central Switz...
Landscape evolution in mountainous catchments is the result of multiple factors acting at different ...
We compile detrital 10Be concentrations of Alpine rivers, representing the denudation rates pattern ...
Alpine water and sediment supply influence the sediment budget of many important European fluvial sy...
International audienceWe used concentrations of in situ cosmogenic 10Be from riverine sediment to qu...
A hydrology–sediment modelling framework based on the model Topkapi‐ETH combined with basin geomorph...
Tectonic and geomorphic processes drive landscape evolution over different spatial and temporal scal...
To constrain the timing of the sediment cascade, the inherent stochastic nature of sediment and tran...
Tectonic and geomorphic processes drive landscape evolution. In mountainous environments, river inci...
Accurately assessing geo-hazards and quantifying landslide risks in mountainous environments are gai...
The coupling relationships between hillslope and channel network are fundamental for the understandi...
Quantification of the volumes of sediment removed by rock–slope failure and debris flows and identif...
International audienceLandscape dynamics are determined by interactions amongst geomorphic processes...
Rates of sediment supply by landsliding to an alluvial channel in a small catchment in central Switz...
Landscape evolution in mountainous catchments is the result of multiple factors acting at different ...
We compile detrital 10Be concentrations of Alpine rivers, representing the denudation rates pattern ...
Alpine water and sediment supply influence the sediment budget of many important European fluvial sy...
International audienceWe used concentrations of in situ cosmogenic 10Be from riverine sediment to qu...
A hydrology–sediment modelling framework based on the model Topkapi‐ETH combined with basin geomorph...