[HTML][HTML] The role of infrequently mobile boulders in modulating landscape evolution and geomorphic hazards
A landscape's sediment grain size distribution is the product of, and an important influence
on, earth surface processes and landscape evolution. Grains can be large enough that the …
on, earth surface processes and landscape evolution. Grains can be large enough that the …
Unsaturated flow processes and the onset of seasonal deformation in slow‐moving landslides
Predicting rainfall‐induced landslide motion is challenging because shallow groundwater
flow is extremely sensitive to the preexisting moisture content in the ground. Here, we use …
flow is extremely sensitive to the preexisting moisture content in the ground. Here, we use …
Rock properties and sediment caliber govern bedrock river morphology across the Taiwan Central Range
Feedbacks between surface and deep Earth processes in collisional mountain belts depend
on how erosion and topographic relief vary in space and time. One outstanding unknown …
on how erosion and topographic relief vary in space and time. One outstanding unknown …
Unravelling fluvial versus glacial legacy controls on boulder‐bed river geomorphology for semi‐alluvial rivers in Fennoscandia
River management is founded on predictable self‐organisation between river form and
catchment controls in alluvial rivers. However, a substantial proportion of rivers are not fully …
catchment controls in alluvial rivers. However, a substantial proportion of rivers are not fully …
Controls on fluvial sediment evacuation following an earthquake-triggered landslide: Observations from LiDAR time series
Catastrophic sediment overloading of mountain streams in response to coseismic
landsliding causes river systems to fundamentally reorganize their morphology and …
landsliding causes river systems to fundamentally reorganize their morphology and …
Wide bedrock valley development and sensitivity to environmental perturbations: Insights from flume experiments in erodible bedrock
AL Langston, CH Robertson - Earth Surface Processes and …, 2023 - Wiley Online Library
Wide bedrock valleys and their genetic descendants, strath terraces, can serve as
morphological records of past climate that reflect river discharge and sediment load during …
morphological records of past climate that reflect river discharge and sediment load during …
Tectonic advection of contacts enhances landscape transience
N Mitchell, AM Forte - Earth Surface Processes and Landforms, 2023 - Wiley Online Library
Contrasts in bedrock erodibility have been shown to drive landscape transience, but it is
unclear whether horizontal tectonic displacements would enhance such effects …
unclear whether horizontal tectonic displacements would enhance such effects …
The lasting legacy of megaflood boulder deposition in mountain rivers
Abstract Infrequent, large‐magnitude discharge (> 106 m3/s) outburst floods—megafloods—
can play a major role in landscape evolution. Prehistoric glacial lake outburst megafloods …
can play a major role in landscape evolution. Prehistoric glacial lake outburst megafloods …
Influence of rarely mobile boulders on channel width and slope: Theory and field application
Large, rarely mobile boulders are observed globally in mountainous bedrock channels.
Recent studies suggest that high concentrations of boulders could be associated with …
Recent studies suggest that high concentrations of boulders could be associated with …
Building a bimodal landscape: bedrock lithology and bed thickness controls on the morphology of Last Chance Canyon, New Mexico, USA
S Anderson, N Gasparini… - Earth Surface Dynamics, 2023 - esurf.copernicus.org
We explore how rock properties and channel morphology vary with rock type in Last Chance
Canyon, Guadalupe Mountains, New Mexico, USA. The rocks here are composed of …
Canyon, Guadalupe Mountains, New Mexico, USA. The rocks here are composed of …