A new data‐driven Bayesian inversion of fluvial topography clarifies the tectonic history of the corinth rift and reveals a channel steepness threshold
Landscape evolution models that invert topography for rock uplift can improve our
understanding of both tectonic and geomorphic processes when properly constrained with …
understanding of both tectonic and geomorphic processes when properly constrained with …
[HTML][HTML] Interplay between tectonics and surface processes in the evolution of mountain ranges: Insights from landscape dynamics, uplift, and active deformation of …
Drainage divides are dynamic features of a landscape that migrate over time during the
development of river networks. In this study, we focused on the geomorphic response of a …
development of river networks. In this study, we focused on the geomorphic response of a …
[HTML][HTML] Growing topography due to contrasting rock types in a tectonically dead landscape
Many mountain ranges survive in a phase of erosional decay for millions of years following
the cessation of tectonic activity. Landscape dynamics in these post-orogenic settings have …
the cessation of tectonic activity. Landscape dynamics in these post-orogenic settings have …
Linear inversion of fluvial topography in the northern Apennines: Comparison of base‐level fall to crustal shortening
Fluvial terraces, longitudinal river profiles, and growth strata carry comparable records of the
deformation history in tectonically active mountain belts. In the northern Apennines, these …
deformation history in tectonically active mountain belts. In the northern Apennines, these …
[HTML][HTML] Morphometric properties of river basins as indicators of relative tectonic activity–Problems of data handling and interpretation
M Różycka, P Migoń - Geomorphology, 2021 - Elsevier
Morphometric properties of drainage basins, expressed as indices related to their shapes,
altitude variability, river networks and stream profiles, are frequently used as proxy …
altitude variability, river networks and stream profiles, are frequently used as proxy …
River patterns reveal two stages of landscape evolution at an oblique convergent margin, Marlborough Fault System, New Zealand
Here we examine the landscape of New Zealand's Marlborough Fault System (MFS), where
the Australian and Pacific plates obliquely collide, in order to study landscape evolution and …
the Australian and Pacific plates obliquely collide, in order to study landscape evolution and …
The lasting legacy of glacial landscape dynamics: Capturing the transport of boulder armor and hillslope retreat with geochronology in the Flint Hills of Kansas
NR McCarroll, A Temme - Geomorphology, 2024 - Elsevier
We present new geochronological data derived from hillslope boulder armor in the Flint Hills
in northeastern KS, United States, that provides insights into the rates and timing of lateral …
in northeastern KS, United States, that provides insights into the rates and timing of lateral …
Tectonic advection of contacts enhances landscape transience
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 …
Lithological controls on the timing of strath terrace staircase formation in a collisional mountain belt
In mountain belts, strath terrace staircases serve as markers for deriving river incision rates
and erosional patterns. Distinguishing between terrace patterns influenced by external …
and erosional patterns. Distinguishing between terrace patterns influenced by external …
Scale‐dependent contributors to river profile geometry
A range of complex hydraulic and geomorphic processes shape terrestrial landscapes. It
remains unclear how these processes act to generate observed drainage networks across …
remains unclear how these processes act to generate observed drainage networks across …