Articles | Volume 5, issue 1
https://doi.org/10.5194/esurf-5-161-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/esurf-5-161-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
River profile response to normal fault growth and linkage: an example from the Hellenic forearc of south-central Crete, Greece
Sean F. Gallen
CORRESPONDING AUTHOR
Geological Institute, Swiss Federal Institute of Technology (ETH),
8092 Zürich, Switzerland
Karl W. Wegmann
Department of Marine, Earth and Atmospheric Sciences, North Carolina
State University, Raleigh, 27695 NC, USA
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Latest update: 20 Nov 2024
Short summary
We present results from a natural experiment where bedrock rivers are adjusting to a step change in rock uplift rate and where constraints on the recent pattern of rock uplift exist. We show that while rivers record the relative rock uplift history, quantitative information on timing is masked by complexities in incision processes, changes in river network configuration, and possibly other factors. Our results emphasize caution when interpreting tectonic signals from some bedrock river systems.
We present results from a natural experiment where bedrock rivers are adjusting to a step change...