『Abstract
we present detailed data of channel morphology for a river undergoing
a transient response to active normal faulting where excellent
constraints exist on spatial and temporal variations in fault
slip rates. We show that traditional hydraulic scaling laws break
down in this situation, and that channel widths become decoupled
from drainage area upstream of the fault. Unit stream powers are
〜4 times higher than those predicted by current scaling paradigms
and imply that incision rates for rivers responding to active
tectonics may be significantly higher than those heretofore modeled.
The loss of hydraulic scaling cannot be explained by increasing
channel roughness and is an intrinsic response to tectonic forcing.
We show that channel aspect ratio is a strongly nonlinear function
of local slope and demonstrate that fault-induced adjustment of
channel geometries has reset hillslope gradients. The results
give new insight into how rivers maintain their course in the
face of tectonic uplift and illustrate the first-order control
the fluvial system exerts on the locus and magnitude of sediment
supply to basins.
Keywords: rivers; tectonics; faulting; channel geometry; geomorphology』
Introduction
Study area and methods
Results
Implications
Conclusions
Acknowledgments
References cited