The shaping of erosional landscapes by internal dynamics
Erosional landscapes transport sediment downstream, host natural hazards and are
geologically active. While perturbations in external forcing, particularly climate and tectonics …
geologically active. While perturbations in external forcing, particularly climate and tectonics …
Fluvial archives, a valuable record of vertical crustal deformation
The study of drainage network response to uplift is important not only for understanding river
system dynamics and associated channel properties and fluvial landforms, but also for …
system dynamics and associated channel properties and fluvial landforms, but also for …
Dynamic reorganization of river basins
Introduction River networks, the backbone of most landscapes on Earth, collect and
transport water, sediment, organic matter, and nutrients from upland mountain regions to the …
transport water, sediment, organic matter, and nutrients from upland mountain regions to the …
Timescales of landscape response to divide migration and drainage capture: Implications for the role of divide mobility in landscape evolution
Efforts to extract information about climate and tectonics from topography commonly assume
that river networks are static. Drainage divides can migrate through time, however, and …
that river networks are static. Drainage divides can migrate through time, however, and …
[PDF][PDF] Miocene rejuvenation of topographic relief in the southern Appalachians
Conventional wisdom holds that the southern Appalachian Mountains have not experienced
a significant phase of tectonic forcing for> 200 myr; yet, they share many characteristics with …
a significant phase of tectonic forcing for> 200 myr; yet, they share many characteristics with …
Neogene rejuvenation of central Appalachian topography: Evidence for differential rock uplift from stream profiles and erosion rates
The persistence of topography within ancient orogens remains one of the outstanding
questions in landscape evolution. In the eastern North American Appalachians, this question …
questions in landscape evolution. In the eastern North American Appalachians, this question …
[图书][B] Rivers in the Landscape
E Wohl - 2020 - books.google.com
Rivers are the great shapers of terrestrial landscapes. Very few points on Earth above sea
level do not lie within a drainage basin. Even points distant from the nearest channel are …
level do not lie within a drainage basin. Even points distant from the nearest channel are …
Geometric disequilibrium of river basins produces long-lived transient landscapes
Although equilibrium has long been considered the attractor state for landscapes, the time
required to reach equilibrium or even the possibility of reaching equilibrium is still debated …
required to reach equilibrium or even the possibility of reaching equilibrium is still debated …
Preservation or piracy: Diagnosing low-relief, high-elevation surface formation mechanisms
Absent clear lithologic control, the presence of elevated, low-relief topography in upland
landscapes has traditionally been interpreted as a signature of relative surface uplift and …
landscapes has traditionally been interpreted as a signature of relative surface uplift and …
River profile response to normal fault growth and linkage: An example from the Hellenic forearc of south-central Crete, Greece
SF Gallen, KW Wegmann - Earth Surface Dynamics, 2017 - esurf.copernicus.org
Topography is a reflection of the tectonic and geodynamic processes that act to uplift the
Earth's surface and the erosional processes that work to return it to base level. Numerous …
Earth's surface and the erosional processes that work to return it to base level. Numerous …