Northern Apennines is tectonically an active fold and thrust belt. Digital Elevation Model (DEM) based drainage network was extracted to analyze river profiles to document the influence of neotectonics on landscape evolution in Rossenna river basin, northern Apennines Italy. This approach decodes the neotectonic signals by computing channel steepness, Hack stream-length gradient (HSLG) and knickpoints analyses. The main objective was to examine how spatially variable rock uplift relate to changes in river morphology. The results obtained are consistent with the recent tectonic uplift of the region. The presence of knickpoint anomalies and higher values of steepness and HSLG index in south west region and the lower segments of Rossenna River...
This study aimed at the reconstruction of magnitude and timing of uplift of a wide sector of the Ce...
In active tectonic landscapes, topography is shaped by the interactions of tectonic activity that up...
The aim of this work is to test an integrated quantitative geomorphic approach based on Stream Lengt...
Northern Apennines is tectonically an active fold and thrust belt. Digital Elevation Model (DEM) bas...
The landscape evolution in active orogens is mainly dictated by the interaction of tectonic and eros...
The investigated area is situated in central Italy and it extends from the axial zone of the Umbria–...
Crustal uplift and erosional processes, such as river-valley incision and hillslope denudation, are ...
Crustal uplift and erosional processes, such as river-valley incision and hillslope denudation, are ...
Geomorphological, morphotectonic, stratigraphical, structural and geological data were collected in ...
The central Italian Apennines have gone through a complex evolutionary history, involving compressio...
The proclivity of river networks to progressively carve mountain surfaces and preserve markers of la...
In active tectonic regions, topography results from the interaction between tectonics and surface pr...
We present detailed observations of rivers crossing active normal faults in the Central Apennines, I...
This study aimed at the reconstruction of magnitude and timing of uplift of a wide sector of the Ce...
In active tectonic landscapes, topography is shaped by the interactions of tectonic activity that up...
The aim of this work is to test an integrated quantitative geomorphic approach based on Stream Lengt...
Northern Apennines is tectonically an active fold and thrust belt. Digital Elevation Model (DEM) bas...
The landscape evolution in active orogens is mainly dictated by the interaction of tectonic and eros...
The investigated area is situated in central Italy and it extends from the axial zone of the Umbria–...
Crustal uplift and erosional processes, such as river-valley incision and hillslope denudation, are ...
Crustal uplift and erosional processes, such as river-valley incision and hillslope denudation, are ...
Geomorphological, morphotectonic, stratigraphical, structural and geological data were collected in ...
The central Italian Apennines have gone through a complex evolutionary history, involving compressio...
The proclivity of river networks to progressively carve mountain surfaces and preserve markers of la...
In active tectonic regions, topography results from the interaction between tectonics and surface pr...
We present detailed observations of rivers crossing active normal faults in the Central Apennines, I...
This study aimed at the reconstruction of magnitude and timing of uplift of a wide sector of the Ce...
In active tectonic landscapes, topography is shaped by the interactions of tectonic activity that up...
The aim of this work is to test an integrated quantitative geomorphic approach based on Stream Lengt...