This work analyzes the role of paleo-drainage network, morphotectonics, and surface processes in landscape evolution in a sector of the transition zone between the chain and the piedmont area of Central Apennines. Particularly, it focuses on the Verde Stream, a tributary of the middle Sangro River valley, which flows in the southeastern Abruzzo area at the boundary with the Molise region. The Verde Stream was investigated through a drainage basin scale geomorphological analysis incorporating the morphometry of the orography and hydrography, structural geomorphological field mapping, and the investigation of morphological field evidence of tectonics with their statistical azimuthal distributions. The local data obtained were compared with th...
We present a geomorphological analysis of the recent extensional tectonics of a Quaternary continent...
The aim of this work is to provide a methodological input based on geostatistical topographic analys...
Geologic and geomorphic data suggest that the topographic growth of the Apennines has been very slow...
This work analyzes the role of paleo-drainage network, morphotectonics, and surface processes in lan...
This work presents the morphotectonic map of the Tasso Stream-Sagittario River valley, located in th...
Topography of the Apennines chain resulted from the combined action of tectonic displacements (relat...
This study focuses on the morphotectonic evolution of the Apennines Central Adriatic piedmont, and i...
This study focuses on the morphotectonic evolution of the Apennines Central Adriatic piedmont, and i...
This study focuses on the morphotectonic evolution of the Apennines Central Adriatic piedmont, and i...
The Umbro-Marchean Apennines form an arcuate NW–SE fold-and-thrust belt of NE convexity. The orogen ...
<p>This paper presents a geomorphological map of the floodplain at the confluence of the Aventino an...
Quaternary continental deposits record spatio-temporal changes of the landscape and offer insights f...
In active tectonic regions, topography results from the interaction between tectonics and surface pr...
We present a geomorphological analysis of the recent extensional tectonics of a Quaternary continent...
The aim of this work is to provide a methodological input based on geostatistical topographic analys...
Geologic and geomorphic data suggest that the topographic growth of the Apennines has been very slow...
This work analyzes the role of paleo-drainage network, morphotectonics, and surface processes in lan...
This work presents the morphotectonic map of the Tasso Stream-Sagittario River valley, located in th...
Topography of the Apennines chain resulted from the combined action of tectonic displacements (relat...
This study focuses on the morphotectonic evolution of the Apennines Central Adriatic piedmont, and i...
This study focuses on the morphotectonic evolution of the Apennines Central Adriatic piedmont, and i...
This study focuses on the morphotectonic evolution of the Apennines Central Adriatic piedmont, and i...
The Umbro-Marchean Apennines form an arcuate NW–SE fold-and-thrust belt of NE convexity. The orogen ...
<p>This paper presents a geomorphological map of the floodplain at the confluence of the Aventino an...
Quaternary continental deposits record spatio-temporal changes of the landscape and offer insights f...
In active tectonic regions, topography results from the interaction between tectonics and surface pr...
We present a geomorphological analysis of the recent extensional tectonics of a Quaternary continent...
The aim of this work is to provide a methodological input based on geostatistical topographic analys...
Geologic and geomorphic data suggest that the topographic growth of the Apennines has been very slow...