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A quantitative geomorphological analysis of the drainage network has been performed to evaluate the influence of landslide processes on morphometric properties of the drainage network.
During the Pleistocene, a wider and larger incising river system resulted in rearrangements of the drainage network.
These anomalies match the directions of the drainage network that eroded the Astroni deposits in the eastern flank of the Solfatara cone, resulting in higher fluxes along the valleys.
Empirical relationships between suspended sediment yield and some geomorphic parameters of the drainage network allowed the estimation of short-term denudation rates in the study area.
We aim to evaluate the relationship between the geometry of the drainage network and the main fault systems in this region.
Breakthrough of the basin threshold and entrenchment of the drainage network must therefore be attributed to a latest Pleistocene to Holocene age.
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The value of R b for sub-watersheds shows that influences of geological structure on the drainage network are negligible.
The mean bifurcation ratio (Rbm) characteristically ranges between 3.0 and 5.0 for a basin when the influence of geological structures on the drainage network is negligible (Verstappen 1983).
R b characteristically ranges between 3.0 and 5.0 for watershed where the influence of geological structure on the drainage network is negligible (Verstappen 1983).
SB1 subwatershed shows low bifurcation index which are sure indicators of notable tectonic imprint on the drainage network.
Jamrar rivers show low bifurcation index which are positive indicators of notable tectonic imprint on the drainage network (Table 2).
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