Geomorphological analysis of drainage changes in the NE Apennines piedmont area: the case of the middle Tavo River bend (Abruzzo, Central Italy)

This work presents a tectonic geomorphology analysis of a river bend in the middle Tavo River valley, in the piedmont area of the NE Apennines (Abruzzo Region), between the eastern slope of the chain (Gran Sasso Massif) and the Adriatic coast. The main map (1:15,000 scale) was obtained through a mor...

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Main Authors: Cristiano Carabella, Marcello Buccolini, Luca Galli, Enrico Miccadei, Giorgio Paglia, Tommaso Piacentini
Format: Article
Language:English
Published: Taylor & Francis Group 2020-12-01
Series:Journal of Maps
Subjects:
Online Access:http://dx.doi.org/10.1080/17445647.2020.1726833
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author Cristiano Carabella
Marcello Buccolini
Luca Galli
Enrico Miccadei
Giorgio Paglia
Tommaso Piacentini
author_facet Cristiano Carabella
Marcello Buccolini
Luca Galli
Enrico Miccadei
Giorgio Paglia
Tommaso Piacentini
author_sort Cristiano Carabella
collection DOAJ
description This work presents a tectonic geomorphology analysis of a river bend in the middle Tavo River valley, in the piedmont area of the NE Apennines (Abruzzo Region), between the eastern slope of the chain (Gran Sasso Massif) and the Adriatic coast. The main map (1:15,000 scale) was obtained through a morphometric, geological, and geomorphological analysis, and was composed of four sections including orography and hydrography at basin scale, main map at local scale, geomorphological cross-section and longitudinal profiles, and morphoneotectonic analysis. This study provides a basis for the recognition of morphostructural and morphotectonic features that control the drainage evolution of the Tavo River. Specifically, the study is focused on the Tavo-Saline basin characterized by possible capture processes, and the evolution of the watershed with the Pescara basin. The results from this study can contribute to the understanding of the evolution of the NE Apennines piedmont area since the Middle Pleistocene.
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spelling doaj.art-1cb263a1a54848c288f5a0e897265d332022-12-21T22:00:11ZengTaylor & Francis GroupJournal of Maps1744-56472020-12-0116222223510.1080/17445647.2020.17268331726833Geomorphological analysis of drainage changes in the NE Apennines piedmont area: the case of the middle Tavo River bend (Abruzzo, Central Italy)Cristiano Carabella0Marcello Buccolini1Luca Galli2Enrico Miccadei3Giorgio Paglia4Tommaso Piacentini5Department of Engineering and Geology, Università degli Studi “G. d’Annunzio” Chieti-Pescara, Laboratory of Tectonic Geomorphology and GISDepartment of Engineering and Geology, Università degli Studi “G. d’Annunzio” Chieti-Pescara, Laboratory of Tectonic Geomorphology and GISDepartment of Engineering and Geology, Università degli Studi “G. d’Annunzio” Chieti-Pescara, Laboratory of Tectonic Geomorphology and GISDepartment of Engineering and Geology, Università degli Studi “G. d’Annunzio” Chieti-Pescara, Laboratory of Tectonic Geomorphology and GISDepartment of Engineering and Geology, Università degli Studi “G. d’Annunzio” Chieti-Pescara, Laboratory of Tectonic Geomorphology and GISDepartment of Engineering and Geology, Università degli Studi “G. d’Annunzio” Chieti-Pescara, Laboratory of Tectonic Geomorphology and GISThis work presents a tectonic geomorphology analysis of a river bend in the middle Tavo River valley, in the piedmont area of the NE Apennines (Abruzzo Region), between the eastern slope of the chain (Gran Sasso Massif) and the Adriatic coast. The main map (1:15,000 scale) was obtained through a morphometric, geological, and geomorphological analysis, and was composed of four sections including orography and hydrography at basin scale, main map at local scale, geomorphological cross-section and longitudinal profiles, and morphoneotectonic analysis. This study provides a basis for the recognition of morphostructural and morphotectonic features that control the drainage evolution of the Tavo River. Specifically, the study is focused on the Tavo-Saline basin characterized by possible capture processes, and the evolution of the watershed with the Pescara basin. The results from this study can contribute to the understanding of the evolution of the NE Apennines piedmont area since the Middle Pleistocene.http://dx.doi.org/10.1080/17445647.2020.1726833morphotectonicsfluvial terraceslongitudinal profilesdrainage evolutionriver bendcapture process
spellingShingle Cristiano Carabella
Marcello Buccolini
Luca Galli
Enrico Miccadei
Giorgio Paglia
Tommaso Piacentini
Geomorphological analysis of drainage changes in the NE Apennines piedmont area: the case of the middle Tavo River bend (Abruzzo, Central Italy)
Journal of Maps
morphotectonics
fluvial terraces
longitudinal profiles
drainage evolution
river bend
capture process
title Geomorphological analysis of drainage changes in the NE Apennines piedmont area: the case of the middle Tavo River bend (Abruzzo, Central Italy)
title_full Geomorphological analysis of drainage changes in the NE Apennines piedmont area: the case of the middle Tavo River bend (Abruzzo, Central Italy)
title_fullStr Geomorphological analysis of drainage changes in the NE Apennines piedmont area: the case of the middle Tavo River bend (Abruzzo, Central Italy)
title_full_unstemmed Geomorphological analysis of drainage changes in the NE Apennines piedmont area: the case of the middle Tavo River bend (Abruzzo, Central Italy)
title_short Geomorphological analysis of drainage changes in the NE Apennines piedmont area: the case of the middle Tavo River bend (Abruzzo, Central Italy)
title_sort geomorphological analysis of drainage changes in the ne apennines piedmont area the case of the middle tavo river bend abruzzo central italy
topic morphotectonics
fluvial terraces
longitudinal profiles
drainage evolution
river bend
capture process
url http://dx.doi.org/10.1080/17445647.2020.1726833
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