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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Format: | Article |
Language: | English |
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Taylor & Francis Group
2020-12-01
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Series: | Journal of Maps |
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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. |
first_indexed | 2024-12-17T06:28:58Z |
format | Article |
id | doaj.art-1cb263a1a54848c288f5a0e897265d33 |
institution | Directory Open Access Journal |
issn | 1744-5647 |
language | English |
last_indexed | 2024-12-17T06:28:58Z |
publishDate | 2020-12-01 |
publisher | Taylor & Francis Group |
record_format | Article |
series | Journal of Maps |
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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