Morphotectonics of the Pescara River basin (Central Italy)

This work presents a morphotectonic map of the Pescara River basin (1:40,000 scale), located in the piedmont-hilly area of the central-eastern Apennines (Abruzzo Region, Italy), and stretching from the eastern slope of the chain (Maiella Massif, Morrone Mt. and Gran Sasso Range) to the Adriatic coas...

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Main Authors: Tullio Urbano, Tommaso Piacentini, Marcello Buccolini
Format: Article
Language:English
Published: Taylor & Francis Group 2017-11-01
Series:Journal of Maps
Subjects:
Online Access:http://dx.doi.org/10.1080/17445647.2017.1338204
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spelling doaj-bf7b4010b54d4410b6ab432c29d77edf2020-11-25T02:02:30ZengTaylor & Francis GroupJournal of Maps1744-56472017-11-0113251152010.1080/17445647.2017.13382041338204Morphotectonics of the Pescara River basin (Central Italy)Tullio Urbano0Tommaso Piacentini1Marcello Buccolini2Università degli Studi “G. d’Annunzio” di Chieti-PescaraUniversità degli Studi “G. d’Annunzio” di Chieti-PescaraUniversità degli Studi “G. d’Annunzio” di Chieti-PescaraThis work presents a morphotectonic map of the Pescara River basin (1:40,000 scale), located in the piedmont-hilly area of the central-eastern Apennines (Abruzzo Region, Italy), and stretching from the eastern slope of the chain (Maiella Massif, Morrone Mt. and Gran Sasso Range) to the Adriatic coast. It is the outcome of an extensive drainage basin-scale geomorphological analysis and incorporates four main sections: orography and hydrography; morphotectonics; azimuthal analysis of the morphotectonic elements; Quaternary fluvial deposits and morphotectonic profiles. The morphotectonic map provides a basis for the study of morphotectonic features at basin-scale, the reconstruction of paleo-landscapes with special regard to drainage network evolution, and the recognition of tectonic control and selective erosion on the landscape. It also contributes to an outline of the main phases of the post-orogenic landscape evolution of the piedmont-hilly area of the Apennines, resulting from the link of alternating morphotectonic and surface processes.http://dx.doi.org/10.1080/17445647.2017.1338204Geomorphological mappingfluvial terraceslongitudinal profilesdrainage evolutionPleistoceneAdriatic piedmont
collection DOAJ
language English
format Article
sources DOAJ
author Tullio Urbano
Tommaso Piacentini
Marcello Buccolini
spellingShingle Tullio Urbano
Tommaso Piacentini
Marcello Buccolini
Morphotectonics of the Pescara River basin (Central Italy)
Journal of Maps
Geomorphological mapping
fluvial terraces
longitudinal profiles
drainage evolution
Pleistocene
Adriatic piedmont
author_facet Tullio Urbano
Tommaso Piacentini
Marcello Buccolini
author_sort Tullio Urbano
title Morphotectonics of the Pescara River basin (Central Italy)
title_short Morphotectonics of the Pescara River basin (Central Italy)
title_full Morphotectonics of the Pescara River basin (Central Italy)
title_fullStr Morphotectonics of the Pescara River basin (Central Italy)
title_full_unstemmed Morphotectonics of the Pescara River basin (Central Italy)
title_sort morphotectonics of the pescara river basin (central italy)
publisher Taylor & Francis Group
series Journal of Maps
issn 1744-5647
publishDate 2017-11-01
description This work presents a morphotectonic map of the Pescara River basin (1:40,000 scale), located in the piedmont-hilly area of the central-eastern Apennines (Abruzzo Region, Italy), and stretching from the eastern slope of the chain (Maiella Massif, Morrone Mt. and Gran Sasso Range) to the Adriatic coast. It is the outcome of an extensive drainage basin-scale geomorphological analysis and incorporates four main sections: orography and hydrography; morphotectonics; azimuthal analysis of the morphotectonic elements; Quaternary fluvial deposits and morphotectonic profiles. The morphotectonic map provides a basis for the study of morphotectonic features at basin-scale, the reconstruction of paleo-landscapes with special regard to drainage network evolution, and the recognition of tectonic control and selective erosion on the landscape. It also contributes to an outline of the main phases of the post-orogenic landscape evolution of the piedmont-hilly area of the Apennines, resulting from the link of alternating morphotectonic and surface processes.
topic Geomorphological mapping
fluvial terraces
longitudinal profiles
drainage evolution
Pleistocene
Adriatic piedmont
url http://dx.doi.org/10.1080/17445647.2017.1338204
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AT marcellobuccolini morphotectonicsofthepescarariverbasincentralitaly
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