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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Online Access: | http://dx.doi.org/10.1080/17445647.2017.1338204 |
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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 |
work_keys_str_mv |
AT tulliourbano morphotectonicsofthepescarariverbasincentralitaly AT tommasopiacentini morphotectonicsofthepescarariverbasincentralitaly AT marcellobuccolini morphotectonicsofthepescarariverbasincentralitaly |
_version_ |
1724952475648131072 |