Geomorphology of fluvial deposits in the middle Tocantins River, eastern Amazon

This paper presents the geomorphological mapping at a 1:100,000 scale of fluvial deposits in the middle Tocantins River. The region preserves an important sedimentary archive of environmental changes of the Amazon and Cerrado biomes. Yet, the region is under influence of diverse anthropogenic activi...

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Main Authors: Jandessa Silva de Jesus, Fabiano do Nascimento Pupim, André Oliveira Sawakuchi, Leonardo Brasil Felipe
Format: Article
Language:English
Published: Taylor & Francis Group 2020-12-01
Series:Journal of Maps
Subjects:
Online Access:http://dx.doi.org/10.1080/17445647.2020.1822938
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spelling doaj-e21c5281fac14525878bc8c8f2f87b8d2021-01-15T13:32:55ZengTaylor & Francis GroupJournal of Maps1744-56472020-12-0116271072310.1080/17445647.2020.18229381822938Geomorphology of fluvial deposits in the middle Tocantins River, eastern AmazonJandessa Silva de Jesus0Fabiano do Nascimento Pupim1André Oliveira Sawakuchi2Leonardo Brasil Felipe3Institute of Geosciences, Universidade de São PauloInstitute of Geosciences, Universidade de São PauloInstitute of Geosciences, Universidade de São PauloInstitute of Geosciences and Engineering, Universidade Federal do Sul e Sudeste do ParáThis paper presents the geomorphological mapping at a 1:100,000 scale of fluvial deposits in the middle Tocantins River. The region preserves an important sedimentary archive of environmental changes of the Amazon and Cerrado biomes. Yet, the region is under influence of diverse anthropogenic activities, including planned or operational hydropower plants, and detailed geomorphological mapping is lacking. The mapping combined interpretation of surface geomorphic features, morphometric analysis, and field surveys. Three main geomorphic units were defined: (i) fluvial plain, (ii) fluvial terraces, and (iii) paleo-alluvial fans. The detailed mapping survey allowed a hierarchical organization of geomorphological units as well as their relative chronology of formation. Our results improve the understanding on the complex geomorphological processes which shape the current fluvial landscape. Specifically, improving the understanding of the Tocantins River floodplains is crucial to support conservation of flooded forests, sustainable use of natural resources and minimize socio-economic losses and damages.http://dx.doi.org/10.1080/17445647.2020.1822938fluvial geomorphologygeomorphological mappingdigital elevation modeltocantins rivermarabá
collection DOAJ
language English
format Article
sources DOAJ
author Jandessa Silva de Jesus
Fabiano do Nascimento Pupim
André Oliveira Sawakuchi
Leonardo Brasil Felipe
spellingShingle Jandessa Silva de Jesus
Fabiano do Nascimento Pupim
André Oliveira Sawakuchi
Leonardo Brasil Felipe
Geomorphology of fluvial deposits in the middle Tocantins River, eastern Amazon
Journal of Maps
fluvial geomorphology
geomorphological mapping
digital elevation model
tocantins river
marabá
author_facet Jandessa Silva de Jesus
Fabiano do Nascimento Pupim
André Oliveira Sawakuchi
Leonardo Brasil Felipe
author_sort Jandessa Silva de Jesus
title Geomorphology of fluvial deposits in the middle Tocantins River, eastern Amazon
title_short Geomorphology of fluvial deposits in the middle Tocantins River, eastern Amazon
title_full Geomorphology of fluvial deposits in the middle Tocantins River, eastern Amazon
title_fullStr Geomorphology of fluvial deposits in the middle Tocantins River, eastern Amazon
title_full_unstemmed Geomorphology of fluvial deposits in the middle Tocantins River, eastern Amazon
title_sort geomorphology of fluvial deposits in the middle tocantins river, eastern amazon
publisher Taylor & Francis Group
series Journal of Maps
issn 1744-5647
publishDate 2020-12-01
description This paper presents the geomorphological mapping at a 1:100,000 scale of fluvial deposits in the middle Tocantins River. The region preserves an important sedimentary archive of environmental changes of the Amazon and Cerrado biomes. Yet, the region is under influence of diverse anthropogenic activities, including planned or operational hydropower plants, and detailed geomorphological mapping is lacking. The mapping combined interpretation of surface geomorphic features, morphometric analysis, and field surveys. Three main geomorphic units were defined: (i) fluvial plain, (ii) fluvial terraces, and (iii) paleo-alluvial fans. The detailed mapping survey allowed a hierarchical organization of geomorphological units as well as their relative chronology of formation. Our results improve the understanding on the complex geomorphological processes which shape the current fluvial landscape. Specifically, improving the understanding of the Tocantins River floodplains is crucial to support conservation of flooded forests, sustainable use of natural resources and minimize socio-economic losses and damages.
topic fluvial geomorphology
geomorphological mapping
digital elevation model
tocantins river
marabá
url http://dx.doi.org/10.1080/17445647.2020.1822938
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