Morphometric Analysis and Erosive Features in the Taturi River Basin (PR)
Autor(a) principal: | |
---|---|
Data de Publicação: | 2022 |
Outros Autores: | , |
Tipo de documento: | Artigo |
Idioma: | por |
Título da fonte: | Geografia (Londrina) |
Texto Completo: | https://ojs.uel.br/revistas/uel/index.php/geografia/article/view/42788 |
Resumo: | This work aimed to evaluate the relief features of the Taturi River watershed Paraná state, Brazil, seeking to identify the interrelationship between the lithologies, the linear features linked to fractures and faults, erosive features and types of landforms. For that, the geomorphological mapping of the area and the survey of morphostructural data were cattied out, through the elaboration of the drainage density, dissection depth, slope and lineation maps. The analysis of these maps made it possible to identify different sectors, mostly determined by the lithological variation and by the lineaments. In this way, the hydrographic basin of the Taturi River, despite its low slope morphology, has morphological and, therefore, varied procedural characteristics, wich are linked to lithology and lineaments. Thus, the domain sectors of sandy lithologies present morphologies that indicate greater intensity of erosive processes, which must be considered when using and occupying the land. |
id |
UEL-7_49ce7a794ee3bd2abee9f7e34d4c62db |
---|---|
oai_identifier_str |
oai:ojs.pkp.sfu.ca:article/42788 |
network_acronym_str |
UEL-7 |
network_name_str |
Geografia (Londrina) |
repository_id_str |
|
spelling |
Morphometric Analysis and Erosive Features in the Taturi River Basin (PR)Análisis Morfométrico y Características Erosivas en la Cuenca del Rio Taturi (PR)Análise Morfométrica e Feições Erosivas na Bacia Hidrográfica do Rio Taturi (PR)LithologyGeomorphological featuresFailures.LitologíaCaracterísticas geomorfológicasFallas geológicas.LitologiaFeições geomorfológicasFalhamentos.This work aimed to evaluate the relief features of the Taturi River watershed Paraná state, Brazil, seeking to identify the interrelationship between the lithologies, the linear features linked to fractures and faults, erosive features and types of landforms. For that, the geomorphological mapping of the area and the survey of morphostructural data were cattied out, through the elaboration of the drainage density, dissection depth, slope and lineation maps. The analysis of these maps made it possible to identify different sectors, mostly determined by the lithological variation and by the lineaments. In this way, the hydrographic basin of the Taturi River, despite its low slope morphology, has morphological and, therefore, varied procedural characteristics, wich are linked to lithology and lineaments. Thus, the domain sectors of sandy lithologies present morphologies that indicate greater intensity of erosive processes, which must be considered when using and occupying the land.Este trabajo tuvo como objetivo evaluar los rasgos de relieve de la cuenca del Río Taturi estado de Paraná, Brasil, buscando identificar la interrelación entre las litologías, los rasgos lineales vinculados a fracturas y fallas, los rasgos erosivos y los tipos de accidentes geográficos. Para ello, se realizó el mapeo geomorfológico del área y el levantamiento de datos morfoestructurales, mediante la elaboración de los diagramas de densidad de drenaje, profundidad de disección, pendiente ylineamiento. El análisis de estas letras permitió identificar diferentes sectores, en su mayoría determinados por la variación litológica y por los lineamientos. De esta forma, la cuenca hidrográfica del Río Taturi, a pesar de su morfología de baja pendiente, presenta características morfológicas y, por tanto, procedimentales variadas que están ligadas a la litología y los lineamentos. Así, los sectores de dominio de las litologías arenosas presentan morfologías que indican mayor intensidad de procesos erosivos, los cuales deben ser considerados a la hora de utilizar y ocupar el terreno.Este trabalho teve como objetivo avaliar as feições do relevo da bacia do Rio Taturi (PR), buscando identificar a inter-relação entre as litologias, as feições lineares vinculadas a fraturas e falhas, as feições erosivas e os tipos de forma de relevo. Para isso, foi realizado o mapeamento geomorfológico da área e o levantamento de dados morfoestruturais, por meio da elaboração das cartas de densidade de drenagem, profundidade de dissecação, clinográfica e lineamentos. A análise dessas cartas possibilitou identificar diferentes setores, determinados em sua grande maioria pela variação litológica e pelos lineamentos. Desta maneira, a bacia hidrográfica do Rio Taturi, apesar de sua morfologia de baixo declive, possui características morfológicas e, portanto, processuais, variadas, as quais estão vinculadas à litologia e aos lineamentos. Assim, os setores de domínio de litologias arenosas apresentam morfologias que indicam maior intensidade dos processos erosivos, o que deve ser considerado quando do uso e ocupação da terra.Universidade Estadual de Londrina2022-01-12info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionAvaliado pelos paresapplication/pdfhttps://ojs.uel.br/revistas/uel/index.php/geografia/article/view/4278810.5433/2447-1747.2022v31n1p237GEOGRAFIA (Londrina); v. 31 n. 1 (2022); 237 - 2572447-1747reponame:Geografia (Londrina)instname:Universidade Estadual de Londrina (UEL)instacron:UELporhttps://ojs.uel.br/revistas/uel/index.php/geografia/article/view/42788/30676Copyright (c) 2021 GEOGRAFIA (Londrina)http://creativecommons.org/licenses/by-nc/4.0info:eu-repo/semantics/openAccessBonzanini, Higor LourenzoniLupinacci, Cenira MariaSanches, Rafael Martins2022-09-20T13:06:43Zoai:ojs.pkp.sfu.ca:article/42788Revistahttps://www.uel.br/revistas/uel/index.php/geografiaPUBhttps://www.uel.br/revistas/uel/index.php/geografia/oairevista.geografia.uel@gmail.com||marcar@uel.br||laudi@uel.br2447-17470102-3888opendoar:2022-09-20T13:06:43Geografia (Londrina) - Universidade Estadual de Londrina (UEL)false |
dc.title.none.fl_str_mv |
Morphometric Analysis and Erosive Features in the Taturi River Basin (PR) Análisis Morfométrico y Características Erosivas en la Cuenca del Rio Taturi (PR) Análise Morfométrica e Feições Erosivas na Bacia Hidrográfica do Rio Taturi (PR) |
title |
Morphometric Analysis and Erosive Features in the Taturi River Basin (PR) |
spellingShingle |
Morphometric Analysis and Erosive Features in the Taturi River Basin (PR) Bonzanini, Higor Lourenzoni Lithology Geomorphological features Failures. Litología Características geomorfológicas Fallas geológicas. Litologia Feições geomorfológicas Falhamentos. |
title_short |
Morphometric Analysis and Erosive Features in the Taturi River Basin (PR) |
title_full |
Morphometric Analysis and Erosive Features in the Taturi River Basin (PR) |
title_fullStr |
Morphometric Analysis and Erosive Features in the Taturi River Basin (PR) |
title_full_unstemmed |
Morphometric Analysis and Erosive Features in the Taturi River Basin (PR) |
title_sort |
Morphometric Analysis and Erosive Features in the Taturi River Basin (PR) |
author |
Bonzanini, Higor Lourenzoni |
author_facet |
Bonzanini, Higor Lourenzoni Lupinacci, Cenira Maria Sanches, Rafael Martins |
author_role |
author |
author2 |
Lupinacci, Cenira Maria Sanches, Rafael Martins |
author2_role |
author author |
dc.contributor.author.fl_str_mv |
Bonzanini, Higor Lourenzoni Lupinacci, Cenira Maria Sanches, Rafael Martins |
dc.subject.por.fl_str_mv |
Lithology Geomorphological features Failures. Litología Características geomorfológicas Fallas geológicas. Litologia Feições geomorfológicas Falhamentos. |
topic |
Lithology Geomorphological features Failures. Litología Características geomorfológicas Fallas geológicas. Litologia Feições geomorfológicas Falhamentos. |
description |
This work aimed to evaluate the relief features of the Taturi River watershed Paraná state, Brazil, seeking to identify the interrelationship between the lithologies, the linear features linked to fractures and faults, erosive features and types of landforms. For that, the geomorphological mapping of the area and the survey of morphostructural data were cattied out, through the elaboration of the drainage density, dissection depth, slope and lineation maps. The analysis of these maps made it possible to identify different sectors, mostly determined by the lithological variation and by the lineaments. In this way, the hydrographic basin of the Taturi River, despite its low slope morphology, has morphological and, therefore, varied procedural characteristics, wich are linked to lithology and lineaments. Thus, the domain sectors of sandy lithologies present morphologies that indicate greater intensity of erosive processes, which must be considered when using and occupying the land. |
publishDate |
2022 |
dc.date.none.fl_str_mv |
2022-01-12 |
dc.type.driver.fl_str_mv |
info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion Avaliado pelos pares |
format |
article |
status_str |
publishedVersion |
dc.identifier.uri.fl_str_mv |
https://ojs.uel.br/revistas/uel/index.php/geografia/article/view/42788 10.5433/2447-1747.2022v31n1p237 |
url |
https://ojs.uel.br/revistas/uel/index.php/geografia/article/view/42788 |
identifier_str_mv |
10.5433/2447-1747.2022v31n1p237 |
dc.language.iso.fl_str_mv |
por |
language |
por |
dc.relation.none.fl_str_mv |
https://ojs.uel.br/revistas/uel/index.php/geografia/article/view/42788/30676 |
dc.rights.driver.fl_str_mv |
Copyright (c) 2021 GEOGRAFIA (Londrina) http://creativecommons.org/licenses/by-nc/4.0 info:eu-repo/semantics/openAccess |
rights_invalid_str_mv |
Copyright (c) 2021 GEOGRAFIA (Londrina) http://creativecommons.org/licenses/by-nc/4.0 |
eu_rights_str_mv |
openAccess |
dc.format.none.fl_str_mv |
application/pdf |
dc.publisher.none.fl_str_mv |
Universidade Estadual de Londrina |
publisher.none.fl_str_mv |
Universidade Estadual de Londrina |
dc.source.none.fl_str_mv |
GEOGRAFIA (Londrina); v. 31 n. 1 (2022); 237 - 257 2447-1747 reponame:Geografia (Londrina) instname:Universidade Estadual de Londrina (UEL) instacron:UEL |
instname_str |
Universidade Estadual de Londrina (UEL) |
instacron_str |
UEL |
institution |
UEL |
reponame_str |
Geografia (Londrina) |
collection |
Geografia (Londrina) |
repository.name.fl_str_mv |
Geografia (Londrina) - Universidade Estadual de Londrina (UEL) |
repository.mail.fl_str_mv |
revista.geografia.uel@gmail.com||marcar@uel.br||laudi@uel.br |
_version_ |
1799315432955445248 |