Geomorphological analysis of the cuesta-peripheral depression: Case study of the Passa Cinco river watershed

Registro completo de metadados
MetadadosDescriçãoIdioma
Autor(es): dc.contributorUniversidade Estadual Paulista (Unesp)-
Autor(es): dc.creatorde Souza, Tissiana de Almeida [UNESP]-
Autor(es): dc.creatorde Andrade, Rafael Vilela [UNESP]-
Autor(es): dc.creatorLupinacci, Cenira Maria [UNESP]-
Data de aceite: dc.date.accessioned2022-02-22T00:45:23Z-
Data de disponibilização: dc.date.available2022-02-22T00:45:23Z-
Data de envio: dc.date.issued2021-06-25-
Data de envio: dc.date.issued2021-06-25-
Data de envio: dc.date.issued2019-12-31-
Fonte completa do material: dc.identifierhttp://dx.doi.org/10.26848/rbgf.v13.2.p465-486-
Fonte completa do material: dc.identifierhttp://hdl.handle.net/11449/205815-
Fonte: dc.identifier.urihttp://educapes.capes.gov.br/handle/11449/205815-
Descrição: dc.descriptionA B S T R A C T The relief of São Paulo is characterized by the presence of long cuesta, whose origin causes discussion until the present day. Thus, the objective of this research is to analyze the morphostructural characteristics of the Passa Cinco River watershed, situated at transition zone of Cuestas-Peripheral Depression, constituting significative example of this relief system, taking in consideration the complexity of existing forms, that include extense continuous cuesta scarp and buttes of different sizes, extensions and characteristics. The data to analyze the study area were obtained through the integrated interpretation of the Geomorphological, Declivity, Drainage Density, Depth of Drainage and Lineation maps, in 1:50.000 scale. Beyond circumdenudation, considered the classic process of origin of these two relief macrocompartments, tectonic factors also need to be evaluated in order to have a better understanding of these relief forms. These factors are responsible for the acceleration of erosive processes promoted by river courses in some sectors, collaborating with the circumdenudation process, as with the local variation of the Cuesta Front and buttes. Thus, it is understood that the technical procedures allowed to obtain data that demonstrate the complexity involved in the elaboration of the relief in this transition sector, being able to be extended to others areas of the interior of the state of São Paulo with this same relief characteristics.-
Descrição: dc.descriptionConselho Nacional de Desenvolvimento Científico e Tecnológico (CNPq)-
Descrição: dc.descriptionFundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP)-
Descrição: dc.descriptionUNESP Campus de Rio Claro, Avenida 24A n. 1515-
Descrição: dc.descriptionUNESP Campus de Rio Claro, Avenida 24A n. 1515-
Descrição: dc.descriptionCNPq: 155332/2016-3-
Descrição: dc.descriptionFAPESP: 2016/25231-1-
Formato: dc.format465-486-
Idioma: dc.languagept_BR-
Relação: dc.relationRevista Brasileira de Geografia Fisica-
???dc.source???: dc.sourceScopus-
Palavras-chave: dc.subjectDeclivity-
Palavras-chave: dc.subjectDepth of drainage-
Palavras-chave: dc.subjectDrainage density-
Palavras-chave: dc.subjectLineation-
Título: dc.titleGeomorphological analysis of the cuesta-peripheral depression: Case study of the Passa Cinco river watershed-
Título: dc.titleAnálise geomorfológica da transição cuestas-depressão periférica: A alta bacia do rio Passa Cinco(SP) como estudo de caso-
Tipo de arquivo: dc.typelivro digital-
Aparece nas coleções:Repositório Institucional - Unesp

Não existem arquivos associados a este item.