NATURAL AND ENVIRONMENTAL VULNERABILITIES AT THE CONTACT BETWEEN THE RIO DAS VELHAS PLAIN AND THE SOUTHERN ESPINHAÇO RIDGE, MINAS GERAIS

Detalhes bibliográficos
Autor(a) principal: Couto, Leandro Cosme Oliveira
Data de Publicação: 2018
Outros Autores: Travassos, Luiz Eduardo Panisset
Tipo de documento: Artigo
Idioma: por
Título da fonte: GeoTextos (Online)
Texto Completo: https://periodicos.ufba.br/index.php/geotextos/article/view/26298
Resumo: This research realizes the application of the model, proposed by Jansen (2013), in the landscape in the contact between the Rio das Velhas Plain and the western edge of the Southern Espinhaço Ridge. This area is a representative sample of wide geo-ecological diversity due to its location. The research was based on the concepts of landscape and geosystems of Bertrand (2004), guiding field work of Couto and Travassos (2016), and allowed the model’s application of natural and environmental vulnerabilities. From west to east, from the municipality of Corinto to Diamantina, there is the Rio das Velhas Plain, the Karst of Monjolos, the Serra do Cabral and the Southern Espinhaço Ridge, the latter compartment is made of 03 facies (West Face, Interfluve, and East Face). These geosystems confirm the geo-ecological diversity that exists in the contact between the Rio das Velhas Plain and the western edge of the Southern Espinhaço Ridge. The Karst of Monjolos is the most fragile geosystem and susceptible to impacts, while the Southern Espinhaço Ridge has the most resistant physical attributes with vegetation cover fragile.
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spelling NATURAL AND ENVIRONMENTAL VULNERABILITIES AT THE CONTACT BETWEEN THE RIO DAS VELHAS PLAIN AND THE SOUTHERN ESPINHAÇO RIDGE, MINAS GERAISVulnerabilidades natural e ambiental no contato entre a Planície do Rio das Velhas e a Serra do Espinhaço Meridional, Minas GeraisLandscapeGeosystemsKarstSouthern Espinhaço RidgePaisagemgeossistemacarsteSerra do Espinhaço MeridionalThis research realizes the application of the model, proposed by Jansen (2013), in the landscape in the contact between the Rio das Velhas Plain and the western edge of the Southern Espinhaço Ridge. This area is a representative sample of wide geo-ecological diversity due to its location. The research was based on the concepts of landscape and geosystems of Bertrand (2004), guiding field work of Couto and Travassos (2016), and allowed the model’s application of natural and environmental vulnerabilities. From west to east, from the municipality of Corinto to Diamantina, there is the Rio das Velhas Plain, the Karst of Monjolos, the Serra do Cabral and the Southern Espinhaço Ridge, the latter compartment is made of 03 facies (West Face, Interfluve, and East Face). These geosystems confirm the geo-ecological diversity that exists in the contact between the Rio das Velhas Plain and the western edge of the Southern Espinhaço Ridge. The Karst of Monjolos is the most fragile geosystem and susceptible to impacts, while the Southern Espinhaço Ridge has the most resistant physical attributes with vegetation cover fragile.Este trabalho realiza a aplicação da modelagem, proposta por Jansen (2013), na paisagem do contato entre a planície do Rio das Velhas e a Serra do Espinhaço Meridional. Esta área surge como amostra representativa de ampla diversidade geoecológica em razão de sua localização. O trabalho baseou-se nos conceitos de paisagem e de geossistemas de Bertrand (2004), norteando os trabalhos de campo de Couto e Travassos (2016), e permitiu a aplicação de modelagens de vulnerabilidades natural e ambiental. De oeste para leste, partindo do município de Corinto até Diamantina, tem-se a Planície do Rio das Velhas, o Carste de Monjolos, a Serra do Cabral e a Serra do Espinhaço Meridional, sendo este último compartimento composto por 03 geofácies (Face Oeste, Interflúvio e Face Leste). Estes geossistemas confirmam a diversidade geoecológica existente no contato entre a planície do Rio das Velhas, onde o Carste de Monjolos é o geossistema mais frágil e susceptível a impactos, e a Serra do Espinhaço Meridional, cujos atributos físicos são resistentes, porém a cobertura vegetal é determinante na fragilidade ambiental. Universidade Federal da Bahia2018-07-15info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionapplication/pdfhttps://periodicos.ufba.br/index.php/geotextos/article/view/2629810.9771/geo.v14i1.26298GeoTextos; Vol. 14, N. 1 (julho de 2018)1984-55371809-189Xreponame:GeoTextos (Online)instname:Universidade Federal da Bahia (UFBA)instacron:UFBAporhttps://periodicos.ufba.br/index.php/geotextos/article/view/26298/16409Copyright (c) 2018 Leandro Cosme Oliveira Couto, Luiz Eduardo Panisset Travassosinfo:eu-repo/semantics/openAccessCouto, Leandro Cosme OliveiraTravassos, Luiz Eduardo Panisset2021-12-13T11:50:30Zoai:ojs.periodicos.ufba.br:article/26298Revistahttps://periodicos.ufba.br/index.php/geotextosPUBhttps://periodicos.ufba.br/index.php/geotextos/oaiangeloserpa@hotmail.com||rodrigomei@hotmail.com1984-55371809-189Xopendoar:2021-12-13T11:50:30GeoTextos (Online) - Universidade Federal da Bahia (UFBA)false
dc.title.none.fl_str_mv NATURAL AND ENVIRONMENTAL VULNERABILITIES AT THE CONTACT BETWEEN THE RIO DAS VELHAS PLAIN AND THE SOUTHERN ESPINHAÇO RIDGE, MINAS GERAIS
Vulnerabilidades natural e ambiental no contato entre a Planície do Rio das Velhas e a Serra do Espinhaço Meridional, Minas Gerais
title NATURAL AND ENVIRONMENTAL VULNERABILITIES AT THE CONTACT BETWEEN THE RIO DAS VELHAS PLAIN AND THE SOUTHERN ESPINHAÇO RIDGE, MINAS GERAIS
spellingShingle NATURAL AND ENVIRONMENTAL VULNERABILITIES AT THE CONTACT BETWEEN THE RIO DAS VELHAS PLAIN AND THE SOUTHERN ESPINHAÇO RIDGE, MINAS GERAIS
Couto, Leandro Cosme Oliveira
Landscape
Geosystems
Karst
Southern Espinhaço Ridge
Paisagem
geossistema
carste
Serra do Espinhaço Meridional
title_short NATURAL AND ENVIRONMENTAL VULNERABILITIES AT THE CONTACT BETWEEN THE RIO DAS VELHAS PLAIN AND THE SOUTHERN ESPINHAÇO RIDGE, MINAS GERAIS
title_full NATURAL AND ENVIRONMENTAL VULNERABILITIES AT THE CONTACT BETWEEN THE RIO DAS VELHAS PLAIN AND THE SOUTHERN ESPINHAÇO RIDGE, MINAS GERAIS
title_fullStr NATURAL AND ENVIRONMENTAL VULNERABILITIES AT THE CONTACT BETWEEN THE RIO DAS VELHAS PLAIN AND THE SOUTHERN ESPINHAÇO RIDGE, MINAS GERAIS
title_full_unstemmed NATURAL AND ENVIRONMENTAL VULNERABILITIES AT THE CONTACT BETWEEN THE RIO DAS VELHAS PLAIN AND THE SOUTHERN ESPINHAÇO RIDGE, MINAS GERAIS
title_sort NATURAL AND ENVIRONMENTAL VULNERABILITIES AT THE CONTACT BETWEEN THE RIO DAS VELHAS PLAIN AND THE SOUTHERN ESPINHAÇO RIDGE, MINAS GERAIS
author Couto, Leandro Cosme Oliveira
author_facet Couto, Leandro Cosme Oliveira
Travassos, Luiz Eduardo Panisset
author_role author
author2 Travassos, Luiz Eduardo Panisset
author2_role author
dc.contributor.author.fl_str_mv Couto, Leandro Cosme Oliveira
Travassos, Luiz Eduardo Panisset
dc.subject.por.fl_str_mv Landscape
Geosystems
Karst
Southern Espinhaço Ridge
Paisagem
geossistema
carste
Serra do Espinhaço Meridional
topic Landscape
Geosystems
Karst
Southern Espinhaço Ridge
Paisagem
geossistema
carste
Serra do Espinhaço Meridional
description This research realizes the application of the model, proposed by Jansen (2013), in the landscape in the contact between the Rio das Velhas Plain and the western edge of the Southern Espinhaço Ridge. This area is a representative sample of wide geo-ecological diversity due to its location. The research was based on the concepts of landscape and geosystems of Bertrand (2004), guiding field work of Couto and Travassos (2016), and allowed the model’s application of natural and environmental vulnerabilities. From west to east, from the municipality of Corinto to Diamantina, there is the Rio das Velhas Plain, the Karst of Monjolos, the Serra do Cabral and the Southern Espinhaço Ridge, the latter compartment is made of 03 facies (West Face, Interfluve, and East Face). These geosystems confirm the geo-ecological diversity that exists in the contact between the Rio das Velhas Plain and the western edge of the Southern Espinhaço Ridge. The Karst of Monjolos is the most fragile geosystem and susceptible to impacts, while the Southern Espinhaço Ridge has the most resistant physical attributes with vegetation cover fragile.
publishDate 2018
dc.date.none.fl_str_mv 2018-07-15
dc.type.driver.fl_str_mv info:eu-repo/semantics/article
info:eu-repo/semantics/publishedVersion
format article
status_str publishedVersion
dc.identifier.uri.fl_str_mv https://periodicos.ufba.br/index.php/geotextos/article/view/26298
10.9771/geo.v14i1.26298
url https://periodicos.ufba.br/index.php/geotextos/article/view/26298
identifier_str_mv 10.9771/geo.v14i1.26298
dc.language.iso.fl_str_mv por
language por
dc.relation.none.fl_str_mv https://periodicos.ufba.br/index.php/geotextos/article/view/26298/16409
dc.rights.driver.fl_str_mv Copyright (c) 2018 Leandro Cosme Oliveira Couto, Luiz Eduardo Panisset Travassos
info:eu-repo/semantics/openAccess
rights_invalid_str_mv Copyright (c) 2018 Leandro Cosme Oliveira Couto, Luiz Eduardo Panisset Travassos
eu_rights_str_mv openAccess
dc.format.none.fl_str_mv application/pdf
dc.publisher.none.fl_str_mv Universidade Federal da Bahia
publisher.none.fl_str_mv Universidade Federal da Bahia
dc.source.none.fl_str_mv GeoTextos; Vol. 14, N. 1 (julho de 2018)
1984-5537
1809-189X
reponame:GeoTextos (Online)
instname:Universidade Federal da Bahia (UFBA)
instacron:UFBA
instname_str Universidade Federal da Bahia (UFBA)
instacron_str UFBA
institution UFBA
reponame_str GeoTextos (Online)
collection GeoTextos (Online)
repository.name.fl_str_mv GeoTextos (Online) - Universidade Federal da Bahia (UFBA)
repository.mail.fl_str_mv angeloserpa@hotmail.com||rodrigomei@hotmail.com
_version_ 1797221575977598976

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