Augen gneiss: the more carioca of the rocks

Detalhes bibliográficos
Autor(a) principal: Mansur, Kátia Leite
Data de Publicação: 2008
Outros Autores: Carvalho, Ismar Souza, Delphim, Carlos Fernando Moura, Barroso, Emilio Velloso
Tipo de documento: Artigo
Idioma: por
Título da fonte: Anuário do Instituto de Geociências (Online)
Texto Completo: https://revistas.ufrj.br/index.php/aigeo/article/view/6782
Resumo: The city of Rio de Janeiro is known by its natural beauties. The mountains and the sea make the city the postcard of Brazil. The sculpture of the carioca landscape is closely related to the augen gneiss, very resistant rock to the weathering and, for this reason, it stands out in the relief. It gives form for Sugar Loaf and Corcovado, for example. Augen gneiss was used in the construction of most of the historical buildings of the city, including museums and churches, many of them were built in the 19th century. It was used in the sculpture of ornaments, facades and frames of doors and windows. The exploitation of the augen gneiss was presented by Jean Baptiste Debret in his book "Voyage Pittoresque et Historique au Brésil". A picture of quarry is presented at Morro da Glória and describes the extraction method by slave labor. He informes that the augen gneiss is softer, less expensive and more easily exploited. It was destined, mainly, to the parts of the buildings that should be sculpted. This rock is still present in an important event of the history of the brazilian arts. Pedra do Sal, a stairway sculpted in the augen gneiss Downtown, was the place that African people met in the past to tell their histories, to do religious cults and to sing. In these meetings in Pedra do Sal samba was born
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spelling Augen gneiss: the more carioca of the rocksO gnaisse facoidal: a mais carioca das rochasThe city of Rio de Janeiro is known by its natural beauties. The mountains and the sea make the city the postcard of Brazil. The sculpture of the carioca landscape is closely related to the augen gneiss, very resistant rock to the weathering and, for this reason, it stands out in the relief. It gives form for Sugar Loaf and Corcovado, for example. Augen gneiss was used in the construction of most of the historical buildings of the city, including museums and churches, many of them were built in the 19th century. It was used in the sculpture of ornaments, facades and frames of doors and windows. The exploitation of the augen gneiss was presented by Jean Baptiste Debret in his book "Voyage Pittoresque et Historique au Brésil". A picture of quarry is presented at Morro da Glória and describes the extraction method by slave labor. He informes that the augen gneiss is softer, less expensive and more easily exploited. It was destined, mainly, to the parts of the buildings that should be sculpted. This rock is still present in an important event of the history of the brazilian arts. Pedra do Sal, a stairway sculpted in the augen gneiss Downtown, was the place that African people met in the past to tell their histories, to do religious cults and to sing. In these meetings in Pedra do Sal samba was bornA cidade do Rio de Janeiro é conhecida por suas belezas naturais. Montanhas que mergulham no mar fazem da cidade um cartão postal do Brasil que em conjunto com o espírito solidário e alegre de seu povo, proporcionaram-lhe o título de Cidade Maravilhosa. O que se pretende com este trabalho é demonstrar a importância da geologia, por meio de um tipo específico de rocha, o gnaisse facoidal, na construção da cidade e dos aspectos culturais que moldaram seu povo e transformaram sua paisagem em um ícone turístico para o país. A paisagem carioca que encanta a todos, desde os naturalistas que visitaram o Brasil nos séculos XVIII e XIX até o turista de hoje, está intimamente relacionada ao gnaisse facoidal, rocha ortoderivada bastante resistente ao intemperismo e que, por este motivo, se sobressai no relevo, dando forma ao Pão de Açúcar e ao Corcovado, por exemplo. Foi usado na construção de grande parte dos monumentos históricos da cidade na forma de ornamentos, fachadas e molduras de portas e janelas, bem como do meio-fio da parte mais antiga da cidade. O uso do gnaisse facoidal na cantaria foi descrito por Jean Baptiste Debret em seu livro "Viagem Pitoresca e Histórica ao Brasil", onde explica que ele é mais macio, menos caro e facilmente explorável, destinando-se às partes dos edifícios que deveriam ser esculpidas. Esta rocha está presente, ainda, em um importante marco da história das artes brasileiras. Foi na Pedra do Sal, escada esculpida no gnaisse facoidal, que os negros se reuniam para contar histórias, realizar cultos religiosos e cantar. Destas reuniões na Pedra do Sal nasceu o sambaUniversidade Federal do Rio de Janeiro2008-12-01info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionapplication/pdfhttps://revistas.ufrj.br/index.php/aigeo/article/view/678210.11137/2008_2_9-22Anuário do Instituto de Geociências; Vol 31, No 2 (2008); 9-22Anuário do Instituto de Geociências; Vol 31, No 2 (2008); 9-221982-39080101-9759reponame:Anuário do Instituto de Geociências (Online)instname:Universidade Federal do Rio de Janeiro (UFRJ)instacron:UFRJporhttps://revistas.ufrj.br/index.php/aigeo/article/view/6782/5379Copyright (c) 2008 Anuário do Instituto de Geociênciashttp://creativecommons.org/licenses/by/4.0info:eu-repo/semantics/openAccessMansur, Kátia LeiteCarvalho, Ismar SouzaDelphim, Carlos Fernando MouraBarroso, Emilio Velloso2017-01-23T21:49:09Zoai:www.revistas.ufrj.br:article/6782Revistahttps://revistas.ufrj.br/index.php/aigeo/indexPUBhttps://revistas.ufrj.br/index.php/aigeo/oaianuario@igeo.ufrj.br||1982-39080101-9759opendoar:2017-01-23T21:49:09Anuário do Instituto de Geociências (Online) - Universidade Federal do Rio de Janeiro (UFRJ)false
dc.title.none.fl_str_mv Augen gneiss: the more carioca of the rocks
O gnaisse facoidal: a mais carioca das rochas
title Augen gneiss: the more carioca of the rocks
spellingShingle Augen gneiss: the more carioca of the rocks
Mansur, Kátia Leite
title_short Augen gneiss: the more carioca of the rocks
title_full Augen gneiss: the more carioca of the rocks
title_fullStr Augen gneiss: the more carioca of the rocks
title_full_unstemmed Augen gneiss: the more carioca of the rocks
title_sort Augen gneiss: the more carioca of the rocks
author Mansur, Kátia Leite
author_facet Mansur, Kátia Leite
Carvalho, Ismar Souza
Delphim, Carlos Fernando Moura
Barroso, Emilio Velloso
author_role author
author2 Carvalho, Ismar Souza
Delphim, Carlos Fernando Moura
Barroso, Emilio Velloso
author2_role author
author
author
dc.contributor.author.fl_str_mv Mansur, Kátia Leite
Carvalho, Ismar Souza
Delphim, Carlos Fernando Moura
Barroso, Emilio Velloso
description The city of Rio de Janeiro is known by its natural beauties. The mountains and the sea make the city the postcard of Brazil. The sculpture of the carioca landscape is closely related to the augen gneiss, very resistant rock to the weathering and, for this reason, it stands out in the relief. It gives form for Sugar Loaf and Corcovado, for example. Augen gneiss was used in the construction of most of the historical buildings of the city, including museums and churches, many of them were built in the 19th century. It was used in the sculpture of ornaments, facades and frames of doors and windows. The exploitation of the augen gneiss was presented by Jean Baptiste Debret in his book "Voyage Pittoresque et Historique au Brésil". A picture of quarry is presented at Morro da Glória and describes the extraction method by slave labor. He informes that the augen gneiss is softer, less expensive and more easily exploited. It was destined, mainly, to the parts of the buildings that should be sculpted. This rock is still present in an important event of the history of the brazilian arts. Pedra do Sal, a stairway sculpted in the augen gneiss Downtown, was the place that African people met in the past to tell their histories, to do religious cults and to sing. In these meetings in Pedra do Sal samba was born
publishDate 2008
dc.date.none.fl_str_mv 2008-12-01
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10.11137/2008_2_9-22
url https://revistas.ufrj.br/index.php/aigeo/article/view/6782
identifier_str_mv 10.11137/2008_2_9-22
dc.language.iso.fl_str_mv por
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dc.relation.none.fl_str_mv https://revistas.ufrj.br/index.php/aigeo/article/view/6782/5379
dc.rights.driver.fl_str_mv Copyright (c) 2008 Anuário do Instituto de Geociências
http://creativecommons.org/licenses/by/4.0
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rights_invalid_str_mv Copyright (c) 2008 Anuário do Instituto de Geociências
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dc.format.none.fl_str_mv application/pdf
dc.publisher.none.fl_str_mv Universidade Federal do Rio de Janeiro
publisher.none.fl_str_mv Universidade Federal do Rio de Janeiro
dc.source.none.fl_str_mv Anuário do Instituto de Geociências; Vol 31, No 2 (2008); 9-22
Anuário do Instituto de Geociências; Vol 31, No 2 (2008); 9-22
1982-3908
0101-9759
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