Morphology and sedimentology of the Itaipú Embayment - Niterói/RJ
Autor(a) principal: | |
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Data de Publicação: | 2002 |
Outros Autores: | |
Tipo de documento: | Artigo |
Idioma: | eng |
Título da fonte: | Anais da Academia Brasileira de Ciências (Online) |
Texto Completo: | http://old.scielo.br/scielo.php?script=sci_arttext&pid=S0001-37652002000100009 |
Resumo: | Bathymetric and sedimentological data from water depths between 3 and 28 meters are the basis of a detailed bathymetric map of the Itaipú Embayment and an understanding of its sedimentary dynamics. Shallower than 16 meters the contours are parallel to the shoreline whereas the morphology of the deeper bottom is influenced by the Menina, Mãe, and Pai islands. Medium sand is prevalent, with local variations in more protected or less protected areas. Minor amount of black mud possibly derives from the Itaipú Lagoon. Siliciclastic granules and pebbles may be relict. The Itaipú Embayments bottom morphology is controlled by stormy waves and the calmer easternmost part of the embayment presents a tendency to accumulate finer sediments. |
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Morphology and sedimentology of the Itaipú Embayment - Niterói/RJcoastal dynamicscoastal sedimentationgeomorphologyquaternaryBathymetric and sedimentological data from water depths between 3 and 28 meters are the basis of a detailed bathymetric map of the Itaipú Embayment and an understanding of its sedimentary dynamics. Shallower than 16 meters the contours are parallel to the shoreline whereas the morphology of the deeper bottom is influenced by the Menina, Mãe, and Pai islands. Medium sand is prevalent, with local variations in more protected or less protected areas. Minor amount of black mud possibly derives from the Itaipú Lagoon. Siliciclastic granules and pebbles may be relict. The Itaipú Embayments bottom morphology is controlled by stormy waves and the calmer easternmost part of the embayment presents a tendency to accumulate finer sediments.Academia Brasileira de Ciências2002-03-01info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersiontext/htmlhttp://old.scielo.br/scielo.php?script=sci_arttext&pid=S0001-37652002000100009Anais da Academia Brasileira de Ciências v.74 n.1 2002reponame:Anais da Academia Brasileira de Ciências (Online)instname:Academia Brasileira de Ciências (ABC)instacron:ABC10.1590/S0001-37652002000100009info:eu-repo/semantics/openAccessSALVADOR,MARCUS VINICIUS S.SILVA,MARIA AUGUSTA M. DAeng2002-05-24T00:00:00Zoai:scielo:S0001-37652002000100009Revistahttp://www.scielo.br/aabchttps://old.scielo.br/oai/scielo-oai.php||aabc@abc.org.br1678-26900001-3765opendoar:2002-05-24T00:00Anais da Academia Brasileira de Ciências (Online) - Academia Brasileira de Ciências (ABC)false |
dc.title.none.fl_str_mv |
Morphology and sedimentology of the Itaipú Embayment - Niterói/RJ |
title |
Morphology and sedimentology of the Itaipú Embayment - Niterói/RJ |
spellingShingle |
Morphology and sedimentology of the Itaipú Embayment - Niterói/RJ SALVADOR,MARCUS VINICIUS S. coastal dynamics coastal sedimentation geomorphology quaternary |
title_short |
Morphology and sedimentology of the Itaipú Embayment - Niterói/RJ |
title_full |
Morphology and sedimentology of the Itaipú Embayment - Niterói/RJ |
title_fullStr |
Morphology and sedimentology of the Itaipú Embayment - Niterói/RJ |
title_full_unstemmed |
Morphology and sedimentology of the Itaipú Embayment - Niterói/RJ |
title_sort |
Morphology and sedimentology of the Itaipú Embayment - Niterói/RJ |
author |
SALVADOR,MARCUS VINICIUS S. |
author_facet |
SALVADOR,MARCUS VINICIUS S. SILVA,MARIA AUGUSTA M. DA |
author_role |
author |
author2 |
SILVA,MARIA AUGUSTA M. DA |
author2_role |
author |
dc.contributor.author.fl_str_mv |
SALVADOR,MARCUS VINICIUS S. SILVA,MARIA AUGUSTA M. DA |
dc.subject.por.fl_str_mv |
coastal dynamics coastal sedimentation geomorphology quaternary |
topic |
coastal dynamics coastal sedimentation geomorphology quaternary |
description |
Bathymetric and sedimentological data from water depths between 3 and 28 meters are the basis of a detailed bathymetric map of the Itaipú Embayment and an understanding of its sedimentary dynamics. Shallower than 16 meters the contours are parallel to the shoreline whereas the morphology of the deeper bottom is influenced by the Menina, Mãe, and Pai islands. Medium sand is prevalent, with local variations in more protected or less protected areas. Minor amount of black mud possibly derives from the Itaipú Lagoon. Siliciclastic granules and pebbles may be relict. The Itaipú Embayments bottom morphology is controlled by stormy waves and the calmer easternmost part of the embayment presents a tendency to accumulate finer sediments. |
publishDate |
2002 |
dc.date.none.fl_str_mv |
2002-03-01 |
dc.type.driver.fl_str_mv |
info:eu-repo/semantics/article |
dc.type.status.fl_str_mv |
info:eu-repo/semantics/publishedVersion |
format |
article |
status_str |
publishedVersion |
dc.identifier.uri.fl_str_mv |
http://old.scielo.br/scielo.php?script=sci_arttext&pid=S0001-37652002000100009 |
url |
http://old.scielo.br/scielo.php?script=sci_arttext&pid=S0001-37652002000100009 |
dc.language.iso.fl_str_mv |
eng |
language |
eng |
dc.relation.none.fl_str_mv |
10.1590/S0001-37652002000100009 |
dc.rights.driver.fl_str_mv |
info:eu-repo/semantics/openAccess |
eu_rights_str_mv |
openAccess |
dc.format.none.fl_str_mv |
text/html |
dc.publisher.none.fl_str_mv |
Academia Brasileira de Ciências |
publisher.none.fl_str_mv |
Academia Brasileira de Ciências |
dc.source.none.fl_str_mv |
Anais da Academia Brasileira de Ciências v.74 n.1 2002 reponame:Anais da Academia Brasileira de Ciências (Online) instname:Academia Brasileira de Ciências (ABC) instacron:ABC |
instname_str |
Academia Brasileira de Ciências (ABC) |
instacron_str |
ABC |
institution |
ABC |
reponame_str |
Anais da Academia Brasileira de Ciências (Online) |
collection |
Anais da Academia Brasileira de Ciências (Online) |
repository.name.fl_str_mv |
Anais da Academia Brasileira de Ciências (Online) - Academia Brasileira de Ciências (ABC) |
repository.mail.fl_str_mv |
||aabc@abc.org.br |
_version_ |
1754302855746945024 |