Estudo geoarqueológico dos sítios do Rodo, Vau e Bispeira 8

Detalhes bibliográficos
Autor(a) principal: Monteiro-Rodrigues, Sérgio
Data de Publicação: 2020
Outros Autores: Gomes, António Alberto
Tipo de documento: Livro
Idioma: por
Título da fonte: Repositório Científico de Acesso Aberto de Portugal (Repositórios Cientìficos)
Texto Completo: https://hdl.handle.net/10216/134250
Resumo: The geoarchaeological studies carried out at Rodo, Vau and Bispeira 8 allowed to the recognition of three archaeological contexts associated with slope deposits that, in the first two cases, cover the surface of Pleistocene fluvial terraces, respectively, of the Vouga river and the Teixeira river. The slope deposits were controlled by small basins located at the top of the hills in the vicinity of the sites. Still with regard to Rodo and Vau, the main stage of slope erosion seems to coincide with the paleoclimatic event known as Dryas III. However, absolute dating and archaeological data showed that erosion also occurred after the Pleistocene. At Vau, Upper Paleolithic occupations were identified associated with flood deposits of the Teixeira river. More recent occupations are connected with local holocene colluvia. At Rodo, the main archaeological remains also date from the Upper Paleolithic, but the possibility of the existence of later occupations is not ruled out. At Bispeira 8, the remains of the human presence are less abundant and date mainly of the Upper Paleolithic and the Middle/Late Neolithic.
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spelling Estudo geoarqueológico dos sítios do Rodo, Vau e Bispeira 8GeografiaGeographyThe geoarchaeological studies carried out at Rodo, Vau and Bispeira 8 allowed to the recognition of three archaeological contexts associated with slope deposits that, in the first two cases, cover the surface of Pleistocene fluvial terraces, respectively, of the Vouga river and the Teixeira river. The slope deposits were controlled by small basins located at the top of the hills in the vicinity of the sites. Still with regard to Rodo and Vau, the main stage of slope erosion seems to coincide with the paleoclimatic event known as Dryas III. However, absolute dating and archaeological data showed that erosion also occurred after the Pleistocene. At Vau, Upper Paleolithic occupations were identified associated with flood deposits of the Teixeira river. More recent occupations are connected with local holocene colluvia. At Rodo, the main archaeological remains also date from the Upper Paleolithic, but the possibility of the existence of later occupations is not ruled out. At Bispeira 8, the remains of the human presence are less abundant and date mainly of the Upper Paleolithic and the Middle/Late Neolithic.20202020-01-01T00:00:00Zinfo:eu-repo/semantics/publishedVersioninfo:eu-repo/semantics/bookapplication/pdfhttps://hdl.handle.net/10216/134250porMonteiro-Rodrigues, SérgioGomes, António Albertoinfo:eu-repo/semantics/openAccessreponame:Repositório Científico de Acesso Aberto de Portugal (Repositórios Cientìficos)instname:Agência para a Sociedade do Conhecimento (UMIC) - FCT - Sociedade da Informaçãoinstacron:RCAAP2023-11-29T13:30:46Zoai:repositorio-aberto.up.pt:10216/134250Portal AgregadorONGhttps://www.rcaap.pt/oai/openaireopendoar:71602024-03-19T23:41:45.827130Repositório Científico de Acesso Aberto de Portugal (Repositórios Cientìficos) - Agência para a Sociedade do Conhecimento (UMIC) - FCT - Sociedade da Informaçãofalse
dc.title.none.fl_str_mv Estudo geoarqueológico dos sítios do Rodo, Vau e Bispeira 8
title Estudo geoarqueológico dos sítios do Rodo, Vau e Bispeira 8
spellingShingle Estudo geoarqueológico dos sítios do Rodo, Vau e Bispeira 8
Monteiro-Rodrigues, Sérgio
Geografia
Geography
title_short Estudo geoarqueológico dos sítios do Rodo, Vau e Bispeira 8
title_full Estudo geoarqueológico dos sítios do Rodo, Vau e Bispeira 8
title_fullStr Estudo geoarqueológico dos sítios do Rodo, Vau e Bispeira 8
title_full_unstemmed Estudo geoarqueológico dos sítios do Rodo, Vau e Bispeira 8
title_sort Estudo geoarqueológico dos sítios do Rodo, Vau e Bispeira 8
author Monteiro-Rodrigues, Sérgio
author_facet Monteiro-Rodrigues, Sérgio
Gomes, António Alberto
author_role author
author2 Gomes, António Alberto
author2_role author
dc.contributor.author.fl_str_mv Monteiro-Rodrigues, Sérgio
Gomes, António Alberto
dc.subject.por.fl_str_mv Geografia
Geography
topic Geografia
Geography
description The geoarchaeological studies carried out at Rodo, Vau and Bispeira 8 allowed to the recognition of three archaeological contexts associated with slope deposits that, in the first two cases, cover the surface of Pleistocene fluvial terraces, respectively, of the Vouga river and the Teixeira river. The slope deposits were controlled by small basins located at the top of the hills in the vicinity of the sites. Still with regard to Rodo and Vau, the main stage of slope erosion seems to coincide with the paleoclimatic event known as Dryas III. However, absolute dating and archaeological data showed that erosion also occurred after the Pleistocene. At Vau, Upper Paleolithic occupations were identified associated with flood deposits of the Teixeira river. More recent occupations are connected with local holocene colluvia. At Rodo, the main archaeological remains also date from the Upper Paleolithic, but the possibility of the existence of later occupations is not ruled out. At Bispeira 8, the remains of the human presence are less abundant and date mainly of the Upper Paleolithic and the Middle/Late Neolithic.
publishDate 2020
dc.date.none.fl_str_mv 2020
2020-01-01T00:00:00Z
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url https://hdl.handle.net/10216/134250
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reponame_str Repositório Científico de Acesso Aberto de Portugal (Repositórios Cientìficos)
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repository.name.fl_str_mv Repositório Científico de Acesso Aberto de Portugal (Repositórios Cientìficos) - Agência para a Sociedade do Conhecimento (UMIC) - FCT - Sociedade da Informação
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