Estudio preliminar de la Geomorfologia de la Cueva del Pindal (Ribadedeva, Oriente de Asturias)

Géomorphologie mapping and structural data provide the preliminary results of the géomorphologie features of the Pindal Cave and surrounding area, described in this work. The landscape results from fluvial, mass wasting, karstic and marine processes, with the outstanding presence of two erosion mari...

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Detalles Bibliográficos
Autores: Jiménez Sánchez, Montserrat, Anadón Ruiz, S., Farias Arquer, Pedro, García Sansegundo, Joaquín, Canto Toimil, N.
Tipo de recurso: artículo
Fecha de publicación:2001
País:España
Institución:Universidad de Huelva (UHU)
Repositorio:Arias Montano. Repositorio Institucional de la Universidad de Huelva
Idioma:español
OAI Identifier:oai:ariasmontano.uhu.es:10272/9467
Acceso en línea:http://hdl.handle.net/10272/9467
Access Level:acceso abierto
Palabra clave:Karst
Cave
Geomorphologic features
Cantabrian Coast
Asturias
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spelling Estudio preliminar de la Geomorfologia de la Cueva del Pindal (Ribadedeva, Oriente de Asturias)Preliminary study of Pindal Cave Geomorphology (Ribadedeva, Eastern Asturias)Jiménez Sánchez, MontserratAnadón Ruiz, S.Farias Arquer, PedroGarcía Sansegundo, JoaquínCanto Toimil, N.KarstCaveGeomorphologic featuresCantabrian CoastAsturiasGéomorphologie mapping and structural data provide the preliminary results of the géomorphologie features of the Pindal Cave and surrounding area, described in this work. The landscape results from fluvial, mass wasting, karstic and marine processes, with the outstanding presence of two erosion marine surfaces called "Rasas": Pimiango (125-170 m) and Pindal (50-64 m). The origin of the Cave, developed in the karstic massif reaching its highest level in Pindal Rasa, is mainly controlled by two fractures trending E-W. The géomorphologie evolution of the Cave is due to 7/ block collapse from the roof related to three joint systems; 21 the episodic infilling by detrital sediment coming from denudation of Pimiango Rasa Range and 3/ the chemical precipitation of speleotheme overlying both alluvial and collapse deposits. The present dynamics of the Cave is controlled by vadose conditions and collapse processes and sporadic flooding of channel inside the cave. A lower active level is inferred from scarps development in deposits over the floor caveSociedad Geológica de España20012001-01-0120012001-01-01journal articlehttp://purl.org/coar/resource_type/c_6501info:eu-repo/semantics/articleapplication/pdfhttp://hdl.handle.net/10272/9467reponame:Arias Montano. Repositorio Institucional de la Universidad de Huelvainstname:Universidad de Huelva (UHU)Españolspaopen accesshttp://purl.org/coar/access_right/c_abf2Atribución-NoComercial-SinDerivadas 3.0 Españahttp://creativecommons.org/licenses/by-nc-nd/3.0/es/info:eu-repo/semantics/openAccessoai:ariasmontano.uhu.es:10272/94672026-06-02T14:58:11Z
dc.title.none.fl_str_mv Estudio preliminar de la Geomorfologia de la Cueva del Pindal (Ribadedeva, Oriente de Asturias)
Preliminary study of Pindal Cave Geomorphology (Ribadedeva, Eastern Asturias)
title Estudio preliminar de la Geomorfologia de la Cueva del Pindal (Ribadedeva, Oriente de Asturias)
spellingShingle Estudio preliminar de la Geomorfologia de la Cueva del Pindal (Ribadedeva, Oriente de Asturias)
Jiménez Sánchez, Montserrat
Karst
Cave
Geomorphologic features
Cantabrian Coast
Asturias
title_short Estudio preliminar de la Geomorfologia de la Cueva del Pindal (Ribadedeva, Oriente de Asturias)
title_full Estudio preliminar de la Geomorfologia de la Cueva del Pindal (Ribadedeva, Oriente de Asturias)
title_fullStr Estudio preliminar de la Geomorfologia de la Cueva del Pindal (Ribadedeva, Oriente de Asturias)
title_full_unstemmed Estudio preliminar de la Geomorfologia de la Cueva del Pindal (Ribadedeva, Oriente de Asturias)
title_sort Estudio preliminar de la Geomorfologia de la Cueva del Pindal (Ribadedeva, Oriente de Asturias)
dc.creator.none.fl_str_mv Jiménez Sánchez, Montserrat
Anadón Ruiz, S.
Farias Arquer, Pedro
García Sansegundo, Joaquín
Canto Toimil, N.
author Jiménez Sánchez, Montserrat
author_facet Jiménez Sánchez, Montserrat
Anadón Ruiz, S.
Farias Arquer, Pedro
García Sansegundo, Joaquín
Canto Toimil, N.
author_role author
author2 Anadón Ruiz, S.
Farias Arquer, Pedro
García Sansegundo, Joaquín
Canto Toimil, N.
author2_role author
author
author
author
dc.contributor.none.fl_str_mv
dc.subject.none.fl_str_mv Karst
Cave
Geomorphologic features
Cantabrian Coast
Asturias
topic Karst
Cave
Geomorphologic features
Cantabrian Coast
Asturias
description Géomorphologie mapping and structural data provide the preliminary results of the géomorphologie features of the Pindal Cave and surrounding area, described in this work. The landscape results from fluvial, mass wasting, karstic and marine processes, with the outstanding presence of two erosion marine surfaces called "Rasas": Pimiango (125-170 m) and Pindal (50-64 m). The origin of the Cave, developed in the karstic massif reaching its highest level in Pindal Rasa, is mainly controlled by two fractures trending E-W. The géomorphologie evolution of the Cave is due to 7/ block collapse from the roof related to three joint systems; 21 the episodic infilling by detrital sediment coming from denudation of Pimiango Rasa Range and 3/ the chemical precipitation of speleotheme overlying both alluvial and collapse deposits. The present dynamics of the Cave is controlled by vadose conditions and collapse processes and sporadic flooding of channel inside the cave. A lower active level is inferred from scarps development in deposits over the floor cave
publishDate 2001
dc.date.none.fl_str_mv 2001
2001-01-01
2001
2001-01-01
dc.type.none.fl_str_mv journal article
http://purl.org/coar/resource_type/c_6501
dc.type.openaire.fl_str_mv info:eu-repo/semantics/article
format article
dc.identifier.none.fl_str_mv http://hdl.handle.net/10272/9467
url http://hdl.handle.net/10272/9467
dc.language.none.fl_str_mv Español
spa
language_invalid_str_mv Español
language spa
dc.rights.none.fl_str_mv open access
http://purl.org/coar/access_right/c_abf2
Atribución-NoComercial-SinDerivadas 3.0 España
http://creativecommons.org/licenses/by-nc-nd/3.0/es/
dc.rights.openaire.fl_str_mv info:eu-repo/semantics/openAccess
rights_invalid_str_mv open access
http://purl.org/coar/access_right/c_abf2
Atribución-NoComercial-SinDerivadas 3.0 España
http://creativecommons.org/licenses/by-nc-nd/3.0/es/
eu_rights_str_mv openAccess
dc.format.none.fl_str_mv application/pdf
dc.publisher.none.fl_str_mv Sociedad Geológica de España
publisher.none.fl_str_mv Sociedad Geológica de España
dc.source.none.fl_str_mv reponame:Arias Montano. Repositorio Institucional de la Universidad de Huelva
instname:Universidad de Huelva (UHU)
instname_str Universidad de Huelva (UHU)
reponame_str Arias Montano. Repositorio Institucional de la Universidad de Huelva
collection Arias Montano. Repositorio Institucional de la Universidad de Huelva
repository.name.fl_str_mv
repository.mail.fl_str_mv
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score 15,811543

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