Evidencias morfogenéticas cuaternarias en el karst de la Sierra del Endrinal (Grazalema, Cádiz)

The geomorphological observations made until now reveal a long morphogenic history for the karst of the Eridrinal: mountains; going back to pre-Quaternary times. The erosion surfaces mapped (Sl, S2 and 53) have å biostatic genesis and are linked to humid media with forest cover, favouring carbonatio...

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Detalles Bibliográficos
Autores: Rodríguez Vidal, Joaquín, Álvarez, G., Cáceres Puro, Luis Miguel, Martínez Aguirre, Arancha, Alcázar, J. M.
Tipo de recurso: artículo
Fecha de publicación:1997
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:10272/18065
Acceso en línea:http://hdl.handle.net/10272/18065
Access Level:acceso abierto
Palabra clave:Karst
Quaternary
Geomorphology
U/Th dating
Betic Range
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spelling Evidencias morfogenéticas cuaternarias en el karst de la Sierra del Endrinal (Grazalema, Cádiz)Quaternary morphogenic features in the Endrinal mountains (Grazalema, SW Spain)Rodríguez Vidal, JoaquínÁlvarez, G.Cáceres Puro, Luis MiguelMartínez Aguirre, AranchaAlcázar, J. M.KarstQuaternaryGeomorphologyU/Th datingBetic RangeThe geomorphological observations made until now reveal a long morphogenic history for the karst of the Eridrinal: mountains; going back to pre-Quaternary times. The erosion surfaces mapped (Sl, S2 and 53) have å biostatic genesis and are linked to humid media with forest cover, favouring carbonation below a karst- cover. The rëlatiônship between speleothems and geomorphology seems to indicate that surfaces 1 and 2 are basal surfaceS of weathering, with biostatic genesis, which would remain active from at least 300 ky BP (Middle Pleistocene), with a petibd of intense carbonation during the isotopic (cold) state 6 between 190 and 140 ky BR Surface 3, of retent genësiS (Late. Pleistócene to Holocene), is the result of a general biostatic situation, with Climatic and anthopögenic rhexistatic disturbances that have movilized, under the action of water flow ånd gravity, the detPitús and regoliths generated in previous. epochs. Regional palaeoenvironmental indicators show a climatic change towards greater aridity during the transition from Middle to Late PleistôceneSociedad Geológica de España19971997-01-0119971997-01-01journal articlehttp://purl.org/coar/resource_type/c_6501info:eu-repo/semantics/articleapplication/pdfhttp://hdl.handle.net/10272/18065reponame: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:10272/180652026-06-02T14:58:11Z
dc.title.none.fl_str_mv Evidencias morfogenéticas cuaternarias en el karst de la Sierra del Endrinal (Grazalema, Cádiz)
Quaternary morphogenic features in the Endrinal mountains (Grazalema, SW Spain)
title Evidencias morfogenéticas cuaternarias en el karst de la Sierra del Endrinal (Grazalema, Cádiz)
spellingShingle Evidencias morfogenéticas cuaternarias en el karst de la Sierra del Endrinal (Grazalema, Cádiz)
Rodríguez Vidal, Joaquín
Karst
Quaternary
Geomorphology
U/Th dating
Betic Range
title_short Evidencias morfogenéticas cuaternarias en el karst de la Sierra del Endrinal (Grazalema, Cádiz)
title_full Evidencias morfogenéticas cuaternarias en el karst de la Sierra del Endrinal (Grazalema, Cádiz)
title_fullStr Evidencias morfogenéticas cuaternarias en el karst de la Sierra del Endrinal (Grazalema, Cádiz)
title_full_unstemmed Evidencias morfogenéticas cuaternarias en el karst de la Sierra del Endrinal (Grazalema, Cádiz)
title_sort Evidencias morfogenéticas cuaternarias en el karst de la Sierra del Endrinal (Grazalema, Cádiz)
dc.creator.none.fl_str_mv Rodríguez Vidal, Joaquín
Álvarez, G.
Cáceres Puro, Luis Miguel
Martínez Aguirre, Arancha
Alcázar, J. M.
author Rodríguez Vidal, Joaquín
author_facet Rodríguez Vidal, Joaquín
Álvarez, G.
Cáceres Puro, Luis Miguel
Martínez Aguirre, Arancha
Alcázar, J. M.
author_role author
author2 Álvarez, G.
Cáceres Puro, Luis Miguel
Martínez Aguirre, Arancha
Alcázar, J. M.
author2_role author
author
author
author
dc.contributor.none.fl_str_mv
dc.subject.none.fl_str_mv Karst
Quaternary
Geomorphology
U/Th dating
Betic Range
topic Karst
Quaternary
Geomorphology
U/Th dating
Betic Range
description The geomorphological observations made until now reveal a long morphogenic history for the karst of the Eridrinal: mountains; going back to pre-Quaternary times. The erosion surfaces mapped (Sl, S2 and 53) have å biostatic genesis and are linked to humid media with forest cover, favouring carbonation below a karst- cover. The rëlatiônship between speleothems and geomorphology seems to indicate that surfaces 1 and 2 are basal surfaceS of weathering, with biostatic genesis, which would remain active from at least 300 ky BP (Middle Pleistocene), with a petibd of intense carbonation during the isotopic (cold) state 6 between 190 and 140 ky BR Surface 3, of retent genësiS (Late. Pleistócene to Holocene), is the result of a general biostatic situation, with Climatic and anthopögenic rhexistatic disturbances that have movilized, under the action of water flow ånd gravity, the detPitús and regoliths generated in previous. epochs. Regional palaeoenvironmental indicators show a climatic change towards greater aridity during the transition from Middle to Late Pleistôcene
publishDate 1997
dc.date.none.fl_str_mv 1997
1997-01-01
1997
1997-01-01
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/10272/18065
url http://hdl.handle.net/10272/18065
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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