Glacial geomorphology of the High Gredos Massif: Gredos and Pinar valleys (Iberian Central System, Spain)

We present a detailed geomorphological map of the landform assemblages originated by the two major paleoglaciers of the Sierra de Gredos mountain range in the Spanish Iberian Central System. Based on previous works, our map focused on the features formed by Gredos and Pinar paleoglaciers during the...

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Autores: Carrasco, Rosa M., Soteres, Rodrigo L., Pedraza, Javier, Fernández-Lozano, Javier, Turu, Valentí, López-Sáez, José Antonio, Karampaglidis, Theodoros, Granja-Bruña, José Luis, Muñoz-Martín, Alfonso
Tipo de recurso: artículo
Estado:Versión publicada
Fecha de publicación:2020
País:España
Institución:Universidad de Barcelona
Repositorio:Dipòsit Digital de la UB
OAI Identifier:oai:diposit.ub.edu:2445/194205
Acceso en línea:https://hdl.handle.net/2445/194205
Access Level:acceso abierto
Palabra clave:Geomorfologia glacial
Períodes glacials
Holocè
Glacial landforms
Glacial epoch
Holocene
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spelling Glacial geomorphology of the High Gredos Massif: Gredos and Pinar valleys (Iberian Central System, Spain)Carrasco, Rosa M.Soteres, Rodrigo L.Pedraza, JavierFernández-Lozano, JavierTuru, ValentíLópez-Sáez, José AntonioKarampaglidis, TheodorosGranja-Bruña, José LuisMuñoz-Martín, AlfonsoGeomorfologia glacialPeríodes glacialsHolocèGlacial landformsGlacial epochHoloceneWe present a detailed geomorphological map of the landform assemblages originated by the two major paleoglaciers of the Sierra de Gredos mountain range in the Spanish Iberian Central System. Based on previous works, our map focused on the features formed by Gredos and Pinar paleoglaciers during the last glaciation and subsequent glacial events. Based on a remote sensing analysis and exhaustive field surveys, we identified with great accuracy the local distribution of glacial, periglacial, mass movement, structural, fluvial, and lacustrine features. We recognized three main glacial geomorphological formations representing: (i) the maximum glacial extension reached (peripheral deposits); (ii) the culmination of glacial conditions (principal moraines) and (iii) the local glacial withdrawal (internal deposits). Our map offers a renewed spatial framework on which to conduct higher-resolution glacial chronologies, especially of Late Glacial and Holocene glacial activity, providing key information for performing future paleoclimatic reconstructions of the northern hemisphere mid-latitudes.Taylor and Francis2020info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionapplication/pdfhttps://hdl.handle.net/2445/194205Articles publicats en revistes (Dinàmica de la Terra i l'Oceà)reponame:Dipòsit Digital de la UBinstname:Universidad de BarcelonaInglésReproducció del document publicat a: https://doi.org/10.1080/17445647.2020.1833768Journal of Maps, 2020, vol. 16, num. 2, p. 790-804https://doi.org/10.1080/17445647.2020.1833768cc-by (c) Carrasco Rosa M. et al., 2020https://creativecommons.org/licenses/by/4.0/info:eu-repo/semantics/openAccessoai:diposit.ub.edu:2445/1942052026-05-27T06:46:51Z
dc.title.none.fl_str_mv Glacial geomorphology of the High Gredos Massif: Gredos and Pinar valleys (Iberian Central System, Spain)
title Glacial geomorphology of the High Gredos Massif: Gredos and Pinar valleys (Iberian Central System, Spain)
spellingShingle Glacial geomorphology of the High Gredos Massif: Gredos and Pinar valleys (Iberian Central System, Spain)
Carrasco, Rosa M.
Geomorfologia glacial
Períodes glacials
Holocè
Glacial landforms
Glacial epoch
Holocene
title_short Glacial geomorphology of the High Gredos Massif: Gredos and Pinar valleys (Iberian Central System, Spain)
title_full Glacial geomorphology of the High Gredos Massif: Gredos and Pinar valleys (Iberian Central System, Spain)
title_fullStr Glacial geomorphology of the High Gredos Massif: Gredos and Pinar valleys (Iberian Central System, Spain)
title_full_unstemmed Glacial geomorphology of the High Gredos Massif: Gredos and Pinar valleys (Iberian Central System, Spain)
title_sort Glacial geomorphology of the High Gredos Massif: Gredos and Pinar valleys (Iberian Central System, Spain)
dc.creator.none.fl_str_mv Carrasco, Rosa M.
Soteres, Rodrigo L.
Pedraza, Javier
Fernández-Lozano, Javier
Turu, Valentí
López-Sáez, José Antonio
Karampaglidis, Theodoros
Granja-Bruña, José Luis
Muñoz-Martín, Alfonso
author Carrasco, Rosa M.
author_facet Carrasco, Rosa M.
Soteres, Rodrigo L.
Pedraza, Javier
Fernández-Lozano, Javier
Turu, Valentí
López-Sáez, José Antonio
Karampaglidis, Theodoros
Granja-Bruña, José Luis
Muñoz-Martín, Alfonso
author_role author
author2 Soteres, Rodrigo L.
Pedraza, Javier
Fernández-Lozano, Javier
Turu, Valentí
López-Sáez, José Antonio
Karampaglidis, Theodoros
Granja-Bruña, José Luis
Muñoz-Martín, Alfonso
author2_role author
author
author
author
author
author
author
author
dc.subject.none.fl_str_mv Geomorfologia glacial
Períodes glacials
Holocè
Glacial landforms
Glacial epoch
Holocene
topic Geomorfologia glacial
Períodes glacials
Holocè
Glacial landforms
Glacial epoch
Holocene
description We present a detailed geomorphological map of the landform assemblages originated by the two major paleoglaciers of the Sierra de Gredos mountain range in the Spanish Iberian Central System. Based on previous works, our map focused on the features formed by Gredos and Pinar paleoglaciers during the last glaciation and subsequent glacial events. Based on a remote sensing analysis and exhaustive field surveys, we identified with great accuracy the local distribution of glacial, periglacial, mass movement, structural, fluvial, and lacustrine features. We recognized three main glacial geomorphological formations representing: (i) the maximum glacial extension reached (peripheral deposits); (ii) the culmination of glacial conditions (principal moraines) and (iii) the local glacial withdrawal (internal deposits). Our map offers a renewed spatial framework on which to conduct higher-resolution glacial chronologies, especially of Late Glacial and Holocene glacial activity, providing key information for performing future paleoclimatic reconstructions of the northern hemisphere mid-latitudes.
publishDate 2020
dc.date.none.fl_str_mv 2020
dc.type.none.fl_str_mv info:eu-repo/semantics/article
info:eu-repo/semantics/publishedVersion
format article
status_str publishedVersion
dc.identifier.none.fl_str_mv https://hdl.handle.net/2445/194205
url https://hdl.handle.net/2445/194205
dc.language.none.fl_str_mv Inglés
language_invalid_str_mv Inglés
dc.relation.none.fl_str_mv Reproducció del document publicat a: https://doi.org/10.1080/17445647.2020.1833768
Journal of Maps, 2020, vol. 16, num. 2, p. 790-804
https://doi.org/10.1080/17445647.2020.1833768
dc.rights.none.fl_str_mv cc-by (c) Carrasco Rosa M. et al., 2020
https://creativecommons.org/licenses/by/4.0/
info:eu-repo/semantics/openAccess
rights_invalid_str_mv cc-by (c) Carrasco Rosa M. et al., 2020
https://creativecommons.org/licenses/by/4.0/
eu_rights_str_mv openAccess
dc.format.none.fl_str_mv application/pdf
dc.publisher.none.fl_str_mv Taylor and Francis
publisher.none.fl_str_mv Taylor and Francis
dc.source.none.fl_str_mv Articles publicats en revistes (Dinàmica de la Terra i l'Oceà)
reponame:Dipòsit Digital de la UB
instname:Universidad de Barcelona
instname_str Universidad de Barcelona
reponame_str Dipòsit Digital de la UB
collection Dipòsit Digital de la UB
repository.name.fl_str_mv
repository.mail.fl_str_mv
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score 15,300719

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