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

[EN] 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...

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Autores: Carrasco, Rosa M., Soteres, Rodrigo L., Pedraza, Javier, Férnandez Lozano, Javier, Turu, Valentí, López Sáez, José Antonio, Muñoz Martín, Alfonso, Granja Bruña, José Luis, Karampaglidis, Theodoros
Tipo de recurso: artículo
Estado:Versión publicada
Fecha de publicación:2020
País:España
Institución:Universidad de León
Repositorio:BULERIA. Repositorio Institucional de la Universidad de León
OAI Identifier:oai:buleria.unileon.es:10612/21611
Acceso en línea:https://hdl.handle.net/10612/21611
Access Level:acceso abierto
Palabra clave:Ingeniería de minas
Sierra De Gredos
Glacial Geomorphological Mapping
Last Glacial Maximum
Last Glacial Termination
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, JavierFérnandez Lozano, JavierTuru, ValentíLópez Sáez, José AntonioMuñoz Martín, AlfonsoGranja Bruña, José LuisKarampaglidis, TheodorosIngeniería de minasSierra De GredosGlacial Geomorphological MappingLast Glacial MaximumLast Glacial TerminationHolocene[EN] 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.SIThis work was supported by the Spanish Ministry of Science and Innovation (Spanish initials: MINECO; project CGL2016-78380-P), University of Castilla–La Mancha Research Group (UCLM, project 2020-GRIN-28992) and the Chilean Ph.D. Fellowship CONICYT #21161417 and the ANID Millennium Science Initiative/Millennium Nucleus PaleoclimateTeylor & FrancisOtrosEscuela Superior y Tecnica de Ingenieros de Minas2020info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionhttps://hdl.handle.net/10612/21611reponame:BULERIA. Repositorio Institucional de la Universidad de Leóninstname:Universidad de LeónIngléshttp://creativecommons.org/licenses/by-nc-nd/4.0/info:eu-repo/semantics/openAccessoai:buleria.unileon.es:10612/216112026-06-24T12:43:27Z
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.
Ingeniería de minas
Sierra De Gredos
Glacial Geomorphological Mapping
Last Glacial Maximum
Last Glacial Termination
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
Férnandez Lozano, Javier
Turu, Valentí
López Sáez, José Antonio
Muñoz Martín, Alfonso
Granja Bruña, José Luis
Karampaglidis, Theodoros
author Carrasco, Rosa M.
author_facet Carrasco, Rosa M.
Soteres, Rodrigo L.
Pedraza, Javier
Férnandez Lozano, Javier
Turu, Valentí
López Sáez, José Antonio
Muñoz Martín, Alfonso
Granja Bruña, José Luis
Karampaglidis, Theodoros
author_role author
author2 Soteres, Rodrigo L.
Pedraza, Javier
Férnandez Lozano, Javier
Turu, Valentí
López Sáez, José Antonio
Muñoz Martín, Alfonso
Granja Bruña, José Luis
Karampaglidis, Theodoros
author2_role author
author
author
author
author
author
author
author
dc.contributor.none.fl_str_mv Otros
Escuela Superior y Tecnica de Ingenieros de Minas
dc.subject.none.fl_str_mv Ingeniería de minas
Sierra De Gredos
Glacial Geomorphological Mapping
Last Glacial Maximum
Last Glacial Termination
Holocene
topic Ingeniería de minas
Sierra De Gredos
Glacial Geomorphological Mapping
Last Glacial Maximum
Last Glacial Termination
Holocene
description [EN] 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/10612/21611
url https://hdl.handle.net/10612/21611
dc.language.none.fl_str_mv Inglés
language_invalid_str_mv Inglés
dc.rights.none.fl_str_mv http://creativecommons.org/licenses/by-nc-nd/4.0/
info:eu-repo/semantics/openAccess
rights_invalid_str_mv http://creativecommons.org/licenses/by-nc-nd/4.0/
eu_rights_str_mv openAccess
dc.publisher.none.fl_str_mv Teylor & Francis
publisher.none.fl_str_mv Teylor & Francis
dc.source.none.fl_str_mv reponame:BULERIA. Repositorio Institucional de la Universidad de León
instname:Universidad de León
instname_str Universidad de León
reponame_str BULERIA. Repositorio Institucional de la Universidad de León
collection BULERIA. Repositorio Institucional de la Universidad de León
repository.name.fl_str_mv
repository.mail.fl_str_mv
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score 15,811543

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