Deglaciation in the Cantabrian Mountains: Pattern and evolution

The last deglaciation of the Cantabrian Mountain began later than 30 ka ago, after a local glacier maximum. After this glaciation a moderate glacier retreat occurred during a less cold period, followed by a new glacier advance that deposited moraines close to the maximum extension moraine complexes....

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Detalhes bibliográficos
Autores: Serrano, E., Gómez-Lende, M., Pellitero, R., González Trueba, Juan José
Tipo de documento: artigo
Data de publicação:2015
País:España
Recursos:Universidad de Cantabria (UC)
Repositório:UCrea Repositorio Abierto de la Universidad de Cantabria
Idioma:inglês
OAI Identifier:oai:repositorio.unican.es:10902/28595
Acesso em linha:https://hdl.handle.net/10902/28595
Access Level:Acceso aberto
Palavra-chave:Glaciations
Deglaciation
Quaternary
Cantabrian Mountains
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spelling Deglaciation in the Cantabrian Mountains: Pattern and evolutionSerrano, E.Gómez-Lende, M.Pellitero, R.González Trueba, Juan JoséGlaciationsDeglaciationQuaternaryCantabrian MountainsThe last deglaciation of the Cantabrian Mountain began later than 30 ka ago, after a local glacier maximum. After this glaciation a moderate glacier retreat occurred during a less cold period, followed by a new glacier advance that deposited moraines close to the maximum extension moraine complexes. This cold but very dry period occurred between~ 22-18 ka and it was related to European LGM. Dating made during the last 12 years support a distinctive model of deglaciation history for the last glacial cycle, different to North European and analogous to NW Iberian Mountains and the Pyrenees. The most important deglaciation phase began after 18 ka, when ice disappeared of the lower massifs, icefields withdraw and the main tongue glaciers divided in minor tongues. From ~14 to ~11 ka a new cold period implied a glacier growth dominated by topoclimatic factors in the massifs above 2100. Only on the highest massifs glaciers developed in all orientations, together withrock glaciers established mainly to the North orientations. During the Holocene there are not evidences of glacial stages and the deglaciation was complete. Only four small glaciers were developed during the Little Ice Age in the Picos de Europa, disappearing at the end of the XIX century.Universidad de La RiojaUniversidad de Cantabria20152015-01-01journal articlehttp://purl.org/coar/resource_type/c_6501NAhttp://purl.org/coar/version/c_be7fb7dd8ff6fe43info:eu-repo/semantics/articlehttps://hdl.handle.net/10902/28595Cuadernos de Investigacion Geografica 2015, 41(2), 389-408reponame:UCrea Repositorio Abierto de la Universidad de Cantabriainstname:Universidad de Cantabria (UC)Inglésengopen accesshttp://purl.org/coar/access_right/c_abf2Attribution-NonCommercial-NoDerivatives 4.0 Internationalhttp://creativecommons.org/licenses/by-nc-nd/4.0/info:eu-repo/semantics/openAccessoai:repositorio.unican.es:10902/285952026-06-02T12:39:31Z
dc.title.none.fl_str_mv Deglaciation in the Cantabrian Mountains: Pattern and evolution
title Deglaciation in the Cantabrian Mountains: Pattern and evolution
spellingShingle Deglaciation in the Cantabrian Mountains: Pattern and evolution
Serrano, E.
Glaciations
Deglaciation
Quaternary
Cantabrian Mountains
title_short Deglaciation in the Cantabrian Mountains: Pattern and evolution
title_full Deglaciation in the Cantabrian Mountains: Pattern and evolution
title_fullStr Deglaciation in the Cantabrian Mountains: Pattern and evolution
title_full_unstemmed Deglaciation in the Cantabrian Mountains: Pattern and evolution
title_sort Deglaciation in the Cantabrian Mountains: Pattern and evolution
dc.creator.none.fl_str_mv Serrano, E.
Gómez-Lende, M.
Pellitero, R.
González Trueba, Juan José
author Serrano, E.
author_facet Serrano, E.
Gómez-Lende, M.
Pellitero, R.
González Trueba, Juan José
author_role author
author2 Gómez-Lende, M.
Pellitero, R.
González Trueba, Juan José
author2_role author
author
author
dc.contributor.none.fl_str_mv Universidad de Cantabria
dc.subject.none.fl_str_mv Glaciations
Deglaciation
Quaternary
Cantabrian Mountains
topic Glaciations
Deglaciation
Quaternary
Cantabrian Mountains
description The last deglaciation of the Cantabrian Mountain began later than 30 ka ago, after a local glacier maximum. After this glaciation a moderate glacier retreat occurred during a less cold period, followed by a new glacier advance that deposited moraines close to the maximum extension moraine complexes. This cold but very dry period occurred between~ 22-18 ka and it was related to European LGM. Dating made during the last 12 years support a distinctive model of deglaciation history for the last glacial cycle, different to North European and analogous to NW Iberian Mountains and the Pyrenees. The most important deglaciation phase began after 18 ka, when ice disappeared of the lower massifs, icefields withdraw and the main tongue glaciers divided in minor tongues. From ~14 to ~11 ka a new cold period implied a glacier growth dominated by topoclimatic factors in the massifs above 2100. Only on the highest massifs glaciers developed in all orientations, together withrock glaciers established mainly to the North orientations. During the Holocene there are not evidences of glacial stages and the deglaciation was complete. Only four small glaciers were developed during the Little Ice Age in the Picos de Europa, disappearing at the end of the XIX century.
publishDate 2015
dc.date.none.fl_str_mv 2015
2015-01-01
dc.type.none.fl_str_mv journal article
http://purl.org/coar/resource_type/c_6501
NA
http://purl.org/coar/version/c_be7fb7dd8ff6fe43
dc.type.openaire.fl_str_mv info:eu-repo/semantics/article
format article
dc.identifier.none.fl_str_mv https://hdl.handle.net/10902/28595
url https://hdl.handle.net/10902/28595
dc.language.none.fl_str_mv Inglés
eng
language_invalid_str_mv Inglés
language eng
dc.rights.none.fl_str_mv open access
http://purl.org/coar/access_right/c_abf2
Attribution-NonCommercial-NoDerivatives 4.0 International
http://creativecommons.org/licenses/by-nc-nd/4.0/
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
Attribution-NonCommercial-NoDerivatives 4.0 International
http://creativecommons.org/licenses/by-nc-nd/4.0/
eu_rights_str_mv openAccess
dc.publisher.none.fl_str_mv Universidad de La Rioja
publisher.none.fl_str_mv Universidad de La Rioja
dc.source.none.fl_str_mv Cuadernos de Investigacion Geografica 2015, 41(2), 389-408
reponame:UCrea Repositorio Abierto de la Universidad de Cantabria
instname:Universidad de Cantabria (UC)
instname_str Universidad de Cantabria (UC)
reponame_str UCrea Repositorio Abierto de la Universidad de Cantabria
collection UCrea Repositorio Abierto de la Universidad de Cantabria
repository.name.fl_str_mv
repository.mail.fl_str_mv
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