The origin and collapse of rock glaciers during the Bølling-Allerød interstadial: A new study case from the Cantabrian Mountains (Spain)

© 2022 The Author(s). Published by Elsevier B.V. This is an open access article under the CC BY-NC-ND license (http://creativecommons.org/licenses/by-nc-nd/4.0/).

Bibliographic Details
Authors: Santos-González, Javier, González-Gutiérrez, Rosa Blanca, Redondo-Vega, José María, Gómez-Villar, Amelia, Jomelli, Vincent, Fernández-Fernández, José M., Andrés, Nuria de, García-Ruiz, José María, Peña-Pérez, Sergio Alberto, Melón-Nava, Adrián, Oliva, Marc, Álvarez-Martínez, Javier, Charton, Joanna, ASTER Team, Palacios, David
Format: article
Status:Published version
Publication Date:2022
Country:España
Institution:Consejo Superior de Investigaciones Científicas (CSIC)
Repository:DIGITAL.CSIC. Repositorio Institucional del CSIC
OAI Identifier:oai:digital.csic.es:10261/359849
Online Access:http://hdl.handle.net/10261/359849
Access Level:Open access
Keyword:Rock glacier
Deglaciation
Paraglacial processes
Cosmic-Ray Exposure dating
Bølling-Allerød interstadial
Cantabrian Mountains
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spelling The origin and collapse of rock glaciers during the Bølling-Allerød interstadial: A new study case from the Cantabrian Mountains (Spain)Santos-González, JavierGonzález-Gutiérrez, Rosa BlancaRedondo-Vega, José MaríaGómez-Villar, AmeliaJomelli, VincentFernández-Fernández, José M.Andrés, Nuria deGarcía-Ruiz, José MaríaPeña-Pérez, Sergio AlbertoMelón-Nava, AdriánOliva, MarcÁlvarez-Martínez, JavierCharton, JoannaASTER TeamPalacios, DavidRock glacierDeglaciationParaglacial processesCosmic-Ray Exposure datingBølling-Allerød interstadialCantabrian Mountains© 2022 The Author(s). Published by Elsevier B.V. This is an open access article under the CC BY-NC-ND license (http://creativecommons.org/licenses/by-nc-nd/4.0/).During the Late Pleistocene, the main mountain ranges of the Iberian Peninsula were covered by small icefields and cirque and alpine glaciers. The deglaciation triggered paraglacial processes that generated landforms, mostly within the ice-free glacial cirques. In this research we analyse the deglaciation process in the Muxivén Cirque (42°15′N – 6°16′W), in the upper Sil River Basin, which includes some of the largest relict rock glaciers of the Cantabrian Mountains. We addressed this objective by means of accurate geomorphological reconstructions, sedimentological analysis, Schmidt-hammer surface weathering measurements and a dataset of 10 10Be Cosmic-Ray Exposure ages. Results reveal that after ~16 ka, glaciers retreated to the bottom of the cirques at the headwaters of the valley, leaving the walls free of ice and triggering rock avalanches onto the remnants of these glaciers. This paraglacial process supplied debris to a small glacier within Muxivén Cirque, which transformed in two rock glaciers. These debris isolated the ice inside the rock glaciers only for a very short period of time and ended up melting completely before the Younger Dryas. The lower sector of the largest one stabilized at 14.5 ± 1.5 ka, while the upper sector remained active until 13.5 ± 0.8 ka. Previous to the stabilization of the lower sector of the northern rock glacier, at its margin a high-energy debris avalanche occurred at ~14.0 ± 0.9 ka. These data agree with previous research, corroborating the paraglacial origin of most Iberian rock glaciers during the Bølling-Allerød interstadial.This research was supported by the project LE080G19 (Paleo-environmental significance and relationship with the global change of the Cantabrian Mountains rock glaciers: relative age dating and analysis of the internal structure using electrical tomography), founded by the Junta de Castilla y León and PR108/20-20 (Santander Bank-UCM Projects). José M. Fernández-Fernández is supported by a postdoctoral grant within the NUNANTAR project, funded by the Fundação para a Ciência e Tecnologia of Portugal (PTDC/CTA-GFI/32002/2017). Marc Oliva is supported by the Ramón y Cajal Program (RYC-2015-17597) and by the Research Group ANTALP (Antarctic, Arctic, Alpine Environments; 2017-SGR-1102) funded by the Government of Catalonia. Adrián Melón-Nava was supported by the FPU program from the Spanish Ministerio de Universidades (FPU20/01220).Peer reviewedElsevier BVJunta de Castilla y LeónBanco SantanderUniversidad Complutense de MadridFundação para a Ciência e a Tecnologia (Portugal)Ministerio de Economía y Competitividad (España)Generalitat de CatalunyaMinisterio de Universidades (España)García-Ruiz, José María [0000-0002-8535-817X]Consejo Superior de Investigaciones Científicas [https://ror.org/02gfc7t72]202420242022info:eu-repo/semantics/articlehttp://purl.org/coar/resource_type/c_6501Publisher's versioninfo:eu-repo/semantics/publishedVersionapplication/pdfhttp://hdl.handle.net/10261/359849reponame:DIGITAL.CSIC. Repositorio Institucional del CSICinstname:Consejo Superior de Investigaciones Científicas (CSIC)Inglés#PLACEHOLDER_PARENT_METADATA_VALUE#info:eu-repo/grantAgreement/MINECO//RYC-2015-17597https://doi.org/10.1016/j.geomorph.2022.108112Síinfo:eu-repo/semantics/openAccessoai:digital.csic.es:10261/3598492026-05-22T06:33:51Z
dc.title.none.fl_str_mv The origin and collapse of rock glaciers during the Bølling-Allerød interstadial: A new study case from the Cantabrian Mountains (Spain)
title The origin and collapse of rock glaciers during the Bølling-Allerød interstadial: A new study case from the Cantabrian Mountains (Spain)
spellingShingle The origin and collapse of rock glaciers during the Bølling-Allerød interstadial: A new study case from the Cantabrian Mountains (Spain)
Santos-González, Javier
Rock glacier
Deglaciation
Paraglacial processes
Cosmic-Ray Exposure dating
Bølling-Allerød interstadial
Cantabrian Mountains
title_short The origin and collapse of rock glaciers during the Bølling-Allerød interstadial: A new study case from the Cantabrian Mountains (Spain)
title_full The origin and collapse of rock glaciers during the Bølling-Allerød interstadial: A new study case from the Cantabrian Mountains (Spain)
title_fullStr The origin and collapse of rock glaciers during the Bølling-Allerød interstadial: A new study case from the Cantabrian Mountains (Spain)
title_full_unstemmed The origin and collapse of rock glaciers during the Bølling-Allerød interstadial: A new study case from the Cantabrian Mountains (Spain)
title_sort The origin and collapse of rock glaciers during the Bølling-Allerød interstadial: A new study case from the Cantabrian Mountains (Spain)
dc.creator.none.fl_str_mv Santos-González, Javier
González-Gutiérrez, Rosa Blanca
Redondo-Vega, José María
Gómez-Villar, Amelia
Jomelli, Vincent
Fernández-Fernández, José M.
Andrés, Nuria de
García-Ruiz, José María
Peña-Pérez, Sergio Alberto
Melón-Nava, Adrián
Oliva, Marc
Álvarez-Martínez, Javier
Charton, Joanna
ASTER Team
Palacios, David
author Santos-González, Javier
author_facet Santos-González, Javier
González-Gutiérrez, Rosa Blanca
Redondo-Vega, José María
Gómez-Villar, Amelia
Jomelli, Vincent
Fernández-Fernández, José M.
Andrés, Nuria de
García-Ruiz, José María
Peña-Pérez, Sergio Alberto
Melón-Nava, Adrián
Oliva, Marc
Álvarez-Martínez, Javier
Charton, Joanna
ASTER Team
Palacios, David
author_role author
author2 González-Gutiérrez, Rosa Blanca
Redondo-Vega, José María
Gómez-Villar, Amelia
Jomelli, Vincent
Fernández-Fernández, José M.
Andrés, Nuria de
García-Ruiz, José María
Peña-Pérez, Sergio Alberto
Melón-Nava, Adrián
Oliva, Marc
Álvarez-Martínez, Javier
Charton, Joanna
ASTER Team
Palacios, David
author2_role author
author
author
author
author
author
author
author
author
author
author
author
author
author
dc.contributor.none.fl_str_mv Junta de Castilla y León
Banco Santander
Universidad Complutense de Madrid
Fundação para a Ciência e a Tecnologia (Portugal)
Ministerio de Economía y Competitividad (España)
Generalitat de Catalunya
Ministerio de Universidades (España)
García-Ruiz, José María [0000-0002-8535-817X]
Consejo Superior de Investigaciones Científicas [https://ror.org/02gfc7t72]
dc.subject.none.fl_str_mv Rock glacier
Deglaciation
Paraglacial processes
Cosmic-Ray Exposure dating
Bølling-Allerød interstadial
Cantabrian Mountains
topic Rock glacier
Deglaciation
Paraglacial processes
Cosmic-Ray Exposure dating
Bølling-Allerød interstadial
Cantabrian Mountains
description © 2022 The Author(s). Published by Elsevier B.V. This is an open access article under the CC BY-NC-ND license (http://creativecommons.org/licenses/by-nc-nd/4.0/).
publishDate 2022
dc.date.none.fl_str_mv 2022
2024
2024
dc.type.none.fl_str_mv info:eu-repo/semantics/article
http://purl.org/coar/resource_type/c_6501
Publisher's version
info:eu-repo/semantics/publishedVersion
format article
status_str publishedVersion
dc.identifier.none.fl_str_mv http://hdl.handle.net/10261/359849
url http://hdl.handle.net/10261/359849
dc.language.none.fl_str_mv Inglés
language_invalid_str_mv Inglés
dc.relation.none.fl_str_mv #PLACEHOLDER_PARENT_METADATA_VALUE#
info:eu-repo/grantAgreement/MINECO//RYC-2015-17597
https://doi.org/10.1016/j.geomorph.2022.108112

dc.rights.none.fl_str_mv info:eu-repo/semantics/openAccess
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