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/).
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| 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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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 |
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article |
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publishedVersion |
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http://hdl.handle.net/10261/359849 |
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Inglés |
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Inglés |
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#PLACEHOLDER_PARENT_METADATA_VALUE# info:eu-repo/grantAgreement/MINECO//RYC-2015-17597 https://doi.org/10.1016/j.geomorph.2022.108112 Sí |
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openAccess |
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Elsevier BV |
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Elsevier BV |
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reponame:DIGITAL.CSIC. Repositorio Institucional del CSIC instname:Consejo Superior de Investigaciones Científicas (CSIC) |
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