Coeval giant landslides in the Canary Islands: Implications for global, regional and local triggers of giant flank collapses on oceanic volcanoes

Giant landslides are an important part of the evolution of most intra-plate volcanic islands. They often proceed in catastrophic events, likely to generate voluminous debris avalanches and eventually trigger destructive tsunamis. Although knowledge of the timing of their recurrence is a key factor regarding the hazard assessment in coastal environments, only a few of them have been well dated. In this contribution, we focus on the La Orotava event on Tenerife, which we date with the unspiked K–Ar technique, between 534 and 523 ka. Such narrow temporal interval is compatible, within uncertainties, with the age of the Cumbre Nueva collapse on the neighboring island of La Palma. We thus examine here the possible common triggering mechanisms at the global, regional and local scales. Both events occurred shortly after the climax of the oxygen isotopic stage 14, during the rapid transition towards the interglacial stage 13, reinforcing the hypothesis of a control from global paleoclimatic changes on the destabilization of oceanic islands. Intense volcanic pulses at the regional scale also lead to the synchronous overgrowth of several volcanic islands in the archipelago, but coeval destabilization on Tenerife and La Palma appears significantly controlled by the intrinsic morphology of the edifices, with contrasted instability thresholds for shield volcanoes and volcanic ridges respectively. Finally, we propose that the two events may be genetically linked. Dynamic transfer of voluminous debris avalanches during a giant landslide episode can induce isostatic readjustments, generate significant ground acceleration and finally produce a large tsunami, three processes which can concur to trigger large scale flank collapse on a neighboring mature unstable volcanic island.

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Main Authors: Boulesteix, Thomas, Hildenbrandab, Anthony, Soler, Vicente, Quidelleur, Xavier, Gillot, Pierre-Yves
Other Authors: Ministerio de Ciencia e Innovación (España)
Format: artículo biblioteca
Language:English
Published: Elsevier 2013-03-21
Subjects:Triggering factor, Tenerife, Canary Islands, K–Ar, Giant sector collapse,
Online Access:http://hdl.handle.net/10261/178403
http://dx.doi.org/10.13039/501100004837
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spelling dig-ipna-es-10261-1784032022-06-30T07:38:33Z Coeval giant landslides in the Canary Islands: Implications for global, regional and local triggers of giant flank collapses on oceanic volcanoes Boulesteix, Thomas Hildenbrandab, Anthony Soler, Vicente Quidelleur, Xavier Gillot, Pierre-Yves Ministerio de Ciencia e Innovación (España) Triggering factor Tenerife Canary Islands K–Ar Giant sector collapse Giant landslides are an important part of the evolution of most intra-plate volcanic islands. They often proceed in catastrophic events, likely to generate voluminous debris avalanches and eventually trigger destructive tsunamis. Although knowledge of the timing of their recurrence is a key factor regarding the hazard assessment in coastal environments, only a few of them have been well dated. In this contribution, we focus on the La Orotava event on Tenerife, which we date with the unspiked K–Ar technique, between 534 and 523 ka. Such narrow temporal interval is compatible, within uncertainties, with the age of the Cumbre Nueva collapse on the neighboring island of La Palma. We thus examine here the possible common triggering mechanisms at the global, regional and local scales. Both events occurred shortly after the climax of the oxygen isotopic stage 14, during the rapid transition towards the interglacial stage 13, reinforcing the hypothesis of a control from global paleoclimatic changes on the destabilization of oceanic islands. Intense volcanic pulses at the regional scale also lead to the synchronous overgrowth of several volcanic islands in the archipelago, but coeval destabilization on Tenerife and La Palma appears significantly controlled by the intrinsic morphology of the edifices, with contrasted instability thresholds for shield volcanoes and volcanic ridges respectively. Finally, we propose that the two events may be genetically linked. Dynamic transfer of voluminous debris avalanches during a giant landslide episode can induce isostatic readjustments, generate significant ground acceleration and finally produce a large tsunami, three processes which can concur to trigger large scale flank collapse on a neighboring mature unstable volcanic island. We would like to thank Tomás Cologan for his help in gaining access to the Pino Soler gallery. Vicente Soler acknowledges the financial support of the Ministerio Ciencia e innovation for the project CGL2011-25494. We also thank Medio Ambiente for authorizing access and sampling. Our manuscript benefitted from the comments of two anonymous reviewers. This is LGMT contribution no. 106. 2019-03-25T08:41:20Z 2019-03-25T08:41:20Z 2013-03-21 2019-03-25T08:41:20Z artículo http://purl.org/coar/resource_type/c_6501 doi: 10.1016/j.jvolgeores.2013.03.008 issn: 0377-0273 Journal of Volcanology and Geothermal Research 257: 90-98 (2013) http://hdl.handle.net/10261/178403 10.1016/j.jvolgeores.2013.03.008 http://dx.doi.org/10.13039/501100004837 en https://doi.org/10.1016/j.jvolgeores.2013.03.008 Sí open Elsevier
institution IPNA ES
collection DSpace
country España
countrycode ES
component Bibliográfico
access En linea
databasecode dig-ipna-es
tag biblioteca
region Europa del Sur
libraryname Biblioteca del IPNA España
language English
topic Triggering factor
Tenerife
Canary Islands
K–Ar
Giant sector collapse
Triggering factor
Tenerife
Canary Islands
K–Ar
Giant sector collapse
spellingShingle Triggering factor
Tenerife
Canary Islands
K–Ar
Giant sector collapse
Triggering factor
Tenerife
Canary Islands
K–Ar
Giant sector collapse
Boulesteix, Thomas
Hildenbrandab, Anthony
Soler, Vicente
Quidelleur, Xavier
Gillot, Pierre-Yves
Coeval giant landslides in the Canary Islands: Implications for global, regional and local triggers of giant flank collapses on oceanic volcanoes
description Giant landslides are an important part of the evolution of most intra-plate volcanic islands. They often proceed in catastrophic events, likely to generate voluminous debris avalanches and eventually trigger destructive tsunamis. Although knowledge of the timing of their recurrence is a key factor regarding the hazard assessment in coastal environments, only a few of them have been well dated. In this contribution, we focus on the La Orotava event on Tenerife, which we date with the unspiked K–Ar technique, between 534 and 523 ka. Such narrow temporal interval is compatible, within uncertainties, with the age of the Cumbre Nueva collapse on the neighboring island of La Palma. We thus examine here the possible common triggering mechanisms at the global, regional and local scales. Both events occurred shortly after the climax of the oxygen isotopic stage 14, during the rapid transition towards the interglacial stage 13, reinforcing the hypothesis of a control from global paleoclimatic changes on the destabilization of oceanic islands. Intense volcanic pulses at the regional scale also lead to the synchronous overgrowth of several volcanic islands in the archipelago, but coeval destabilization on Tenerife and La Palma appears significantly controlled by the intrinsic morphology of the edifices, with contrasted instability thresholds for shield volcanoes and volcanic ridges respectively. Finally, we propose that the two events may be genetically linked. Dynamic transfer of voluminous debris avalanches during a giant landslide episode can induce isostatic readjustments, generate significant ground acceleration and finally produce a large tsunami, three processes which can concur to trigger large scale flank collapse on a neighboring mature unstable volcanic island.
author2 Ministerio de Ciencia e Innovación (España)
author_facet Ministerio de Ciencia e Innovación (España)
Boulesteix, Thomas
Hildenbrandab, Anthony
Soler, Vicente
Quidelleur, Xavier
Gillot, Pierre-Yves
format artículo
topic_facet Triggering factor
Tenerife
Canary Islands
K–Ar
Giant sector collapse
author Boulesteix, Thomas
Hildenbrandab, Anthony
Soler, Vicente
Quidelleur, Xavier
Gillot, Pierre-Yves
author_sort Boulesteix, Thomas
title Coeval giant landslides in the Canary Islands: Implications for global, regional and local triggers of giant flank collapses on oceanic volcanoes
title_short Coeval giant landslides in the Canary Islands: Implications for global, regional and local triggers of giant flank collapses on oceanic volcanoes
title_full Coeval giant landslides in the Canary Islands: Implications for global, regional and local triggers of giant flank collapses on oceanic volcanoes
title_fullStr Coeval giant landslides in the Canary Islands: Implications for global, regional and local triggers of giant flank collapses on oceanic volcanoes
title_full_unstemmed Coeval giant landslides in the Canary Islands: Implications for global, regional and local triggers of giant flank collapses on oceanic volcanoes
title_sort coeval giant landslides in the canary islands: implications for global, regional and local triggers of giant flank collapses on oceanic volcanoes
publisher Elsevier
publishDate 2013-03-21
url http://hdl.handle.net/10261/178403
http://dx.doi.org/10.13039/501100004837
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