Characterization and geophysical evaluation of the recent 2023 Alausí landslide in the northern Andes of Ecuador

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Campo DCValorIdioma
dc.contributorIngeniería del Terreno y sus Estructuras (InTerEs)es_ES
dc.contributor.authorMacías, Lucia-
dc.contributor.authorQuiñonez‑Macías, María-
dc.contributor.authorToulkeridis, Theofilos-
dc.contributor.authorPastor Navarro, José Luis-
dc.contributor.otherUniversidad de Alicante. Departamento de Ingeniería Civiles_ES
dc.date.accessioned2024-01-09T08:21:11Z-
dc.date.available2024-01-09T08:21:11Z-
dc.date.issued2023-12-30-
dc.identifier.citationLandslides. 2024, 21: 529-540. https://doi.org/10.1007/s10346-023-02185-6es_ES
dc.identifier.issn1612-510X (Print)-
dc.identifier.issn1612-5118 (Online)-
dc.identifier.urihttp://hdl.handle.net/10045/139547-
dc.description.abstractThe province of Chimborazo located in the northern Andes of Ecuador presents many intrinsic factors, which contribute to the occurrence of mass movements, leaving in many of the cases registered damages of materials and loss of life. The recent landslide of March 26, 2023, in the Alausí canton is an event of great interest due to the magnitude of the occurred destruction and the corresponding fatalities. Therefore, there are two predominant objectives of the current study, of which the first has been to determine the most relevant characteristics of this mass movement by identifying and analyzing the geomorphology of the recorded slope movement and the lithological units involved, by field work and through geophysical surveys. Secondly, we performed a preliminary study of the possible triggers of the movement by means of the historical analysis of the precipitations during the months of January to March of the last decade and the study of the recent seismic series. However, through the obtained analysis, it is determined that the study site is composed of three distinctive lithological units. The observed mass movement is of the rotational type, as result of the intense rainfall that occurred during the first quarter of 2023, being hereby the most probable triggering factor. This corresponds to a 600% increase in the average monthly rainfall compared to the period from 2010 to 2022.es_ES
dc.description.sponsorshipOpen Access funding provided thanks to the CRUE-CSIC agreement with Springer Nature.es_ES
dc.languageenges_ES
dc.publisherSpringer Naturees_ES
dc.rights© The authors. Open Access This article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons licence, and indicate if changes were made. The images or other third party material in this article are included in the article's Creative Commons licence, unless indicated otherwise in a credit line to the material. If material is not included in the article's Creative Commons licence and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder. To view a copy of this licence, visit http://creativecommons.org/licenses/by/4.0/.es_ES
dc.subjectSaturationes_ES
dc.subjectPrecipitationes_ES
dc.subjectRupture zonees_ES
dc.subjectAlausí landslidees_ES
dc.subjectEcuadores_ES
dc.titleCharacterization and geophysical evaluation of the recent 2023 Alausí landslide in the northern Andes of Ecuadores_ES
dc.typeinfo:eu-repo/semantics/articlees_ES
dc.peerreviewedsies_ES
dc.identifier.doi10.1007/s10346-023-02185-6-
dc.relation.publisherversionhttps://doi.org/10.1007/s10346-023-02185-6es_ES
dc.rights.accessRightsinfo:eu-repo/semantics/openAccesses_ES
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