Multidisciplinary study of the impacts of the 1600 CE Huaynaputina eruption and a project for geosites and geo-touristic attractions

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dc.contributor.authorMariño, Jersy
dc.contributor.authorCueva, Kevin
dc.contributor.authorThouret, Jean-Claude
dc.contributor.authorArias, Carla
dc.contributor.authorFinizola, Antony
dc.contributor.authorAntoine, Raphael
dc.contributor.authorDelcher, Eric
dc.contributor.authorFauchard, Cyrille
dc.contributor.authorDonnadieu, Franck
dc.contributor.authorLabazuy, Philippe
dc.contributor.authorJapura, Saida
dc.contributor.authorGusset, Rachel
dc.contributor.authorSanchez, Paola
dc.contributor.authorRamos, Domingo
dc.contributor.authorMacedo Franco, Luisa Diomira
dc.contributor.authorLazarte, Ivonne
dc.contributor.authorLiliane, Thouret
dc.contributor.authorDel Carpio Calienes, José Alberto
dc.contributor.authorJaime, Lourdes
dc.contributor.authorSaintenoy, Thibault
dc.coverage.spatialHuaynaputina, Volcán (Moquegua, Perú)
dc.date.accessioned2022-02-16T10:50:14Z
dc.date.available2022-02-16T10:50:14Z
dc.date.issued2021-07
dc.description.abstractThe Huaynaputina volcano, southern Peru, was the site of the largest historical eruption (VEI 6) in the Andes in 1600 CE, which occurred during the historic transition between the Inca Empire and the Viceroyalty of Peru. This event had severe consequences in the Central Andes and a global climatic impact. Spanish chronicles reported that at least 15 villages or settlements existed around the volcano, of which seven of them were totally destroyed by the eruption. Multidisciplinary studies have allowed us to identify and analyze the characteristics of six settlements buried by the eruption. Tephra fallout and pyroclastic current deposits (PDCs) had different impacts according to the settlement distance from the crater, the location with respect to the emplacement of PDCs along valleys, the geomorphological characteristics of the site, and type of constructions. Thus, Calicanto, Cojraque, and San Juan de Dios, located beneath the main axis of tephra dispersal lobe due west and/or on valley edges, were buried under several meters of pyroclastic deposits, while the villages of Estagagache, Chimpapampa, and Moro Moro, located to the S and SE of the lobe, were partially mantled by tephra. The 1600 CE Huaynaputina eruption created an important geological and cultural heritage, which has scientific, educational, and touristic values. Geo-touristic attractions are proposed based on identification, characterization, and qualitative evaluation of four groups totaling 17 geosites: volcanic geosites, volcanic-cultural geomorphosites, and hot springs. Seven geological roads along with seven viewpoints are proposed, which allow to value the most relevant landscapes, deposits and geological structures.es_ES
dc.description.peer-reviewPor pareses_ES
dc.formatapplication/pdfes_ES
dc.identifier.citationMariño, J., Cueva, K., Thouret, J.-C., Arias, C., Finizola, A., Antoine, R., … Saintenoy, T. (2021). Multidisciplinary Study of the Impacts of the 1600 CE Huaynaputina Eruption and a Project for Geosites and Geo-touristic Attractions.==$Geoheritage, 13$==(3), 64. https://doi.org/10.1007/s12371-021-00577-5es_ES
dc.identifier.doihttps://doi.org/10.1007/s12371-021-00577-5es_ES
dc.identifier.govdocindex-oti2018
dc.identifier.journalGeoheritagees_ES
dc.identifier.urihttp://hdl.handle.net/20.500.12816/5091
dc.language.isoenges_ES
dc.publisherSpringeres_ES
dc.relation.ispartofurn:issn:1867-2477
dc.rightsinfo:eu-repo/semantics/closedAccesses_ES
dc.subjectHuaynaputinaes_ES
dc.subjectEruptiones_ES
dc.subjectBuried settlementses_ES
dc.subjectHeritagees_ES
dc.subjectGeositeses_ES
dc.subject.ocdehttps://purl.org/pe-repo/ocde/ford#1.05.07es_ES
dc.titleMultidisciplinary study of the impacts of the 1600 CE Huaynaputina eruption and a project for geosites and geo-touristic attractionses_ES
dc.typeinfo:eu-repo/semantics/articlees_ES

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