dc.creatorAntoine, Raphael
dc.creatorMacedo Franco, Luisa Diomira
dc.creatorFinizola, Anthony
dc.creatorDelcher, Eric
dc.creatorThouret, Jean-Claude
dc.creatorFauchard, Cyrille
dc.creatorGusset, Rachel
dc.creatorJapura Paredes, Saida Blanca
dc.creatorLazarte Zerpa, Ivonne Alejandra
dc.creatorGuilber, Vincent
dc.creatorBacri, Clémentine
dc.creatorNormier, Adrien
dc.creatorRamos Palomino, Domingo A.
dc.creatorSaintenoy, Thibault
dc.creatorThouret, Liliane
dc.creatorDel Carpio, José
dc.creatorPuma, Nino
dc.date.accessioned2022-04-22T17:24:07Z
dc.date.accessioned2022-10-27T15:36:21Z
dc.date.available2022-04-22T17:24:07Z
dc.date.available2022-10-27T15:36:21Z
dc.date.created2022-04-22T17:24:07Z
dc.date.issued2018
dc.identifierAntoine, R.; Macedo, L.; Finizola, A.; Delcher, E.; Thouret, J.; Fauchard, C.; Gusset, R.; Japura, S.; Lazarte, I.; Mariño, J.; Guilber, V.; Bacri, C.; Normier, A.; Ramos, D.; Saintenoy, T.; Thouret, L.; Del Carpio, J.; Puma, N. & Macedo, O. (2018). The Huayruro Project: mapping the Calicanto Inca area buried by the A.D. 1600 Huaynaputina eruption, with geophysical imaging and remote sensing. En: Corsaro, R.A.; Di Giuseppe, M.G.; Isaia, R.; Mormone, A.; Nave, R., eds. Millenia of Stratification between Human Life and Volcanoes: strategies for coexistence. Abstracts Volume of the International Cities on Volcanoes 10, 2-7 September 2018, Napoli, Italy. Roma: Istituto Nazionale di Geofisica e Vulcanologia, Miscellanea INGV, 43, p. 654.
dc.identifierhttps://hdl.handle.net/20.500.12544/3825
dc.identifier10th International Cities on Volcanoes “Millenia of Stratification between Human Life and Volcanoes: strategies for coexistence”, Napoli, Italy, 2-7 September 2018. Abstracts Volume.
dc.identifier.urihttps://repositorioslatinoamericanos.uchile.cl/handle/2250/4906058
dc.description.abstractWe present geophysical and remote sensing observations near the Quinistaquillas town (southern Peru), in the framework of the HUAYRURO Project. This Inca zone was buried during the A.D. 1600 Huaynaputina eruption, the most important volcanic phenomenon of the last 400 years. The eruption had a global impact, due to the volume of emitted ash (2-3 times the one emitted by Vesuvius in A.D. 79). This lead to a 1.13°C cooling of the planet and caused a worlwide agricultural crisis. During the eruption, the Calicanto-Chimpapampa zone was covered by ashes and pyroclastic flows, with a thickness in the range [1 - 20] m. From 2015 to 2017, remote sensing and geophysical methods were deployed to map a ~ 1 km*2 km area, up to 3-m depth.
dc.languageeng
dc.publisherIstituto Nazionale di Geofisica e Vulcanologia
dc.publisherITA
dc.rightshttps://creativecommons.org/licenses/by-nc-nd/4.0/deed.es
dc.rightsinfo:eu-repo/semantics/openAccess
dc.sourceRepositorio Institucional INGEMMET
dc.sourceInstituto Geológico, Minero y Metalúrgico – INGEMMET
dc.subjectVolcanes
dc.subjectErupciones volcánicas
dc.subjectImágenes
dc.subjectGeofísica
dc.subjectSensores remotos
dc.titleThe Huayruro Project: mapping the Calicanto Inca area buried by the A.D. 1600 Huaynaputina eruption, with geophysical imaging and remote sensing
dc.typeActas de congresos


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