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dc.contributor.author Finizola, Anthony
dc.contributor.author Macedo Franco, Luisa Diomira
dc.contributor.author Antoine, Raphael
dc.contributor.author Thouret, Jean-Claude
dc.contributor.author Delcher, Eric
dc.contributor.author Fauchard, Cyrille
dc.contributor.author Gusset, Rachel
dc.contributor.author Japura Paredes, Saida Blanca
dc.contributor.author Lazarte Zerpa, Ivonne Alejandra
dc.contributor.author Mariño Salazar, Jersy
dc.contributor.author Ramos Palomino, Domingo A.
dc.contributor.author Saintenoy, Thibault
dc.contributor.author Thouret, Liliane
dc.contributor.author Chávez, José Antonio
dc.contributor.author Chijcheapaza, Rolando
dc.contributor.author Del Carpio Calienes, José Alberto
dc.contributor.author Perea, Ruddy
dc.contributor.author Puma Sacsi, Nino
dc.contributor.author Macedo Sánchez, Orlando Efraín
dc.contributor.author Torres Aguilar, José Luis
dc.contributor.author Vella, Marc-Antoine
dc.date.accessioned 2018-11-09T10:42:35Z
dc.date.available 2018-11-09T10:42:35Z
dc.date.issued 2017-11
dc.identifier.uri http://hdl.handle.net/20.500.12816/3482
dc.description Resumen de artículo presentado en el "I Congreso Internacional del Cambio Climático y sus Impactos" (International Congress on Climate Change and its Impacts-Abstracts Volume), realizado del 29 noviembre al 1 diciembre del 2017, en la ciudad de Huaraz-Ancash, Perú. es_ES
dc.description.abstract The February-March CE 1600 eruption of Huaynaputina (VEI 6) has a well-documented worldwide climatic impact but the regional consequences of this eruption on climate, habitat and inhabitants are poorly known. The location of several villages buried below the Huaynaputina erupted deposits exceeding one meter in thickness is not clearly mentioned in the historical early Spanish chronicles. Geophysical investigations carried out during the20 15-2016 period on three different sites (Coporaque, Calicanto and Chimpapampa within 16 km from the volcano summit/crater) are the initial stage and part of a large project termed <<HUAYRURO», the objective of which is to better understand the physical and socio-economic impacts of the CE 1600 Huaynaputina eruption. An array of geophysical methods and tools was used: one drone to obtain high-resolution digital elevation models using aerial photographs, georadar 3D imaging, magnetism, infrared pictures, and electromagnetic measurements. These first two years of preliminary geophysical investigation have allowed us to clearly identify a future strategy and select the best device to map as fast as possible one of the areas, namely Calicanto, defining the X, Y and Z location of the walls of the settlements and the extent of the buried village. This map is the basis on which the future tephro-stratigraphical and archeological studies will be built up. The final goal of this project is to disseminate the results of the multi-disciplinary study to a large audience including an onsite museum. es_ES
dc.format application/pdf es_ES
dc.language.iso eng es_ES
dc.publisher Sociedad Geológica del Perú es_ES
dc.rights info:eu-repo/semantics/openAccess es_ES
dc.rights.uri https://creativecommons.org/licences/by/4.0/ es_ES
dc.subject Volcanoes es_ES
dc.subject Volcanic eruptions es_ES
dc.subject Geophysical investigation es_ES
dc.subject Volcanology es_ES
dc.subject Volcán Huaynaputina es_ES
dc.title Physical impacts of the CE 1600 Huaynaputina eruption on the local habitat: geophysical insights es_ES
dc.type info:eu-repo/semantics/conferenceObject es_ES
dc.subject.ocde http://purl.org/pe-repo/ocde/ford#1.05.07 es_ES

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