Actas de congresos
The Huayruro Project: mapping the Calicanto Inca area buried by the A.D. 1600 Huaynaputina eruption, with geophysical imaging and remote sensing
Fecha
2018Registro en:
Antoine, 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.
10th International Cities on Volcanoes “Millenia of Stratification between Human Life and Volcanoes: strategies for coexistence”, Napoli, Italy, 2-7 September 2018. Abstracts Volume.
Autor
Antoine, Raphael
Macedo Franco, Luisa Diomira
Finizola, Anthony
Delcher, Eric
Thouret, Jean-Claude
Fauchard, Cyrille
Gusset, Rachel
Japura Paredes, Saida Blanca
Lazarte Zerpa, Ivonne Alejandra
Guilber, Vincent
Bacri, Clémentine
Normier, Adrien
Ramos Palomino, Domingo A.
Saintenoy, Thibault
Thouret, Liliane
Del Carpio, José
Puma, Nino
Institución
Resumen
We 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.