EGU26-2954, updated on 13 Mar 2026
https://doi.org/10.5194/egusphere-egu26-2954
EGU General Assembly 2026
© Author(s) 2026. This work is distributed under
the Creative Commons Attribution 4.0 License.
Poster | Tuesday, 05 May, 08:30–10:15 (CEST), Display time Tuesday, 05 May, 08:30–12:30
 
Hall X2, X2.26
The southernmost Central Volcanic Zone of the Andes: a natural laboratory for reconstructing the impact of large explosive Holocene eruptions (NEVA2)
Jose-Luis Fernandez-Turiel1, Alejandro Rodriguez-Gonzalez2, Francisco-Jose Perez-Torrado2, María del Carmen Cabrera2, Norma Ratto3, Edmundo Polanco4, David Benavente5, Noé N. García-Martínez5, and Esmeralda Estevez2
Jose-Luis Fernandez-Turiel et al.
  • 1GEO3BCN, CSIC, Barcelona, Spain (jlfernandez@geo3bcn.csic.es)
  • 2Institute of Environmental Studies and Natural Resources (i-UNAT), University of Las Palmas de Gran Canaria (ULPGC), Las Palmas de Gran Canaria, Spain
  • 3Instituto de las Culturas (UBA-CONICET), Ciudad Autónoma de Buenos Aires, Argentina
  • 4Plan Nacional de Geología, Servicio Nacional de Geología y Minería, Santiago, Chile
  • 5Department of Earth and Environmental Sciences, University of Alicante, San Vicente del Raspeig, Spain

NEVA2 explores the impacts of large explosive volcanic eruptions during the Holocene, with a focus on the southern end of the Central Volcanic Zone (CVZ) of the Andes. These rare but catastrophic events release enormous volumes of pyroclastic material and gases, reshaping landscapes for centuries and influencing the global climate. Despite their significance, the cumulative and cascading effects of these processes on the Earth’s critical zone—the interface of rock, soil, water, air, and life—as well as their role in past climate variability remain insufficiently constrained.

The project targets a unique natural laboratory in Chile and Argentina, where preliminary evidence suggests previously undocumented Holocene eruptions, including a major event at Nevado Tres Cruces volcano around 1,300 years BP (around the 8th century). This eruption appears to coincide with palaeoclimatic anomalies and cultural changes in pre-Hispanic societies, offering an exceptional opportunity to link geological, environmental, and archaeological records.

NEVA2 aims to identify and date large Holocene eruptions in the southern CVZ, model their dynamics and dispersal using advanced simulation tools, and assess multiscale impacts on the critical zone. It also seeks to correlate eruption timelines with palaeoclimate archives to evaluate associated climatic effects and disseminate findings to scientific communities, stakeholders, and the public.

Combining field surveys, laboratory analyses and modelling approaches, NEVA2 will deliver novel insights into volcanic hazards, provide new Holocene tephrochronological markers for the Southern Hemisphere, and contribute to improved risk mitigation strategies. The project also promotes education and stakeholder engagement to enhance resilience in volcanic regions.

The NEVA2 Project (Ref. ProID2024010012) is funded by the Canary Islands Agency for Research, Innovation and Information Society (ACIISI) and by the European Union under the Canary Islands ERDF Programme 2021–2027. Institutional support was provided by the GEOVOL research group (iUNAT, ULPGC) and Structure and Dynamics of the Earth (Generalitat de Catalunya, 2021 SGR 00413).

How to cite: Fernandez-Turiel, J.-L., Rodriguez-Gonzalez, A., Perez-Torrado, F.-J., Cabrera, M. C., Ratto, N., Polanco, E., Benavente, D., N. García-Martínez, N., and Estevez, E.: The southernmost Central Volcanic Zone of the Andes: a natural laboratory for reconstructing the impact of large explosive Holocene eruptions (NEVA2), EGU General Assembly 2026, Vienna, Austria, 3–8 May 2026, EGU26-2954, https://doi.org/10.5194/egusphere-egu26-2954, 2026.