Agusto, Mariano, Lamberti, María Clara, Tassi, Franco, Carbajal, Fabricio, Llano, Joaquín, Nogués, Victoria, Núñez, Nicolás, Sánchez, Hernán, Rizzo, Andrea, García, Sebastián, Yiries, Jazmín, Vélez, María Laura, Massenzio, Antonella, Velasquez, Gabriela, Bucarey, Claudia, Gómez, Martín, Euillades, Pablo, and Ramos, Víctor
Over the past decade, we have conducted geochemical and isotopic monitoring of the fumarolic gases of the Peteroa volcano (Argentina‐Chile). Using the resulting data set, we constructed a conceptual model that describes the evolution of the magmatic‐hydrothermal system and identifies precursory geochemical signals of the last eruption. Our data set includes new chemical and isotopic analyses of fumarolic gas samples collected from 2016 to 2021, as well as previously published data from the 2010–2015 period. After an eruptive period in 2010–2011, the activity was characterized by low degassing rates and seismic activity. However, an increase in seismic activity and fumarolic gas emissions was observed from 2016 to 2018–2019 eruptive episode, leading to a major phreato‐magmatic eruption. Fumarole gases show different compositions during quiescent versus unrest/eruptive degassing related to the interaction of deep (magmatic) and shallow (hydrothermal) fluid contributions. During quiescent periods, fumaroles exhibited low SO2/H2S, HF/CO2, and HCl/CO2 ratios (<0.1), revealing a dominant hydrothermal contribution. In contrast, during pre‐and syn‐eruptive periods, fumaroles showed ratios up to 100 times higher indicative of an enhanced magmatic input. When compared to the evolution of the seismic activity, the increment of magmatic‐related strong acidic gases suggests repeated inputs of hot magmatic fluids, which are only partially dissolved into the hydrothermal system feeding the fumaroles. Interestingly, the 3He/4He and δ13C‐CO2 values remained relatively constant during the magmatic and hydrothermal degassing in 2016–2021, suggesting that the deep magmatic gas source did not significantly change throughout variations in Peteroa's activity.Plain Language Summary: The Peteroa volcano is an active volcano located in the southern Andes Mountains of South America. It has erupted multiple times in recent years, but there is limited knowledge about its behavior and potential damage it could cause. To address this, we have been studying the volcano for the past decade using special techniques to examine the gases that come out of the openings in the ground, known as fumaroles. These fumaroles allow volcanic gases to escape, and by collecting data on fumarolic gas samples from 2010 to 2021, we have developed a model that helps us understand how the volcano changes over time and identify warning signs of an upcoming eruption. Our research found increased seismic activity and fumarolic gas emissions starting in 2016, leading to a significant eruption from 2018 to 2019. We also discovered that the composition of the fumarolic gases varies depending on whether the volcano is in a quiet or unrest period. During quiet periods, the gases show compositions with a stronger influence from underground water, but before and during the 2018–2019 eruption, the gas compositions showed changes indicating a more significant influence of magma. This study is vital as it enhances our understanding of volcano behavior and provides valuable insights for forecasting future eruptions. This is particularly important in the region as there are many potentially dangerous volcanoes with limited available information, but the findings can be applied to improve our understanding of other volcanoes, ultimately contributing to the global knowledge base on volcanic processes.Key Points: Geochemical and isotopic monitoring of Peteroa volcano allowed us to elaborate a conceptual model that explains the evolution of the magmatic‐hydrothermal systemFumarolic gases exhibit different compositions during quiescent and unrest/eruptive periods, allowing the identification of precursory signals of the last eruptionDespite variations in activity, the deep magmatic gas source of Peteroa volcano remained relatively constant, as indicated by consistent He and C isotopic values [ABSTRACT FROM AUTHOR]