scholarly journals Supplemental Material: Magma recharge patterns control eruption styles and magnitudes at Popocatépetl volcano (Mexico)

2021 ◽  
Author(s):  
Martin Mangler ◽  
et al.

Items S1 (full time scale datasets), (S2) diffusion model details, and S3 (priming durations for eruptions with published time-scale data).<br>

2021 ◽  
Author(s):  
Martin Mangler ◽  
et al.

Items S1 (full time scale datasets), (S2) diffusion model details, and S3 (priming durations for eruptions with published time-scale data).<br>


Geology ◽  
2022 ◽  
Author(s):  
Martin F. Mangler ◽  
Chiara Maria Petrone ◽  
Julie Prytulak

Diffusion chronometry has produced petrological evidence that magma recharge in mafic to intermediate systems can trigger volcanic eruptions within weeks to months. However, less is known about longer-term recharge frequencies and durations priming magma reservoirs for eruptions. We use Fe-Mg diffusion modeling in orthopyroxene to show that the duration, frequency, and timing of pre-eruptive recharge at Popocatépetl volcano (Mexico) vary systematically with eruption style and magnitude. Effusive eruptions are preceded by 9–13 yr of increased recharge activity, compared to 15–100 yr for explosive eruptions. Explosive eruptions also record a higher number of individual recharge episodes priming the plumbing system. The largest explosive eruptions are further distinguished by an ~1 yr recharge hiatus directly prior to eruption. Our results offer valuable context for the interpretation of ongoing activity at Popocatépetl, and seeking similar correlations at other arc volcanoes may advance eruption forecasting by including constraints on potential eruption size and style.


Geology ◽  
2009 ◽  
Vol 37 (2) ◽  
pp. 107-110 ◽  
Author(s):  
Julie Roberge ◽  
Hugo Delgado-Granados ◽  
Paul J. Wallace

Author(s):  
Quetzalcoatl Rodríguez-Pérez ◽  
Marisol Monterrubio-Velasco ◽  
F. Ramón Zúñiga ◽  
Carlos M. Valdés-González ◽  
Raúl Arámbula-Mendoza

2003 ◽  
Vol 13 (03n04) ◽  
pp. 133-139 ◽  
Author(s):  
F. ALDAPE ◽  
J. FLORES M.

Samples of airborne particulate matter were collected in four sites along an east-west line from the Popocatépetl volcano after the eruption episode of June 30, 1997. The Popocatépetl volcano, with variable activity since it was known, is currently under low but continuous activity prolonged for almost one decade, with occasional moderate eruption episodes producing mainly fumes, ashes and volcanic dusts. The main objective of this study is to determine whether or not some elements have increased their presence in the atmosphere as a result of the volcanic activity, and also if some others, not usually found in urban aerosols, have appeared because of the same reason. In addition, the information obtained will be a source of scientific data for health risk assessment of the population exposed to volcanic emanations. The sample collection was performed on alternate days from July 10 to August 13 1997 in Puebla and Atlixco in Puebla State. Tlalpan within Mexico City, and Salazar in the State of Mexico. Two samples a day were taken in two periods: 7-19 h and 19-7 h. The samplers separated particles into two particle size fractions. PM25 and PM15. Elemental concentrations were determined by PIXE and the results obtained showed increased concentrations of mainly Ti and Fe in all sampling sites, thus indicating a long range transportation of volcanic dusts in both particle size fractions. Concentrations of Ti were found clearly above the average values of urban areas such as Mexico City, and although this element can be considered of low toxicity, the biological, metabolic and toxic effects on human beings are still under investigation.


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