Here are the papers I will talk about: Dupont de Dinechin et al. (2025), doi.org/10.1007/s004... and Ostorero et al. (2022), doi.org/10.1038/s432...

Really looking forward to seeing you there!

Many great seminars will be given each week by other ECRs within this series so stay tuned!

The schedule: e5k.github.io/IAVCEI-SA202...
We can't wait to see you there! 🌋
@charlinator.bsky.social @albertocaracciolo.bsky.social @magmafc.bsky.social @simonecosta.bsky.social

#IAVCEI2025

@iavcei.bsky.social #IAVCEI2025

The schedule: e5k.github.io/IAVCEI-SA202...
We can't wait to see you there! 🌋
@charlinator.bsky.social @albertocaracciolo.bsky.social @magmafc.bsky.social @simonecosta.bsky.social

I carried out this research as a PhD student at @ipgp.bsky.social and @upcite.bsky.social, in collaboration with colleagues from other institutes that I thank again: ISTeP, ISTO, @universityofleeds.bsky.social, the Institute of Volcanology and Seismology in Kamchatka and Lomonosov University!

⏱️In Part II, we tracked magmatic processes over twelve years prior to the eruption, followed by magma ascent to a shallow reservoir and a heating process at least three months before the eruption. Magma was last stored in a cryptodome at least two months before the climactic phase of the eruption.

🌋Our Part I paper (Martel et al., 2025) identified a three-level magma storage below Bezymianny: a deep reservoir, a shallow reservoir in which the pre-cryptodome magma resided and from which the post-blast pumiceous magma originated, and a subsurface cryptodome from which the blast was initiated.