06/18/2026
The plumbing systems of volcanoes are vast and complex. But they aren’t consistent, even within the same volcano.
A recent Cornell University-led study co-authored by Lamont-Doherty Earth Observatory geochemist/volcanologist Terry Plank and colleagues found very different mechanisms behind two historic eruptions of Italy’s Mount Etna, one of the tallest active volcanoes in Europe.
In one eruption, water-rich magma rose and stalled at shallow depths before erupting; in another, carbon dioxide-rich magma rose quickly from much deeper underground. Understanding these dynamics can help geologists assess the risk of future eruptions.
“Etna is such a tourist destination today for climbers and skiers, but it had these very explosive eruptions in the past. The textbooks say that these hot, mafic magmas that erupt from Etna can’t be explosive. Our work shows the power of CO2,” says Plank.
Learn more: https://lamont.columbia.edu/news/carbon-dioxide-and-water-played-key-roles-historic-mount-etna-eruptions
📷 Mount Etna volcano in Sicily, Italy. Courtesy: Esteban Gazel