New research led by Carnegie’s Hélène Le Mével reveals new details about the system of magma chambers under the Hunga volcano, both before and after its disastrous 2022 eruption. The team’s findings, published last week in Science Advances, demonstrate a new method for probing submarine volcanoes for their potential to cause similar damage.
The eruption came at the end of a month-long period of volcanic unrest, following a seven-year hiatus for the volcano—devastating the Kingdom of Tonga islands and causing a global tsunami, an unprecedented amount of volcanic lightning, and perturbations in the upper atmosphere. . It was the largest explosive eruption recorded since Pinatubo in 1991.
“Although we have a wealth of data about the Hunga eruption’s effects both locally and globally, we know very little about its subsurface structure,” Le Mével explained.







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