Advances in Geosciences
Advances in Geosciences
ADGEO
Articles | Volume 52
Articles | Volume 52
https://doi.org/10.5194/adgeo-52-119-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/adgeo-52-119-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
Articles | Volume 52
18 Feb 2021
 | 18 Feb 2021

Aseismic strain episodes at Campi Flegrei Caldera, Italy

Bellina Di Lieto, Pierdomenico Romano, Roger Bilham, and Roberto Scarpa

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Latest update: 25 Apr 2024
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Short summary
Changes to a volcanic edifice and its surroundings can be caused by movements of underground magma, gas or other fluids (typically water). These deformations are usually very small in magnitude, so very sensitive instruments are the only capable of detecting them. A discrimination between deformations caused by volcanic processes in regards to those caused by external sources could help in understanding the volcano dynamics and give scientists a way to forecast volcanic eruptions.
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