Abstract
At Mount Etna volcano, the focus point of persistent tectonic extension is represented by the Summit Craters. A muographic telescope has been installed at the base of the North-East Crater from August 2017 to October 2019, with the specific aim to find time related variations in the density of volcanic edifice. The results are significant, since the elaborated images show the opening and evolution of different tectonic elements; in 2017, a cavity was detected months before the collapse of the crater floor and in 2018 a set of underground fractures was identified, at the tip of which, in June 2019, a new eruptive vent started its explosive activity, still going on (February, 2020). Although this is the pilot experiment of the project, the results confirm that muography could be a turning point in the comprehension of the plumbing system of the volcano and a fundamental step forward to do mid-term (weeks/months) predictions of eruptions. We are confident that an increment in the number of telescopes could lead to the realization of a monitoring system, which would keep under control the evolution of the internal dynamic of the uppermost section of the feeding system of an active volcano such as Mount Etna.
Highlights
At Mount Etna volcano, the focus point of persistent tectonic extension is represented by the Summit Craters
Once a fracture is open, it is filled with high temperature volcanic gas, which has a very low density compared to surrounding basaltic rock
Note that this value is similar to what is recorded in the top-most region of North-East Crater (NEC), where the traversed thickness is lower, and the cumulative density is equal to that of standard rock
Summary
At Mount Etna volcano, the focus point of persistent tectonic extension is represented by the Summit Craters.
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