A partire dalle ore 5 di stamane UTC la rete di monitoraggio del Laboratorio di Geofisica Sperimentale - Dipartimento di Scienze della terra dell’Università di Firenze ha registrato un aumento dell’attività di spattering al cratere di NE e un aumento del tremore sismico: a seguito del quale è avvenuta un’ulteriore fase di trabocco lavico.
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