I satelliti del programma europeo Copernicus hanno confermato i dati sulla deformazione della faglia che ha scatenato il terremoto di Messina del 1908. Questi dati sono di importanza cruciale anche per la corretta progettazione del ponte. L’ubicazione in mappa, i tassi di attività tettonica e le dimensioni della faglia rappresentano gli elementi fondamentali per la stima delle azioni sismiche.
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