History of Sicily unrest enjoyed wide support in Messina and produced an organized structure, and consciousness of the need to link the struggle to the whole of Sicily. The insurgents briefly gained control of the city but, despite bitter resistance, the Bourbon army was victorious and suppressed the revolt. This suppression resulted in further oppression and created a diaspora of Messinian and Sicilian revolutionaries outside Sicily and locked Sicily under the control of the reactionary government. The bombardments of Messina and Palermo earned Ferdinand II the name "King Bomba". "See also: " Sicily was merged with the Kingdom of Sardinia in 1860 following
Geology of Sicily well as the regional uplift of the Calabrian unit. The tectonic setting of Sicily is controlled by the rate of collision of the African plate and Eurasian plate and the rate of back rolling of the African plate. The tectonic history of Sicily can be divided into four main stages: During Late Triassic, the ancient Neotethys ocean was formed by a major continental rifting event and rapid tectonic subsidence. Traces of the tectonic event can be found at both the Hyblean plateau and western Sicily. After the rapid subsidence during Triassic to Early Jurassic, there was a slow thermal subsidence