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Geological and structural evolution of tectonically active areas of the central Calabria Arc
(2016-03-04)
The Catanzaro Trough is a Neogene-Quaternary basin developed between the Serre
and the Sila Massif, filled by up to 2000 m of Upper Miocene to Quaternary sedimentary
succession, belonging to the central Calabrian Arc and ...
Valutazione della scuscettibilità e degli scenari di pericolosità e di rischio da frana in aree di interesse socio-economico (Calabria Settentrionale)
(2016-02-02)
Landslides are natural geologic processes that play a key role in landscape evolution, but
represent also one of the most widespread natural hazard in Italian territory. In particular, many
areas of the Calabria region ...