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After the November 10, 2009 event occurring in the northern sector of the island (the town of Casamicciola), a detailed geo-morphological survey was conducted to ascertain the evolution of the phenomenon.

In the watersheds upstream of Casamicciola, many landslides were mapped and the volume of material involved during detachment and sliding was estimated.

In the lower course area, near the town and towards the sea, flow pathways were reconstructed with the aid of extensive video footage taken during the event.

Rainfall data were also analyzed and a relationship was established between the hourly rainfall rate and the flash flood.

The phenomenon was found to be quite complex, with many upstream landslides stopping before reaching the urban area.

In the lower course the alluvial event occurred as a flood with a very small sediment discharge, which left a very thin layer of sediment.

Reconstruction of the flash flood phenomenon suggested possible action for future risk mitigation, early warning and civil protection plans.

Highlights Flash flood hazard scenario in especially vulnerable Mediterranean area.

Historical analysis of the landslides and floods of Ischia island, Italy.

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