San Felice a Cancello post-fire debris flow

LCI : .
Main Information
Landslide Name : San Felice a Cancello post-fire debris flow
Latitude : 41:0:9.69 N
Longitude : 14:30:34.74 E
Location
City / District : San Felice a Cancello
Province : Campania
Country : Italy
Reporter
Reporter 1 : Stefano Luigi Gariano
Reporter 2 : Giuseppe Esposito
Landslide Type
Material : Debris
Movement : Flow
Velocity (mm/sec) : Extremely Rapid
Depth (m) : Surficial
Slope (degree) : Steep
Volume (m³) : Small
Date of Occurence
Date of Occurence : Aug 27, 2024
Other Information
Land Use Source area : Forest, Pasture
Run-out/deposition area : Urban area, Road
Other Activity : Active in the past
Triggering Factor : Rainfall
Death(s) & Missing : 2
Houses and other structural damage : extensive damage to the road network, and the ground and basement floors of many buildings
Photo of landslide :
Google earth kmz file : watershed.kmz
Plan of landslide : -
Cross section of landslide :
Reference (paper/report) : Esposito, G., Gariano, S. Overview of the first fatal post-fire debris flow event recorded in Italy. Landslides 22, 2131–2139 (2025). https://doi.org/10.1007/s10346-025-02516-
Testing graph : -
Monitoring graph : -
Video of moving landslides including 3D simulation : https://www.youtube.com/watch?v=QW8_3lo03yI
Description :

On 27 August 2024, a large part of the Campania region, southern Italy, was affected by intense rainfall associated with forming local storm cells forced by orography. Three watersheds affected by wildfires some weeks before (3 and 14 August 2024) responded to rainfall with intense runoff and erosion processes supplying debris and hyperconcentrated flows downstream. In the town of San Felice a Cancello, a post-fire debris flow hit the urban fabric causing extensive damage to the road network, and the ground and basement floors of many buildings. The closest rain gauge recorded 29.2 mm in 20 min, as well as a peak intensity in 30 min of 83.6 mm/h. The highest peak intensity in 10 min was 106.8 mm/h. Landforms related to gully erosion generated by the runoff concentration were observed in the highest part of low-order channels, likely associated with rill and interrill erosion processes. A lot of sediments resulted from the incision of steep drainage channels and was carried out by turbulent flows. When hitting the urban fabric, flows poured down very fast along the roads and changed their rheology gradually along their paths downstream, transitioning from high-magnitude debris flows through to hyperconcentrated flows. Due to high sediment concentrations and human modifications of the drainage sections, the flows abandoned the natural drainage network to overwhelm roads and buildings. In the urban center of San Felice a Cancello, a vehicle with two people on board was dragged by flows for about 800 m. The vehicle was found a few hours after the accident. The two lifeless bodies were found only after long searches in a former quarry 2 km away from the impact point on 2 and 12 of September, respectively. This was the first known post-fire debris flow with fatal consequences in Italy.