Reconstructing the Gorte and Spiaz de Navesele Landslides, NE of Lake Garda, Trentino Dolomites (Italy)

We applied a multi-method approach to reconstruct the Gorte rock avalanche (85-95 Mm(3)) located at the northeastern end of Lake Garda. The combination of field mapping, characterization of bedrock discontinuities, Dan3D-Flex runout modeling and dating of boulders with cosmogenic Cl-36 supports the conclusion that the deposits stem from a single rock avalanche at 6.1 & PLUSMN; 0.8 ka. The Gorte event may have triggered the Spiaz de Navesele-Salto della Capra landslide (3.2 Mm(3)), whose deposits cover the southern end of the Gorte deposits. First-order controls on detachment were the NNE-SSW- and WNW-ESE-oriented fractures in the limestone bedrock, related to the Giudicarie and Schio-Vicenza fault systems, respectively. Dan3D-Flex runout modeling sufficiently reproduced the Gorte rock avalanche, which involved detachment and sliding of a quasi-intact block, likely along marly interbeds, followed by rapid disintegration. The frictional rheology in the source area and the turbulent frictional rheology (Voellmy) in the remaining part best replicate the observed deposit extent and thickness. Heavy precipitation that occurred at that time may have contributed to failure at Gorte. Nonetheless, its timing overlaps with the nearby (< 15 km) Dosso Gardene (6630-6290 cal BP) and Marocca Principale (5.3 & PLUSMN; 0.9 ka) landslides, making a seismic trigger plausible.

Automated summary

A multi-method approach was used to reconstruct the Gorte rock avalanche at the northeastern end of Lake Garda, suggesting it occurred around 6.1±0.8 ka. The event may have triggered the Spiaz de Navesele-Salto della Capra landslide, with related deposits covering the southern end of the Gorte deposits. This study highlights the potential for seismic triggers in the region.