Abstract
In mountainous urbanized areas, shallow landslides cause significant, often unpredictable, hazard conditions. Landslides may involve and destroy infrastructures, kill people. Source areas are often located along the road network, representing a recurring situation also during not heavy rainstorms in Northern Tuscany. The landslides are generally first time debris slide-flows, occurring in peculiar environments: colluvium/debris slope cover (0.5–2 m thick), semipermeable-impermeable bedrock, hollow shaped slope, high slope gradient. Despite little size, they cause damage and deaths owing to their high velocity and erosion power. The source area along the road network is generally associated to the lack of efficient drainage systems. In fact, the concentration of uncontrolled runoff downslope creates an “unnatural” increase in pore pressure that the only rainfall should not have produced. This generates reaching and exceeding of the local critical rainfall threshold, making landslide hazard assessment more difficult. As example, in October 2010, almost 60 % of the landslides source area in the Massa area was located along the road network.
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Acknowledgments
The Authors are grateful to the Tuscan Region Hydrologic Service (in particular to Dr. Luca Pisani) and to the Agro-meteorological Regional Agency (A.R.S.I.A.) for giving the rainfall data. The Authors thanks the Reviewers for the useful suggestions.
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Avanzi, G.D., Galanti, Y., Giannecchini, R., Puccinelli, A. (2013). Fragility of Territory and Infrastructures Resulting from Rainstorms in Northern Tuscany (Italy). In: Margottini, C., Canuti, P., Sassa, K. (eds) Landslide Science and Practice. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-31319-6_33
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DOI: https://doi.org/10.1007/978-3-642-31319-6_33
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