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2013 | OriginalPaper | Buchkapitel

The Susceptibility Map for Landslides with Shallow Initiation in the Emilia Romagna Region (Italy)

verfasst von : Mauro Generali, Marco Pizziolo

Erschienen in: Landslide Science and Practice

Verlag: Springer Berlin Heidelberg

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Abstract

The Emilia Romagna Region (RER) is probably one of the most landslide susceptible regions of the world, with ~24 % of the mountain sector covered by landslide accumulations. The regularly updated 1:10,000 Landslides Inventory Map (LIM), managed by the Regional Geological Survey, counts more than 70,000 landslides. Nowadays most land-use planning is based on LIM but this has several intrinsic shortcomings, mainly due to its scale and forecast significativity. This paper presents the methods we used to compile a detailed susceptibility map for the whole RER Apennines.
The triggering mechanism of the most common landslides phenomena in RER, disregarding of the subsequent evolution, is characterized by a first movements that may be described as “shallow phenomena” involving the upper part of the landslides (depletion areas). For this reasons we developed a model for the areas “outside” the LIM mapped landslides aimed to identify the triggering areas for future landslides. For this statistical analysis we used Bivariate Logistic Regression methods. As our aim was to predict triggering phenomena, we calibrated the model on the depletion areas, selected using a semi-automatic GIS procedure. The resulting map can be used for LIM verification and updating and adds it a forecast connotation useful for land use planning; nevertheless it has to be used by experienced users, for this purpose the model advantage and shortcomings will be discussed.

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Fußnoten
1
The State of activity definition doesn’t correspond to that used by Varnes (1978), WP/WLI (1993) or Cruden and Varnes (1996), but assume as active a landslide that has shown activity in the last ~30 years.
 
2
We used the Zevenbergen and Thorne (1987) algorithm that performs better then others on sharp slope changes.
 
3
For the flow accumulation we used the D∞ algorithm (Tarboton 1997), that performs much better then D8 to identify the accumulation/dispersion of water flow along the hillslopes.
 
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Metadaten
Titel
The Susceptibility Map for Landslides with Shallow Initiation in the Emilia Romagna Region (Italy)
verfasst von
Mauro Generali
Marco Pizziolo
Copyright-Jahr
2013
Verlag
Springer Berlin Heidelberg
DOI
https://doi.org/10.1007/978-3-642-31325-7_57