INVENTORY AND CHARACTERIZATION OF SICILIAN BADLANDS

The United Nations Convention to Combat Desertification (UNCCD, 1994) addressed desertification as a global problem defining it as \u201cland degradation in arid, semi-arid, and dry sub-humid areas, resulting from various factors, including climate variations and human activity\u201d. In the Mediterranean areas, this phenomenon results from the interaction of various factors such as climate, lithology, vegetation and land use. The study of the predisposing factors allows the time/space assessment of the phenomenon and a continuous field monitoring allows to quantify the data in terms of vulnerability degree and to develop decision-making tools for integrated land use planning. One of the most fragile ecosystems are the badlands areas in Sicily. Their geological and climatic features (erosive rocks and marginal soils, and highly variable rainfall) and often a negative human impacts (inadequate land use and agricultural practices) led to increasing soil erosion and vegetation degradation, predisposing the terrain to the badlands. Moreover, the slope topography can be considered as a driver factor for the inception and the evolution of the badlands, in particular if we considered the badlands as miniature drainage systems, fully comparable to small river basins. The present work focused on the role of the pre-incision slope topography on the typologies and characteristics of the Sicilian badlands. The badlands areas of the entire Sicily were mapped in order to create an inventory of landforms based on morphological criteria. The digital orthophotos (2007-2008) at a nominal scale of 1:10.000 available in the WebGIS server of the Regione Sicilia and the Google Earth images of the same periods were closely examined. The landforms were digitized as polygons by means of a GIS software and recorded into a geo-database. The channel networks of each badland were traced and their drainage density (D) were calculated. The numbers of furrows directly tributary to the external drainage network were measured by using the index Gully Tributary (GT). This allowed to distinguish two typologies of badlands drainage pattern: dendritic for GT=1 (with only one main furrow) and parallel for GT>1 (with several parallel furrows). For each landform, the pre-erosion topography was reconstructed by filling the incision, using the heights of the watershed divide as point values in a topography interpolation tool in GIS. It represented the slope topography prior to the development of the current drainage network. The pre-incision slope morphometry of each landform was characterized by calculating the Morphometric Slope Index (MSI) considered as general index for slope morphometry. MSI, GT and D were compared via statistics in order to detect the influence of pre-erosion slope morphometry on the typology and the arrangement of the badlands drainage networks

Rockfall hazard assessment of the Monte Gallo Oriented Nature Reserve area (Southern Italy)

The Monte Gallo area is a carbonate relief that develops a significant nature reserve and highly attracts tourism to the urbanized area of the City of Palermo (Southern Italy). The slopes are affected by several rockfall events, which have also caused death, injuries, material damage, and a strong social and economic impact. Here, a detailed geological and geotechnical study to assess the rockfall hazard relating to two sectors of the mount has been carried out. The hazard assessment at the slope scale was performed based on geological, geomorphological, geomechanical, and seismic analysis. Using both analytical and empirical methods and by means of different software, the reconstruction of the propagation areas for the eastern sector of the Mount was possible. Results were used to better understand the overall structure, characterize the rockfall source areas' kinematics, and recognize the basic failure mechanisms. The obtained runout areas were compared with each other and with those of previous studies conducted in a neighboring area, as well as with the corresponding hazard area maps of the official cartography, which is being updated. It is expected to be supplemented with maps derived from empirical models

Geomorphology of the urban area of Palermo (Italy)

The results of a geomorphological study carried out in the urban area of Palermo are summarized in a thematic map. Field survey, analysis of aerial photographs and topographic maps, consultation of historical documents and maps, stratigraphic and topographic reconstruction from numerous wells and subsoil data, and bibliographic search were performed, in order to display the geomorphological changes produced by man over time in a densely populated area and to define the Anthropocene of the study area. Palermo town rises along large marine terrace surfaces cut by small river valleys and bordered by wide degraded and abandoned coastal cliffs. Over the last 2700 years, this area was affected by remarkable man-made changes to topographic surface and underground, exposing large areas of the city to hydraulic, sinkhole, and landslide risks, and increasing the levels of seismic susceptibility. In light of these results, the produced map is useful for urban planning studies

Combining multi-typologies landslide susceptibility maps: a case study for the Visso area (central Italy)

The research proposes a simple but geomorphologically adequate method to produce a combined landslide susceptibility map. In fact, in a logic of real use, offering type-specific landslide susceptibility maps to land use planners and administration could be not a successful solution. On the other hand, the simple grouping of more types of landslides could be misleading for model calibration considering that the relationships between slope failures and geo-environmental predictors should be conveyed by the abundance of each type of landslide resulting not specific and diagnostic for each typology. In this test, after having produced independent models for flow, slide and complex landslide by exploiting MARS (Multivariate Adaptive Regression Splines) and a set of type-specific geo-environmental variables, a combined landslide susceptibility map was obtained by combining the scores of the three source maps. The combined map was finally validated with a new unknown archive, showing very good performances

Analysis of the Rockfall Phenomena Contributing to the Evolution of a Pocket Beach Area Using Traditional and Remotely Acquired Data (Lo Zingaro Nature Reserve, Southern Italy)

The coastal domain of central western Sicily is characterized by the presence of rocky coasts, which mainly consist of pocket beaches situated between bedrock headlands that constitute ecological niches of great touristic and economic value. In this peculiar morphodynamic system, the sedimentary contributions are mainly derived from the rockfall that affects the back of nearby cliffs or the sediment supply of small streams that flow into it. In this study, we investigated the geomorphological processes and related landforms that contribute to the evolution of a pocket beach area located in a coastal sector of NW Sicily Island. The cliffs in this are affected by several rockfalls, and deposits from these rockfalls also add to the rate of sedimentary contribution. The analysis was conducted through the application of traditional approaches and contemporary methods that have previously been used to forecast the collection of input data in the field, often under difficult conditions due to the accessibility of the sites, and which have been supported by UAV surveys. Through the analysis of the digital models of terrain and orthophotos, geometrical and multitemporal analyses of landforms were carried out. A dedicated software was utilized for the detection of rockfall runout zones and block trajectories and for defining the automatic extraction of rock mass discontinuities. The data were compared with those derived from traditional geomechanical surveys. The availability of the existing and acquired remote sensing data proved essential for this study for both defining the reference geological model and for performing the site-specific analysis of rockfall

Rockfall hazards of Mount Pellegrino area (Sicily, Southern Italy)

A map derived by rockfall analysis at Mount Pellegrino is presented herein. The study area is affected by several phenomena of rockfall which caused numerous damage and a strong social and economic impact. Official reports and maps that give a general assessment of rockfall hazard are available in this respect, however, it would be advisable to provide a more specific cartographic support useful for land management and planning. The drafting of new maps showing the rockfall runout areas is an additional tool that may be used in conjunction with the existing maps as a means of risk mitigation and reduction. On the basis of geological, geomorphological, and geomechanical analysis and exploiting the information relating to a landslides inventory obtained by using both analytical and empirical methods, two different rockfall propagation areas were reconstructed. The final thematic map permit to appreciate the differences and similarities between the obtained runout areas

Geositi nel paesaggio mediterraneo: confronto tra aree costiere maltesi e siciliane.

Le isole maltesi mostrano aspetti geologici, geomorfologici e ambientali comparabili con quelli siciliani che danno luogo alla presenza di elementi paesaggistici ad elevata potenzialit\ue0 turistica, ad oggi non sufficientemente valorizzati. Nell\u2019ambito di un progetto di ricerca internazionale volto alla realizzazione di reti ecologiche transfrontaliere Malta-Sicilia (RE.MA.SI.), sono stati condotti studi sulla valorizzazione, divulgazione e corretta fruizione del patrimonio geologico di alcuni territori di queste due isole. Vengono qui presentati i risultati preliminari che hanno portato all'identificazione e valorizzazione di geositi di interesse geomorfologico, le cui caratteristiche sono state analizzate qualitativamente e quantitativamente, tramite l\u2019applicazione di metodologie gi\ue0 sperimentate a livello internazionale e basate sulla stima del loro valore scientifico, addizionale e di fruibilit\ue0. Sono state analizzate principalmente forme di rilevante interesse scientifico, didattico e paesaggistico, quali morfotipi costieri, evidenze morfologiche di processi gravitativi e di erosione idrica e forme carsiche

Predicting Earthquake-Induced Landslides by Using a Stochastic Modeling Approach: A Case Study of the 2001 El Salvador Coseismic Landslides

In January and February 2001, El Salvador was hit by two strong earthquakes that triggered thousands of landslides, causing 1259 fatalities and extensive damage. The analysis of aerial and SPOT-4 satellite images allowed us to map 6491 coseismic landslides, mainly debris slides and flows that occurred in volcanic epiclastites and pyroclastites. Four different multivariate adaptive regression splines (MARS) models were produced using different predictors and landslide inventories which contain slope failures triggered by an extreme rainfall event in 2009 and those induced by the earthquakes of 2001. In a predictive analysis, three validation scenarios were employed: the first and the second included 25% and 95% of the landslides, respectively, while the third was based on a k-fold spatial cross-validation. The results of our analysis revealed that: (i) the MARS algorithm provides reliable predictions of coseismic landslides; (ii) a better ability to predict coseismic slope failures was observed when including susceptibility to rainfall-triggered landslides as an independent variable; (iii) the best accuracy is achieved by models trained with both preparatory and trigger variables; (iv) an incomplete inventory of coseismic slope failures built just after the earthquake event can be used to identify potential locations of yet unreported landslides

Hydrogeological behaviour and geochemical features of waters in evaporite-bearing low-permeability successions: A case study in Southern Sicily, Italy

Knowledge about the hydrogeological behaviour of heterogeneous low-permeability media is an important tool when designing anthropogenic works (e.g., landfills) that could potentially have negative impacts on the environment and on people’s health. The knowledge about the biogeochemical processes in these media could prevent “false positives” when studying groundwater quality and possible contamination caused by anthropogenic activities. In this research, we firstly refined knowledge about the groundwater flow field at a representative site where the groundwater flows within an evaporite-bearing low-permeability succession. Hydraulic measurements and tritium analyses demonstrated the coexistence of relatively brief to very prolonged groundwater pathways. The groundwater is recharged by local precipitation, as demonstrated by stable isotopes investigations. However, relatively deep groundwater is clearly linked to very high tritium content rainwater precipitated during the 1950s and 1960s. The deuterium content of some groundwater samples showed unusual values, explained by the interactions between the groundwater and certain gases (H2S and CH4), the presences of which are linked to sulfate-reducing bacteria and methanogenic archaea detected within the saturated medium through biomolecular investigations in the shallow organic reach clayey deposits. In a wider, methodological context, the present study demonstrates that interdisciplinary approaches provide better knowledge about the behaviour of heterogeneous low-permeability media and the meaning of each data type