G.M. Crisci, R. Rongo, V. Lupiano, G. Niceforo, G. Iovine., 2006, A Methodological Example of Lava-Flow Hazard Zonation in the SE Sector of the Etna Volcano (Sicily Southern Italy),
3rd AOGS (Asia Oceania Geosciences Society) Annual Meeting, Singapore, 10-14 luglio 2006,
D. DAmbrosio, W. Spataro, G. Iovine, M.V. Avolio, G.M. Crisci, S. Di Gregorio, R. Rongo, G.A. Trunfio, V. Lupiano., 2006, Macroscopic Cellular Automata Approach For Modelling Superficial Dangerous Geological Processes.,
Washington, D.C.)., 2006,
G. Iovine, O. Petrucci, V. Rizzo, C. Tansi., 2006, The March 7th 2005 Cavallerizzo (Cerzeto) landslide in Calabria – Southern Italy. Proc. Geol. Soc. of London (in CD).,
Engineering geology for tomorrow's cities. The 10th IAEG Congress, Nottingham, UK, 6-10 September,
W. Spataro, M.V. Avolio, S. Di Gregorio, G.M. Crisci, D. D`Ambrosio, R. Rongo, G. Iovine, V. Lupiano, 2006, Surface Flows Modelling_ Cellular Automata Simulations of Lava Flows, Debris Flows and Pyroclastic Flows,
Third iEMSs Biennial Meeting "Summit on Environmental Modelling and Software", The Wyndham Hotel (Burlington, Vermont), 9-12 luglio 2006,
Petrucci O.; Polemio M., 2006, Characterisation of drought effect on groundwater of a coastal plain (Southern Italy),
Geophysical research abstracts 8 (2006): 3644–3644.,
Abstract
Main droughts recently occurred in Calabria and regional sectors hardest hit have been
found carrying out ...
Main droughts recently occurred in Calabria and regional sectors hardest hit have been
found carrying out an historical research. A regional newspaper has been selected as an
information source and articles concerning drought have been selected for the period
among 1980 to 2004. Data inferred from the articles have been organized in a database
in which both hit areas and damaged sectors have been highlighted.
During the study period, the northern sector of Calabria has been hit the hardest. On
this sector additional data have been found in order to better understand the effects of
drought on groundwater availability, particularly on the Sibari Plain, the main costal
plain of Calabria.
For this reason, the climatic trend and the occurrence/duration of exceptionally dry
periods have been investigated, based on long rainfall and temperature time series. In
addition, in order to characterize the effects of droughts periods on the availability of
groundwater, piezometric data, which had been collected from the thirties, have been
compared to 2002 and 2005 in-situ measurements.
At the end a geo-database has been implemented including too climatic and hydrogeological
data.
The analysis shows a remarkably negative rainfall trend and a widespread piezometric
lowering.
Petrucci O.; Iovine G.; Caloiero T.; Pasqua A.A., 2006, Frequency of disastrous hydrogeological events in northern Calabria from historical information,
Geophysical research abstracts (Online) 8 (2006): 2351.,
Abstract
Disastrous Hydrogeological Events (DHEs) can be defined as the complex of landslide and flood phenomena ...
Disastrous Hydrogeological Events (DHEs) can be defined as the complex of landslide and flood phenomena induced by either heavy or prolonged rainfall. As these latter can simultaneously trigger different types of phenomena, DHEs represent multiplehazard events, which commonly cause huge economic losses and damage in many areas of the Earth. Owing to its geological, geomorphological and climatic characteristics,
Calabria is frequently hit by disastrous hydrogeological events. The ASICal database (Italian acronym for Historically Flooded Areas in CALabria) has recently been implemented, by collecting historical information on landslides and floods occurred during the past centuries, and on related damage (the database is accessible on-line at http_\www.camilab.unical.it). In the present study, historical and hydrologic information concerning DHEs occurred in Northern Calabria (Cosenza province) have been analysed in detail, aiming at exploring the climatic conditions which characterised the main hydrogeological crises. Rainfall data recorded at n.88 rain gauges, uniformly distributed in the study area, have first been statistically analysed, aiming at characterising the most severe rainfall periods. Moreover, the series of the principal damaging events has been reconstructed, and the spatial distribution of damage plotted. Despite it is only a sub-sample of the "complete" history of damage actually suffered in Northern Calabria, this series can be assumed as representative of the most severe damaging events, and it can be compared with the results of the hydrologic analysis. Events have been classified on the base of the severity of damage; rainfall occurred before each event has then been analysed in terms of cumulative values, in order to assess its exceptionality. By considering the results of historical analyses, villages' territories have been classified on the base of frequency of damage. Rainfall periods responsible of principal damaging events have also been typified (in terms of intensity and duration), and their return periods assessed. For each village, the most recurrent phenomena and vulnerated sites/elements have then been recognised. Performed analyses can be helpful in defining scenarios and strategies for risk management in the study area.
AVOLIO M.V. (1), CRISCI G.M. (2), DAMBROSIO D. (1), DI GREGORIO S. (1), IOVINE G. (3), LUPIANO V. (3), RONGO R. (2), SPATARO W. (1), TRUNFIO A. (1), 2006, Explicit velocity for Modelling Surface Complex Flows with Cellular Automata and Applications,
Systemics of Emergence_ Research and Development,, edited by MINATI G., PESSA E. & ABRAM M., pp. 79–92. New York_ Springer New York, 2006,
Betrò B.; Bodini A.; Cossu A.; Gullà G.; Terranova O.;, 2006, A hidden Markov model for daily rainfall occurrence over souther Calabria Ionica (Italy).,
XLIII Riunione Scientifica della Società Italiana di Statistica, Torino, 14-16 Giugno 2006,
Abstract
Si presenta un'analisi statistica della serie temporali giornaliere delle piogge,
schematizzate come fenomeno binario, relativamente ad ...
Si presenta un'analisi statistica della serie temporali giornaliere delle piogge,
schematizzate come fenomeno binario, relativamente ad un'area della Calabria Ionica
Meridionale. Fra le 45 stazioni disponibili per quest'area sono state selezionate quelle, 5,
che possiedono un periodo di osservazione comune sufficientemente lungo e completo. In
particolare si `e considerato il trentennio 1961-1990. Il fenomeno `e stato quindi modellato
tramite un cosidetto hidden Markov process.
Avolio M.V. (1), Crisci G.M. (2), DAmbrosio D. (1), Di Gregorio S. (1), Iovine G. (3), Lupiano V. (3), Rongo R. (2), Spataro W. (1), 2006, Surface Flows Modeling_ Cellular Automata Simulation of Lava, Debris and Pyroclastic Flows.,
3rd iEMSs Biennial Meeting Summit on Environmental Modelling and Software, Burlington, USA, July 9-13, 2006,
Abstract
Cellular Automata (CA) are a computational paradigm, a valid alternative to standard methods
with differential ...
Cellular Automata (CA) are a computational paradigm, a valid alternative to standard methods
with differential equations for modelling and simulating complex systems, whose behaviour may be
specified in terms of local interactions in a context of discrete time and space. Some surface flows may be
approximated to such a type of complex systems. The Empedocles Research Group developed an empirical
methodology for modelling this kind of macroscopic phenomena. The CA space for surface flows is divided
in hexagonal cells, whose specification (state) describes the physical characteristics (substates) relevant to
the evolution of the system and relative to the space portion corresponding to the cell. The cell neighbouring,
specifying the interaction range, is given by its adjacent cells. The evolution of the phenomenon is obtained
by updating the values of the substates simultaneously at discrete time steps in all the cellular space
according to the CA transition function, which is split in sequential "elementary" processes. This CA
methodological approach for modelling large scale surface flows was applied to lava flows (the model
SCIARA), pyroclastic flows (the PYR model) and debris flows (the SCIDDICA model). Satisfying
simulations of real events are exhibited_ the NE flank lava flows of the 2002 Etnean eruption, the pyroclastic
flows invading the Sacobia area during the 1991 eruption of Mount Pinatubo in the island of Luzon (The
Philippines Islands), the Chiappe di Sarno (Italy) catastrophic debris flows on 1998.
Crisci G.M., Rongo R., DAmbrosio D., Di Gregorio S., Spataro W., Iovine G., 2006, Some results from PYR, a simple Cellular Automata model for pyroclastic flow.,
VIII Congresso SIMAI, Baia Samuele (RG), 2006,
Iovine G., 2006, Problematiche di instabilità superficiale dei versanti.,
Seminario su Problematiche di instabilità superficiale dei versanti e Tecniche di bonifica, 2006,
Iovine G., 2006, Metodo per la valutazione delle zone esposte al problema delle colate detritiche.,
Seminari specialistici Strumenti avanzati di Ricerca Applicata per la Tutela del Territorio, 2006,
Avolio M.V., Crisci G.M., DAmbrosio D., Di Gregorio S., Iovine G., Lupiano V., Rongo R., Spataro W., 2006, A Computational Method for Modelling and Simulating Lava Flows and Pyroclastic Flows by Cellular Automata.,
CITIES ON VOLCANOES 4, Quito, Ecuador, 2006,
DAmbrosio D., Avolio M.V., Crisci G.M., Di Gregorio S., Iovine G., Lupiano V., Niceforo G., Rongo R.., 2006, Lava-flows hazard zonation through a statistical approach.,
3rd EGU, General Assembly, Vienna, Austria, 2006,
Avolio M.V. (1), Crisci G.M. (2), Di Gregorio S. (1), Iovine G. (3), Lupiano V. (3), Rongo R. (2), 2006, Modelling lava flows characterised by distinct temperatures_ a first attempt through the “double layer” approximation,
Geophysical research abstracts (Online) 8 (2006).,
Iovine G. (1), DAmbrosio D. (2), Merenda L. (1), Lupiano V. (1), Spataro W. (2), 2006, An improved CA model for simulating flow-type landslides,
Geophysical research abstracts (Online) 8 (2006).,
Iovine G., Avolio M.V., Crisci G.M., Di Gregorio S., Rongo R., 2006, The double layer approximation for modelling lava flows with distinct temperatures.,
3rd AOGS, Annual Meeting, Singapore, 2006,
Iovine G., DAmbrosio D., Merenda L., Lupiano V., Spataro W., 2006, SCIDDICA S4d_ an improved CA-model for simulating flow-type landslides.,
3rd AOGS, Annual Meeting, Singapore, 2006,
Crisci G.M., Rongo R., Lupiano V., Niceforo G., Iovine G., 2006, A Methodological Example of Lava-Flow Hazard Zonation in the SE Sector of the Etna Volcano (Sicily Southern Italy).,
3rd AOGS, Annual Meeting, Singapore, 2006,
DAmbrosio D., Spataro W., Iovine G., Avolio M.V., G.M. Crisci, Di Gregorio S., Rongo R., Trunfio G.A., Lupiano V., 2006, Macroscopic Cellular Automata Approach For Modelling Superficial Dangerous Geological Processes.,
Wolfram Science Conference NKS, Washington, 2006,
Tansi C. (1), Muto F. (2), Critelli S. (2), Iovine G. (1), 2006, Timing and style of strile-slip tectonics in central Calabrian Arco (southern Italy).,
25° Convegno Nazionale del Gruppo nazionale di Geofisica della Terra Solida., pp. 47–39, Roma (Italy), november 28-30, 2006,
Buttafuoco G., Caloiero T., Coscarelli R., 2006, Variabilità spaziale e persistenza temporale delle precipitazioni media annue in Calabria.,,
XXX Convegno di Idraulica e Costruzioni Idrauliche, Roma, 2006,
Iovine G., Petrucci O., Rizzo V. & Tansi C., 2006, The March 7th 2005 Cavallerizzo (Cerzeto) landslide in Calabria – Southern Italy,
10th IAEG Int. Congress "IAEG 2006", pp. 1–12, Nottingham, United Kingdom, 6-10 September 2006,
Abstract
In the early morning of March 7th 2005, after a period of prolonged rainfall (645 ...
In the early morning of March 7th 2005, after a period of prolonged rainfall (645 mm in 90 days,
about 72% of mean annual precipitation) and snowfall, the hamlet of Cavallerizzo was severely damaged by a
vast complex debris slide-earth flow. In total, thirty buildings were severely damaged or destroyed by the
landslide, and the main road connecting Cavallerizzo with the villages of Cerzeto and Mongrassano was
disrupted. About 310 inhabitants had to be evacuated to nearby villages.
Several superimposed tectonic units, made of metamorphic rocks (Palaeozoic-Mesozoic) overlain by clastic
terrains (Cenozoic-Neozoic), crop out in the vicinity of the study area. The main scarp of the slide developed at
the eastern tectonic boundary of the Coastal Chain, marked by the "San Fili-Cerzeto-San Marco Argentano"
recent (presumably active) N-S trending normal fault; its crown is mainly located within the cataclastic zone
associated with such master fault. In the lower part of the landslide, two main earth-flows extended eastward
along minor valleys, that merged down slope along the S. Nicola torrent.
The sector affected by the landslide belongs to a wider large-scale slope movement, which extends
westwards up to about 800 m a.s.l. The 2005 event is only the last paroxysmal episode of a long history of
deformation recorded in the area of Cavallerizzo since the XVIII century. The area has been kept under control
by the CNR-IRPI, by means of desultory field measurements (essentially, deep and superficial displacements,
and piezometric levels) since 1999. Velocities, recorded at superficial benchmarks along opening cracks,
pointed out "anomalous" conditions in the weeks preceding the collapse_ pre-rupture velocities ranged from 0.8
to 5-6 cm/day. Despite its emergency character, the monitoring carried out helped to support civil-protection
activities, and allowed all inhabitants to be saved.
Gabriele S., Chiaravalloti F., Brocca L., Melone F., 2006, Stima di precipitazioni convettive mediante dati satellitari_ evento alluvionale del 15,
XXX Congresso di Idraulica e Costruzioni Idrauliche, Roma, 2006,
Sorriso-Valvo M. & Terranova O., 2006, The Calabrian fiumara,
143 (2006): 105–121.,
Gabriele S., Chiaravalloti F., Cotecchia V., 2006, Levento pluviometrico del 22 ottobre 2005 in Puglia. Una ricostruzione sperimentale mediante Meteosat-8 e modello afflussi deflussi a parametri distribuiti.,,
4 (2006): 37–48.,
Petrucci O. & Pasqua A.A., 2006, L’inventario delle opere di sistemazione e bonifica fluviale effettuate nel 900 nella provincia di Cosenza.,
Quaderni di Idronomia montana 26 (2006): 205–215.,
Abstract
Si presentano i primi risultati di una ricerca storica attualmente in corso
nell'ambito di un accordo ...
Si presentano i primi risultati di una ricerca storica attualmente in corso
nell'ambito di un accordo di collaborazione fra il CNR-IRPI, l'ODA
(Osservatorio di Documentazione Ambientale dell'UNICAL) e il Genio Civile
di Cosenza. In virtù di tale accordo il CNR-IRPI ha acquisito il settore dell'archivio
storico del Genio Civile di Cosenza riguardante le opere di sistemazione e
bonifica fluviale realizzate da quest'ultimo Ente, nel periodo 1899-1984, nella
provincia cosentina (6464 kmq, 155 comuni). La nota propone la metodologia di
archiviazione dei dati a scala di bacino mediante tecnologie di tipo GIS e presenta
alcune semplici elaborazioni a scala provinciale dei dati raccolti.
IOVINE G., SHERIDAN M.F. & DI GREGORIO S., 2006, Guest Editorial,
Computers & geosciences 32 (2006): 859–860.,
IOVINE G. (1), DI GREGORIO S. (2), SHERIDAN M.F. (3), 2006, Preface,
Computational geosciences (Amst.) 10 (2006): 159–160. doi_10.1007/s10596-005-9016-0,
DOI: 10.1007%2Fs10596-005-9016-0
R. Gaudio, S. G. De Bartolo, L. Primavera, S. Gabriele and M. Veltri, 2006, Lithologic control on the multifractal spectrum of river networks.,
Journal of hydrology (Amst.) 327 (2006): 365–375. doi_10.1016/j.jhydrol.2005.11.025,
DOI: 10.1016%2Fj.jhydrol.2005.11.025
Abstract
Previous observations on some natural river networks showed the similar values of
the support fractal dimension ...
Previous observations on some natural river networks showed the similar values of
the support fractal dimension and the information entropy in basins having similar source rocks.
In the present work, lithologic control on river network multifractality is investigated through
the reconstruction of the spectra belonging to two classes of different lithology_ the plutonicmetamorphic
class and the coherent sedimentary one. Two computational methods of the
generalised fractal dimensions and multifractal spectra are illustrated and applied to river
networks of the Calabria region (Southern Italy). It is shown that an increment of both the fractal
dimensions and the Lipschitz-Ho¨lder exponents of singularity occurs when passing from a
coherent sedimentary to a plutonic-metamorphic river network. The importance of this finding
emerges from the direct link between flood hydrographs and multifractal spectra, as expressed
in the Multifractal Instantaneous Unit Hydrograph (MIUH): the increment of the multifractal
parameters produces an increment of the flood peaks.
D'Ambrosio D. (1); Spataro W. (1); Iovine G. (2), 2006, Parallel genetic algorithms for optimising cellular automata models of natural complex phenomena_ an application to debris-flows.,
Computers & geosciences 32 (2006): 861–875. doi_10.1016/j.cageo.2005.10.027,
DOI: 10.1016%2Fj.cageo.2005.10.027
Abstract
Cellular automata models of natural complex phenomena may depend on a set of parameters which ...
Cellular automata models of natural complex phenomena may depend on a set of parameters which can significantly
influence the global dynamics of the simulated events. In order to reliably apply such models for predictive purposes, their
parameters have to be estimated with the greatest possible accuracy. However, no standardised optimisation techniques
exist in this specific research field. Genetic Algorithms (GAs) offer a possible solution_ they are parallel algorithms, and can
be easily implemented to exploit the simultaneous use of multiple CPUs, thereby greatly reducing the execution time.
An application of a parallel GA to the optimisation of a cellular automata model for the simulation of debris flows
characterised by strong inertial effects is presented. The May 1998, Curti-Sarno (Italy) debris flow has been selected as a
case study for the optimisation of the model. Theoretical considerations on the dynamics of the adopted GA are discussed,
with reference to two different fitness functions applied to an idealised case study.
Results demonstrated the usefulness of the approach, in terms of both computing time and quality of performed
simulations. Moreover, experiments on the idealised case study pointed out that the simplest fitness function (only based
on the comparison of affected areas) could conveniently be adopted for calibration purposes.
Caballero L., Macias J.L., Garcia-Palomo A., Saucedeo G.R., Borselli L. , Sarocchi D., Sanchez J.M., 2006, The september 8-9, 1998 rain triggered flood events at Motozintla, Chiapas, Mexico.,
Natural hazards (Dordr.) 39(1) (2006): 103–126.,
PETRUCCI O., 2005, Ricerca storica e difesa del suolo in Calabria,
Progettando il passato_ memoria storica e difesa del suolo in Calabria - CNR-IRPI, UOS di Cosenza e Archivio di Stato di Cosenza, Cosenza, 4 LUGLIO 2005,
Pasqua A.A. e Petrucci O., 2005, Fenomeni di dissesto innescati in Calabria dalle piogge del novembre 2004,
2005,
Versace, P., Sirangelo, B., Iiritano, G., Biondi, D., Petrucci, O., De Luca, D.L., Cruscomagno, F., Maletta, D., Gigliotti, A., Zaffino, T., 2005, Aspetti metodologici nella revisione delle soglie pluviometriche di primo livello,
2005,
SORRISO-VALVO M, GULLA' G., ANTRONICO L. (curatori), M. Cilento, O. Petrucci, C. Tansi, L. Aceto, L. Militi, 2005, Relazione finale. “Indagini, studio e monitoraggio del dissesto in atto nel centro abitato di Cirò Marina”,
2005,
Abstract
Indagini, studio e monitoraggio del dissesto in atto nel centro abitato di Cirò Marina ...
Indagini, studio e monitoraggio del dissesto in atto nel centro abitato di Cirò Marina
AVOLIO M.V. (1), CRISCI G.M. (2), D'AMBROSIO D. (1), DI GREGORIO S. (1), IOVINE G. (3), LUPIANO V. (3), RONGO R. (2), SPATARO W. (1), 2005, Cellular Modelling of Surface Flows_ Cellular Automata for Simulating Complex Phenomena_ Lava Flows, Pyroclastic Flows, Debris Flows,
14th ECTQG'05, "European Colloquium on Theoretical and Quantitative Geography", pp. 10–12, Tomar, Portugal, September 9-13, 2005,
Sorriso-Valvo M. (1), Gabriele S. (1), Gullà G. (1), Antronico L. (1), Tansi C. (1), Aceto L. (1), Greco R. (1), Fantucci R. (2), 2005, Studio geologico-geomorfologico-geotecnico e monitoraggio della frana di Serra di Buda (Acri),
pp.1–114, 2005,
Rizzo V., Calendino A., Caruso P., Curcio G., Casalinovo R., Ferraro M., Micieli M., Petrucci O., Soleri S., Caloiero T., 2005, Indagini Storiche, Indagini geognostiche e Relazione sulla pericolosità nel Centro Abitato di Cavallerizzo,
2005,
Rizzo V., Iovine G., Tansi C., Petrucci O., 2005, Esecuzione di un programma di studio e di indagini finalizzati alla verifica dell’idoneità geologico-tecnica e sismica delle aree comunali individuate per la possibile delocalizzazione dell’abitato della frazione “Cavallerizzo” del comune di Cerzeto (CS).,
2005,
Tansi C., 2005, Caratteri geologico-strutturali dell’area compresa tra Montalto Uffugo e Mongrassano (CS), Calabria, Italia – Progetto RISCMASS, Interreg III B, Mediterraneo Occidentale, Asse 4, misura 4.3,
pp.1–34, 2005,
Tansi C., 2005, Caratterizzazione dei possibili nuovi siti di insediamento dell’abitato di Cavallerizzo di Cerzeto_ caratteri geologico-strutturali dell’area di Cavallerizzo-Cerzeto (Cosenza),
2005,
Gullà G., Cilento M., Aceto L., Militi L., 2005, Aspetti geotecnici connessi al fenomeno di dissesto idrogeologico manifestatosi a Cirò Marina nellestate del 2004_ indicazioni ed indirizzi preliminari per la gestione in emergenza e per la gestione ordinaria.,
2005,
Coscarelli R., Gaudio R, Caloiero T., 2005, Valutazione di trend climatici. Applicazioni al bacino del F. Crati (Calabria).,
2005,
Abstract
Negli ultimi anni, numerosi studi sugli andamenti temporali di alcune variabili climatiche (temperatura, composizione chimica ...
Negli ultimi anni, numerosi studi sugli andamenti temporali di alcune variabili climatiche (temperatura, composizione chimica dell'atmosfera, precipitazione, livello medio del mare etc.) hanno messo in risalto l'esistenza di sensibili variazioni globali del clima terrestre. In questa memoria si presentano alcune analisi di dati idrologici misurati in stazioni pluviometriche e termometriche ricadenti nel bacino del Fiume Crati (Calabria). Le elaborazioni hanno riguardato il trend delle precipitazioni e delle temperature, nonché l'evoluzione temporale dei principali indici di aridità. I risultati evidenziano in maniera chiara un trend
negativo per le altezze di pioggia annua e per il numero di giorni piovosi. Per le temperature, invece, l'insufficiente numero di dati non permette di individuare andamenti temporali ben definiti, anche se si rileva su alcune stazioni un'estremizzazione dei valori, ossia un trend positivo della temperatura massima e un trend negativo della temperatura minima.
Gli indici di aridità, infine, rivelano condizioni tendenti all'aridità, pur essendo attualmente 'umide'.
Terranova O. ed altri, 2005, Carta del rischio di erosione attuale e potenziale della regione Calabria,
2005,
Petrucci O., 2005, Relazione sintetica relativa al sopralluogo effettuato il 26.04.2005 a S. Severina (KR), su richiesta del Dipartimento della Protezione Civile Nazionale,
2005,
DI GREGORIO S., IOVINE G., MERENDA L., 2005, – Relazione Sintetica sullAttività di Ricerca svolta dalle Unità Operative presso il Cnr-Irpi Sezione di Cosenza ed il Dipartimento di Matematica dellUniversità della Calabria, concernente la Modellizzazione e la Simulazione di Colate di Detrito, nel Qu,
2005,
IOVINE G., 2005, Indagini geomorfologiche per la caratterizzazione della franosità e delle tendenze morfoevolutive dei siti A e B, indicati dalla Protezione Civile Nazionale e dalla Regione Calabria per leventuale delocalizzazione della frazione Cavallerizzo di Cerze,
2005,
IOVINE G., 2005, Application case of Cellular Automata for debris flows_ protocols. Workshop On High Performance And Grid Computing. Alarico Campus @ University of Calabria, Rende (CS),,
2005,
Gullà G., Iaquinta P., Borrelli L., Terranova O., 2005, Criteri di progettazione della banca dati ingegneristica connessa alle problematiche di dissesto idrogeologico.,
2005,
