C. Tansi & G. Iovine, 2002, Geomorphic and subsurface evidence of active tectonics in the Sant’Eufemia plain (Central Calabria, Southern Italy): the Zinnavo fault,
Geophysical research abstracts (Online) 4 (2002).,
DI GREGORIO S. (1), IOVINE G. (2), LUPIANO V. (2), MERENDA L. (2), RONGO R. (3) & SPATARO W. (1), 2002, Simulating mudflows through cellular automata_ a first attempt for the May, 5th 1998 event of Sarno (Southern Italy),
X-IDNDR "International Symposium - 10 years of the IDNDR", pp. 113–123, Perugia, 16-20 luglio 2000,
D'AMBROSIO D.(1), DI GREGORIO S. (1), IOVINE G. (2), LUPIANO V. (2), RONGO R. (3), SPATARO W. (1), 2002, Modelling surface flows for macroscopic phenomena by cellular automata_ an application to debris flows.,
Lecture notes in computer science 2493 (2002): 304–314.,
Abstract
Cellular automata are good candidates for modelling and simulating
complex dynamical systems, whose evolution depends on ...
Cellular automata are good candidates for modelling and simulating
complex dynamical systems, whose evolution depends on the local interactions
of their constituent parts. Many macroscopic phenomena have such features,
but their complexity involves sometime the interaction of heterogeneous
processes, whose composition is not immediate in a cellular automaton frame.
Furthermore the managing of flows could be not trivial, because cellular
automata and derived models as lattice-gas methods cannot always be applied
successfully to macroscopic cases. We propose some empirical and practical
rules for modelling some macroscopic phenomena with surface flows. An
application to complex debris flows is exhibited together with the results of
simulations of a real case.
IOVINE G. (1), DI GREGORIO S. (2), D'AMBROSIO D. (2) & LUPIANO V. (1), 2002, Debris Flows and Cellular Automata_ an example of simulation from the 1998 disaster of Sarno (Italy).,
Geomorphology: from expert opinion to modelling, pp. 55–64, Strasbourg, 26-27 aprile 2002,
Iovine G. (1), Tansi C. (1), 2002, Active Tectonics and Ground Failure Hazards In The Crati Graben (northern Calabria, Southern Italy): The Bisignano-Rogliano Fault System,
EGS XXVII General Assembly, pp. abstract #4220, Nice (France), 21-26 April 2002,
Abstract
In the study area, located on eastern boundary of the Crati valley (Northern Calabria), a ...
In the study area, located on eastern boundary of the Crati valley (Northern Calabria), a regional normal fault system, oriented N-S, developed from the area of Bisignano to Rogliano (Cosenza province). Thanks to the activity of this tectonic structure, the horst of the Sila Massif, on the east, mainly constituted by igneous-metamorphic rocks belonging to the Palaeozoic "chain", was upthrown with respect to the graben of the R. Crati, on the west, filled by clastic Plio-Quaternary sediments. The above mentioned tectonic structure is made of a complex of synthetic normal step faults, downthrow- ing toward W, generally oriented between N and NNE. Moreover, an antithetic fault, oriented NNW and developed between the village of Paterno Calabro and Cosenza, can be referred to the same tectonic structure. On the whole, the Bisignano-Rogliano tectonic structure extends for about 50 km, with a mean width of ca. 10 km. In the same area, several villages are to be found (besides the above mentioned_ Mangone, Aprigliano, Spezzano della Sila, S. Pietro in Guarano and Rose) and notable roads, such as the Highway "A3", the State Roads SS.270 and SS.107. Historic investigations pointed out that, in the same area, numerous catastrophic earthquakes originated, char- acterised by MCS intensities greater than X, which had a significant role in hamper- ing the socio-economic development of the area. Furthermore, several seismic shocks (Magnitude 4-5) have recently been recorded, with epicentres located in the same area of study_ these latter events allowed a detailed characterisation of the instrumental seismic activity. The recentmost of them, felt by the population within a large ter- ritory, have been recorded between October and December 2001_ in particular, these epicentres have been localised along a segment (oriented NNE) of the considered fault system, in the area between Rogliano and Spezzano della Sila. Morpho-neotectonics and structural investigations have been performed in the study area, by means of field surveying and interpretation of air-photographs. The obtained morpho-structural map, together with the above mentioned seismologic data, constitute an indispensable tool for seismic hazard evaluations in the Bisignano-Rogliano fault
Tansi C. (1), Iovine G. (1), 2002, Tettonica attiva e fagliazione di superficie lungo il sistema di faglie distensive al bordo orientale del graben del Crati (Calabria settentrionale),
81ma Riunione Estiva della Società Geologica Italiana, Torino, 10-12 Settembre 2002,
Tansi C. (1), Iovine G. (1), 2002, Strutture cuneiformi da accomodamento tettono-gravitativo: IL caso di studio di Acri (Calabria settentrionale),
81ma Riunione Estiva della Società Geologica Italiana, Torino, 10-12 Settembre 2002,
Tansi C. (1), Iovine G. (1), Riga G. (2), 2002, Evidenze geomorfologiche e di sottosuolo di tettonica attiva nella Piana di Lametia (Calabria Centrale): la Zinnavo Fault,
81ma Riunione Estiva della Società Geologica Italiana, Torino, 10-12 Settembre 2002,
SORRISO-VALVO M, COSCARELLI R, MINERVINO I, 2002, Il fenomeno della desertificazione. Stato dell’arte,
2002,
Petrucci O., Polemio M., 2002, Hydrogeological multiple hazard_ a characterisation based on the use of historical data,
Landslides, edited by J. Rybar, J. Stemberk and P. Wagner, pp. 269–274. Rotterdam_ Balkema, 2002,
Gullà G., Antronico L., Terranova O., Aceto L., Niceforo D., Cilento M., Perna E., 2002, Scenari di collasso per la frana di Serra di Buda (Acri-CS),
Conservazione dell'ambiente e rischio idrogeologico, pp. 194–203, Assisi, 11-12 dicembre 2002,
Tortorici G. (1), Bianca M. (1), Monaco M. (1), Tortorici L. (1), Tansi C. (2), De Guidi G. (1), Catalano S. (1), 2002, Quaternary normal faulting and marine terracing in the area of Capo Vaticano and S. Eufemia Plain (Southern Calabria, Italy),
Studi Geologici Camerti. Nuova Serie 2 (2002): 1–16.,
D?AMBROSIO D. (1), DI GREGORIO S. (1), IOVINE G. (2), LUPIANO V. (2), MERENDA L. (2), RONGO R. (3), SPATARO W. (2), 2002, Simulating the Curti-Sarno debris flow through cellular automata_ the model SCIDDICA (release S2),
Physics and chemistry of the earth (2002) 27 (2002): 1577–1585. doi_10.1016/S1474-7065(02)00179-1,
DOI: 10.1016%2FS1474-7065(02)00179-1
Abstract
Cellular automata (CA) are based on a regular division of the space in cells. Each ...
Cellular automata (CA) are based on a regular division of the space in cells. Each cell embeds an identical finite automaton, whose input is given by the states of neighbouring cells. The transition function of the CA is made of a set of rules, simultaneously applied, step by step, to each cell of the cellular space. Rules are derived by subdividing, in computational terms, the physical phenomenon into a set of independent, elementary processes. By properly combining each elementary result, the behaviour of the
phenomenon can be simulated.
Debris flows are dense mixtures of sediment and water, which surge down the slopes and along the drainage system, characterised by severe destructive potential. They can be described in terms of local interactions among their elementary portions, and can thus be efficiently modelled through CA. Debris-flows rheologic equations cannot be easily solved without making substantial simplifications. By applying CA, a phenomenological description - able to overcome resource computational limits - can be obtained.
On May 1998, hundreds of soil slip-debris flows were triggered by exceptional rains in Campania (Italy), mostly on the slopes of Pizzo dAlvano. Aiming at modelling purposes, the Curti debris flow was selected as a case study, among the whole population of landslides triggered by the event.
The general frame of SCIDDICA_S2 is inherited from previous releases, recently applied for the simulation of the 1992 Tessina (Italy) earth flow and of the 1984 Mt. Ontake (Japan) debris avalanche. Since its S1 release, the model satisfactorily simulated the Curti-Sarno debris flow. Latest improvements to the transition function led to the S2 release, and to better simulations (presented here). SCIDDICA exhibits a notable flexibility in modelling and simulating flow-like landslides. It could be usefully applied in
hazard mapping (also through a statistical approach), and in evaluating the effects of either human works or accidents along the path of the flow.
ANTRONICO L., GULLA' G., SORRISO-VALVO M., TANSI C., TERRANOVA O., 2001, Effetti dell’incendio del 10 e 11 Agosto 1999 nella campagna cefaludese sulla morfodinamica delle aree colpite e programma di studi per la progettazione degli interventi.,
2001,
ANTRONICO L., GULLA' G., TERRANOVA O., 2001, Condizioni di dissesto sui versanti e processi in alveo conseguenti alle piogge dell’8-10 Settembre 2000 nel settore compreso tra la F.ra Allaro e la F.ra Torbido (Basso Ionio della Calabria),
2001,
ANTRONICO L., GULLA' G., TERRANOVA O., 2001, Condizioni di dissesto sui versanti e processi in alveo conseguenti alle piogge dell’8-10 Settembre 2000 nel bacino del T. Beltrame e nelle aree circostanti (Basso Ionio della Calabria),
2001,
GULLA' G., ACETO L., GRECO R., NICEFORO D., DODARO F., 2001, Definizione preliminare del Modello Geotecnico della Frana di Serra di Buda (Acri – Calabria),
2001,
Lorenzo M. (1), Schiattarella M. (1), Sdao F. (1), Tansi C. (2), 2001, Inquadramento geologico e condizioni di stabilità dei versanti dell’area interessata dal sisma del 9 settembre 1998,
Dissesti prodotti o aggravati dal sisma del 9 settembre 1998 nei territori del Confine calabro-lucano, edited by Gullà G., Sdao F., pp. 9–35. Soveria Mannelli_ Rubbettino, 2001,
Petrucci O., Taddei A. e Minervino I., 2001, WP6000: Selection of Case studies in the Cosenza province,
2001,
Sorriso-Valvo M., Petrucci O., Capparelli G., Silvestri F., Varra' V., Versace P., 2001, Literature survey on landslide types, activity and models,
2001,
PETRUCCI O., 2001, L’analisi dei dati storici per lo studio delle catastrofi idrogeologiche,
22° Corso di aggiornamento_ Tecniche per la difesa dall'inquinamento. Gruppo Italiano di Idraulica, GUARDIA PIEMONTESE, 20 GIUGNO 2001,
Iovine G., Petrucci O., Ferrari E., 2001, Eventi di dissesto idrogeologico nell’Alto Jonio calabrese (CS),
Emergenze ambientali di carattere geomorfologico e tettonico. Comunità Montana Alto Ionio e Min. LL. PP., Oriolo Calabro, 01/02/2001,
Iovine G., Petrucci O., Ferrari E., 2001, Eventi di dissesto idrogeologico nell’Alto Jonio calabrese,
Emergenze ambientali di carattere geomorfologico e tettonico, pp. 15–31, Oriolo Calabro, 1-2 Febbraio 2001,
Petrucci O., Polemio M., 2001, The use of historical data in the characterisation of hydrogeological multiple hazard,
Geophysical research abstracts 3 (2001): 223–223.,
M. Polemio (1), O. Petrucci (2), 2001, Landslides triggered by rainfall_ a critical analysis of international experiences,
XXVI EGS General Assembly, Nice (Francia), 25-30/3/2001,
Polemio, M., Petrucci, O., 2001, Landslides triggered by rainfall_ a critical analysis of international experiences,
Geophysical research abstracts (Online) 3 (2001): 334.,
Rizzo V., Fragale F., Terranova O., 2001, Widespread landslide and flood events in the Catanzaro isthmus (Calabria, Italy). Relationship with rainfall data.,
Natural Hazards and Hydrological Science Symposium of the XXIV general assembly of the European Geophysica Society, pp. 169–183, The Hague (NL), 19-23 Aprile 1999,
Gullà G., Antronico, L., Sorriso-Valvo M., Borrelli L., Greco R., Niceforo D., Aceto L, Terranova O., Naccarato G., 2001, Progettazione esecutiva per la rete nazionale di monitoraggio frane – Sezione territoriale della Regione Calabria,
2001,
Abstract
Svolto per la Presidenza del Consiglio dei Ministri-DSTN-Servizio Geologico Nazionale, P.O. Assistenza tecnica del Q.C.S. ...
Svolto per la Presidenza del Consiglio dei Ministri-DSTN-Servizio Geologico Nazionale, P.O. Assistenza tecnica del Q.C.S. Obiettivo 1 - 1994-1999 - Misura 2.5 Studio di fattibilità e progettazion.
Antronico L., Gullà G., Oddo B., 2001, Considerazioni preliminari sulla caratterizzazione di soil slip in alcune zone di studio della Stretta di Catanzaro (Calabria),
Bollettino della Società Geologica Italiana (Testo stamp.) 56 (2001): 1–10.,
Abstract
In a study area of Calabria multidisciplinary researches are in progress in order to test ...
In a study area of Calabria multidisciplinary researches are in progress in order to test procedures devoted to define the geo-environmental contexts with homogeneous characteristics with respect to specific types of slope instability.
In the study area, that falls inside a graben structure, sedimentary and metamorphic rocks crop out. Both rocks are affected by widespread slope instability, shallow and deep seated landslides, and erosion processes (from moderate to intense).
The shallow failures in the slopes (from 0.5 to 2 m in depth) assume particular importance in the area. This type of instability, indicated as "soil slips", involves small volumes of soil and can produce serious damage to property and danger to people.
The hazard that this type of instability represents is determined by their kinematic mechanism (slide and immediately subsequent rapid flow) and by their spreading during particularly severe rainstorms.
The high incidence of such type of slope instability, has suggested a research aimed at defining a methodological approach to quickly identify their features. These features are essential for the development of forecasting models and subsequent definition of remedial measures, aimed at preventing or reducing risks.
For this reason, in three sample zones of the study area where soil slips involving sedimentary terrains detailed geo-morphological reliefs and geotechical surveys have been carried out. This survey, analyzed together with the photographic documentation acquired during about ten years of observation, has produced a satisfactory definition of the geometric characteristics of the shallow failures.
The knowledge of the dates of some mobilization occurred in the period considered and the rainfall time series, allowed to assess the characteristics of the triggering rainstorm events.
Moreover, the results of some accurate topographic surveys carried out in order to obtain important information about the geometry of the slopes, are shown.
Finally, the results of geotechnical tests enabled to define the particle size envelopes and the index properties of the soil covers involved in shallow instabilities.
ANTRONICO L, SORRISO-VALVO M., TANSI C., GULLA' G., 2001, Carta litologico-strutturale e dei movimenti in massa della Stretta di Catanzaro (Scala 1_50000),
2001,
GULLA' G., ANTRONICO L, COSTA P., D'AMBROSIO R., 2001, Banche dati nell’ingegneria geotecnica_ l’applicativo Geotec.da.ba,
Convengno "GIS: strumenti avanzati ed applicazioni per la gestione ed il controllo del territorio", Università degli Studi del Sannio, pp. 79–83, Benevento, 14 novembre 2001,
M.V. Avolio (1), G. D. D'Ambrosio (1), S. Di Gregorio (1), R. Rongo (1), W. Spataro (1), G. Iovine (2), V. Lupiano (2), 2001, Simulating different complexity landslides with cellular automata methods,
Geophysical research abstracts (Online) 3 (2001).,
IOVINE G. (1), PETRUCCI O. (1) & FERRARI E. (2), 2001, Eventi di dissesto idrogeologico nell’Alto Jonio calabrese (CS).,
Conv. Naz. "Emergenze ambientali di carattere geomorfologico e tettonico. Le frane, le alluvioni, i terremoti"., pp. 15–31, Oriolo Calabro (CS), 1-2 febbraio, 2001,
D'AMBROSIO D. (1), DI GREGORIO S. (1), IOVINE G. (2), LUPIANO V. (2), RONGO R. (3) & SPATARO W. (1), 2001, Simulation of flow-like landslides through cellular automata.,
"ROCC - International Conference on Coastal Rock Slope Instability_ Geohazard and Risk Analysis", pp. 49–51, Le Havre, 30-31 maggio 2001,
AVOLIO M.V. (1), D'AMBROSIO D. (1), DI GREGORIO S. (1), RONGO R. (2), SPATARO W. (1), IOVINE G. (3), LUPIANO V. (3), MERENDA L. (3) & NARDI G. (4), 2001, Simulating landslides of different complexity with hexagonal cellular automata.,
"IAMG 2001 - International Association for Mathematical Geology", Session M, Cancùn, Mexico, 6-12 settembre 2001,
Abstract
The paradigms of acentrism and parallelism that are embedded in the definition of Cellular
Automata (CA) ...
The paradigms of acentrism and parallelism that are embedded in the definition of Cellular
Automata (CA) can be easily and efficiently applied in the simulation of very complex natural
processes like landslides. This permits a phenomenological description that is able to overcome
resource computational limits, placed in a classical approach and therefore based on the resolution
of differential equation systems.
We present a general frame and the latest developments of a CA based model for the
simulation of debris flow type landslides.
Landslides are here viewed as a dynamical system that is subdivided in parts which
components evolve exclusively on the basis of "local interactions" in a spatial and temporal
discretum, where space is represented by hexagonal cells, which specifications (namely substates)
describe the average physical characteristics of the respective area. Such a method permits to start
from simple landslides, that can be modeled using few substates and simple local interactions; a
more complex landslide can be modeled from the previous model, adding substates and local
interactions.
SCIDDICA can be considered to exhibit great flexibility in modeling and simulating debris
flows. Furthermore it can be applied in some field of intervention such as_ The creation of risk
maps also with a statistical approach; the simulation of the possible effects of intervention on
flows for stream deviation, introducing data which represent alterations of the original conditions
(e.g., the construction of a canal or embankment, occlusion of a mud canal etc.). Examples of
practical applications on real events involved_ the 1992 reactivation of the Tessina landslide in
Italy, the 1984 Ontake volcano debris avalanche in Japan and a first partial application to the
landslides occurred in the Sarno area of Campania Region (Italy) in the May of 1998.
O. Petrucci, 2001, Social and economic impact of slope instability in Italy and in Calabria,
2001,
Lorenzo M. (1), Schiattarella M. (1), Sdao F. (1), Tansi C. (2), 2001, Inquadramento geologico, condizioni di stabilità dei versanti dell’area interessata dal sisma del 9 settembre 1998.,
pp.9–35, 2001,
Tansi C., 2001, I dissesti in località Giardini Nuova del Comune di Castelluccio Superiore (PZ).,
pp.87–93, 2001,
Paolucci R., Petrucci O., Polemio M., 2001, L’evoluzione delle pianure costiere e il dissesto idrogeologico in un’area campione della Calabria,
Conoscenza e salvaguardia delle aree di pianura_ il contributo delle Scienze della Terra, Ferrara, 2001,
Tansi C. (1), 2001, I dissesti in località Giardini Nuova del Comune di Castelluccio Superiore (PZ),
Dissesti prodotti o aggravati dal sisma del 9 settembre 1998 nei territori del Confine calabro-lucano, edited by Gullà G., Sdao F., pp. 87–93. Soveria Mannelli_ Rubbettino, 2001,
Bianca M. (1), Monaco C. (1), Tansi C. (2), Tortorici G. (1), Tortorici L. (1), 2001, Quaternary normal faulting and marine terracing in the area of Capo Vaticano and S. Eufemia Gulf (southern Calabria),
3° Forum Italiano di Scienze della Terra, Chieti, 5-8 Settembre 2001,
Polemio M., Petrucci O., 2001, La ricerca internazionale sulle relazioni tra piogge e frane,
X Congresso Nazionale Geologi_ Il territorio fragile, lo stato del dissesto idrogeologico nel mondo, Previsione, prevenzione, mitigazione, pp. 503–510, Roma, 8 dicembre 2000,
Polemio M.; Petrucci O., 2001, Hydrogeological monitoring and image analysis of a mudslide in Southern Italy,
Physics and chemistry of the earth. Part C_ Solar-terrestrial and planetary science 9 (2001): 689–695. doi_10.1016/S1464-1917(01)00068-X,
DOI: 10.1016%2FS1464-1917(01)00068-X
Abstract
This paper describes a methodological example of a data-integration procedure to improve the knowledge ...
This paper describes a methodological example of a data-integration procedure to improve the knowledge of landslide hazard related to a seismic area in the southern Apennine (Italy). Attention is focused on remote sensing data. The analysis is validated using detailed topographical, geophysical, geotechnical and hydrogeological data as ground truth. The investigated phenomenon, which started at the end of 1993, is an earthflow. The presented methodology recommends the combined use of DEM, multi-temporal panchromatic visible aerial photographs and thermal infrared images. The integration between these data and multidisciplinary monitoring data proved useful. The main hydrogeological pattern, the geological and geomorphological framework and the areas of latent instability can be clearly determined. Insight can be gained through the synoptic slope view in the relative short time needed to cany out the analysis. The proposed approach can be regarded as a useful contribution to the evaluation of landslide hazard, particularly during emergency periods. 0 2001 Elsevier Science Ltd. All rights reserved the 1980 earthquake. Interdisciplinary investigations and monitoring 'were carried out between 1994 and 1996, within an EC funded research project (EC, 1996) and partially continued by Authors. This area has been chosen as a case study owing both to the landslide dimensions, which are large enough to allow remote sensing, and the wealth of available data. The selection of the most suitable kind of data - mainly remotely sensed - and the proposal of the most appropriate processing is aimed at improving landslide knowledge. The availability of field data ensures the validation of the proposed work. The combined analysis of DEM, panchromatic visible aerial photographs and thermal infrared images has been carried out aiming to perform a study approach able to provide a multi-temporal and multi-spectral analysis of slope instability phenomena. This framework has then been merged to data coming from multidisciplinary monitoring of study area in order to both verify the results of image analysis and test the proposed methodology.
D'Ambrosio D. 1, Di Gregorio S. 1, Gabriele S. 2, Gaudio R. 2, 2001, A Cellular Automata Model for Soil Erosion by Water,
26(1) (2001): 33–39.,
Abstract
A Cellular Automata model for soil erosion by water, SCAVATU, was developed. It involves a ...
A Cellular Automata model for soil erosion by water, SCAVATU, was developed. It involves a larger number of states in comparison to the previous models, including altitude, water depth, total head, vegetation density, infiltration, erosion, sediment transport and deposition.
The model was applied to the small catchment of the Fiumara Armaconi, Calabria, Southern Italy. First simulations gave encouraging results, even if field erosion data are needed for validation and future calibration and setting of the CA parameters.
The model is susceptible of improvement and could represent a valid alternative to classical physically based methods, for the description of complexity through simple local rules.
Sorriso-Valvo M. (1), Tansi C. (1), Borrelli L. (2), De Simone M. (2), 2000, A numerical appraisal in the study of the relationships between joint separation and faulting,
XXXI International Geological Congress (IGC), Rio de Janeiro, Brazil, August 10-20 2000,
PETRUCCI O., 2000, Le Banche dati regionali_ l’esperienza di ASICal,
Biennale della Protezione Civile, BASTIA UMBRA, 27 NOVEMBRE 2000,
Abstract
La conoscenza inadeguata delle aree esposte a pericolo di frane ed inondazioni fluviali genera incertezze ...
La conoscenza inadeguata delle aree esposte a pericolo di frane ed inondazioni fluviali genera incertezze nella scelta degli interventi prioritari di sistemazione e difesa del suolo e condiziona gli studi di pianificazione territoriale.
Non è, infatti, possibile stabilire la destinazione d'uso per un territorio per il quale non sia disponibile un quadro di riferimento relativo ai fenomeni di dissesto idrogeologico in atto o potenziali. Una adeguata programmazione territoriale, oltre che sul quadro completo delle risorse territoriali, deve basarsi anche sulla valutazione del rischio idro-geologico al quale il territorio è soggetto.
La valutazione probabilistica del rischio risulta fortemente condizionata dalla difficoltà di identificare la frequenza di accadimento dei fenomeni considerati. Disporre di una informazione sugli eventi del passato, omogeneamente distribuita su un ampio intervallo temporale, che comprenda la descrizione dei fenomeni accaduti e degli eventi pluviometrici che li hanno innescati, consente di formulare ipotesi ragionevoli circa l'entità degli eventi da temere, il loro periodo di ritorno, i fenomeni piovosi che possono determinarli.
Si possono così costruire plausibili scenari di evento sulla base dei quali programmare adeguati interventi di riduzione del rischio o predisporre idonei piani di emergenza.
PETRUCCI O., 2000, La Caratterizzazione delle aree a rischio di piena_ un caso di studio in Calabria,
Giornata di Studio sul Rischio Idrogeologico. AIGA - Associazione Italiana Geologia Applicata, ROMA, 15 DIC 2000,
Sorriso-Valvo M., Antronico L., Ausilio E., Caloiero D., Dente G., Gabriele S., Gaudio R., Gullà G., Iovine G., Merenda L., Nicoletti P.G.. Petrucci O., Tansi C., Terranova O., Zimmaro S., 2000, Evento alluvionale dell’8-10 settembre 2000. Rapporto Speditivo del CNR-IRPI di Rende (CS) e del Dipartimento di Difesa del Suolo dell’Università della Calabria realizzato su incarico del Dipartimento Nazionale di Protezione Civile,
2000,
Petrucci O., Polemio M., 2000, Catastrophic Geomorphological events and the role of rainfall in South-Eastern Calabria (Southern Italy),
1st EGS-Plinius Conference on Mediterranean Storms, pp. 449–459, Maratea, 14-16 ottobre 1999,
Ferrari E., Terranova O., 2000, Analysis of threshold parameters of rainfall triggering landslides. Application on Calabrian study areas (Italy),
Newsletter (Eur. Geophys. Soc., Online) (2000).,
