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,
Responsabile: Polemio M.. Altri autori_ Dragone V., Limoni P. P., Mitolo D., Santaloia F.., 2002, Extended Report on deliverables_ first year of activity – European research project “Crystalisation technologies for prevention of salt water intrusion”,
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
Deline, P. (a), Chiarle, M. (b), Mortara, G. (b), 2002, Il crollo frontale del Ghiacciaio di Frébouge (Massiccio del Monte Bianco, Valle d’Aosta) del 18 settembre 2002,
Geografia fisica e dinamica quaternaria (Testo stamp.) 25 (2002): 101–104.,
Abstract
In September 2002, a part (>0,1 × 106 m3) of the Frébouge Glacier (Val Ferret) ...
In September 2002, a part (>0,1 × 106 m3) of the Frébouge Glacier (Val Ferret) front avalanched onto the apex of the polygenic fan. The 0.1 × 106 m3 deposit was composed of poorly-sorted, subspherical, open- work ice particles and formed a lobate front; the lateral margins are steep metric ridges, along longitudinal shear zones. Some big ice boulders rolled 100-150 m ahead the front. Following Alean's (1985) ice avalanching typology, the Frébouge event is a type IA event_ that is to say, avalanching of a low elevation temperate glacier front on a steep rock bed. Others type IA ice avalanches have probably occured in recent decades, but the rapid fusion of avalanche deposits makes their survey difficult. The ignorance of this process frequency explains its underestimation in alpine hazard analysis.
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,
Polemio, M.
Limoni, P. P.
Mitolo, D.
Santaloia, F., 2002, Characterisation of the Ionian-Lucanian coastal plain aquifer,
Groundwater and human development, pp. 874–883, Mar del Plata, Argentina, 2002,
Abstract
This paper deals with a Southern Italy area, 40 km by 10 km wide, located ...
This paper deals with a Southern Italy area, 40 km by 10 km wide, located where four river valleys anastomose themselves in the coastal plain. The geological and hydrogeological features of the study area and the chemical-physical groundwater characterisation have been inferred from the data analysis of 1130 boreholes. Some aquifers, connected among them, constituted by soils of different geological origin -marine terraces deposits, river valley alluvial deposits and alluvial and coastal deposits - have been considered. The coastal plain aquifer is the most interesting for practical utilisation. Groundwater flow is mainly unconfined in the marine terraces and in the river valleys while it becomes mostly confined in the coastal plain aquifer. An upper clayey layer overlies the sandy coastal aquifer characterised by a mean hydraulic conductivity value equal to 2.3 10-4 m/s. The bottom is a silty-clayey bed which lies under the sea level. Being the direct natural recharge extremely low, the recharge of this coastal aquifer is mainly guaranteed by the discharge from upward aquifers and from the river leakage. The new acquired knowledge permits to delineate scenarios useful for an optimization of the groundwater resources tapping and for
pursuing the safeguard of them. Resumen.
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,
Pagliarulo R., 2002, The glacioeustatic control on the evolution of the Sibari alluvial plain (Southern Italy),
GI 2 S Coast Research Publication, edited by Mastronuzzi G., Sansò P., pp. 57–60, 2002,
M. Polemio, 2002, Le conoscenze e le problematiche idrogeologiche della Piana di Metaponto,
Convegno "La ricerca europea per la riduzione dell'inquinamento salino delle acque sotterranee, il caso della piana di Metaponto", Scanzano Jonico, 27/9/2002,
M. Polemio, 2002, La qualità e i fattori di rischio di degrado delle risorse idriche sotterranee della piana di Metaponto,
Seminario "Caratteristiche idrogeologiche dell'acquifero e rischi di degrado delle risorse idriche sotterranee della piana di metaponto", ALSIA-IRPI Bari, presso la Azienda agricola Sperimentale Pantanello, Metaponto (MT), 13-14/5/2002,
M. Polemio, 2002, I sistemi informativi geografici (GIS) applicati allo studio delle risorse idriche sotterranee_ il caso della Puglia,
. Planetek Italia, Istituto per le Applicazioni del Calcolo-CNR, Bari, 30/4/2002,
M. Polemio, 2002, The preliminary hydrogeological characteristaion of the selected test site,
II Meeting "Crystalisation technologies for prevention of salt water intrusion", Unione Europea, V Programma Quadro (1998-2002), Ghent, Belgio, 19-20/4/2002,
Cardinali M. 1, Carrara A. 2, Guzzetti F. 3, Reichenbach P. 4, 2002, Carta della pericolosità da frana dell?alto bacino del Fiume Tevere. Landslide hazard map for the Upper Tiber River basin.,
2002,
Abstract
La carta mostra la pericolosità da frana nellalto bacino del Fiume Tevere. La pericolosità è ...
La carta mostra la pericolosità da frana nellalto bacino del Fiume Tevere. La pericolosità è espressa dalla probabilità di ricorrenza spaziale delle frane allinterno delle unità territoriali in cui il bacino è stato suddiviso. La probabilità di ricorrenza spaziale delle frane è stata determinata attraverso unanalisi statistica multivariata (analisi discriminante) a partire da informazioni litologiche, strutturali, morfologiche e di uso del suolo. Le frane utilizzate per la produzione del modello statistico sono scorrimenti, colate e scorrimenti-colata, superficiali e profondi. Le informazioni geo-ambientali sono state acquisite attraverso tecniche dindagine foto-geologica, rilevamenti di campagna, ricerche bibliografiche, indagini storiche ed elaborazioni spaziali effettuate con tecnologie GIS. Per realizzare la carta, lalto bacino del Fiume Tevere (4.098 km2) è stato suddiviso in 28.600 unità territoriali idro-morfo-litologiche, ossia in aree delimitate da confini idrologici (impluvi), morfologici (displuvi) o litologici. La suddivisione è stata eseguita utilizzando tecnologie GIS a partire da un modello digitale del terreno e dalla cartografia foto-geologica esistente. I valori di probabilità di ricorrenza spaziale delle frane sono raggruppati in 7 classi, visualizzate con tonalità di colore crescente rispettivamente di verde, per le aree predette stabili, e di rosso per le aree predette instabili.
BUSONI, E., COLICA, A., 2002, Analysis of linears, landforms and geology relationships and anthropic effects in the period 1976-1994, Northern Asso river basin (Siena, Italy).,
2002,
WASOWSKI, J., DEL GAUDIO, V. e D.K. Keefer et al., 2002, Special Issue on Assessment and Mitigation of Collateral Seismic Hazards.,
2002,
Corradini C., Morbidelli R., Saltalippi C., Melone F., 2002, An adaptive model for flood forecasting on medium size basins,
, 2002,
Moramarco T., Melone F., 2002, Flooding investigation by coupling hydraulic and hydrologic modelling_ a case study in the upper Tiber basin,
, 2002,
Barbetta S, Melone F., Moramarco T., Saltalippi C., 2002, On discharge simulation from observed stage hydrographs,
, 2002,
Morbidelli R, Corradini C., Saltalippi C., Melone F., 2002, Role of coupled spatial variability of rainfall and soil hydraulic properties on the hillslope hydrograph,
, 2002,
Cotecchia V. , Trizzino R., 2002, Countrywide overviews of data on earthquake influence on underground facilities_ Irpinia earthquake, Italy,
Effects of earthquakes on the deep repository for spent fuel in Sweden based on case studiesand preliminary model results, 2002,
Moscariello A.1, Marchi L. 2, Maraga F.3, Mortara G. 3, 2002, Alluvial fans in the Italian Alps_ sedimentary facies and processes,
Flood and Megaflood Processes and Deposits_ Recent and Ancient Examples, edited by Martini P.I., Baker V.R., Garzon G., pp. 141–166. Oxford_ Blackwell, 2002,
Abstract
Sediment gravity flows are very common sedimentary processes in the Alpine region and are often ...
Sediment gravity flows are very common sedimentary processes in the Alpine region and are often characterized
by rapid deposition of large amounts of material. Hazard evaluation in such mountainous areas
depends on proper identification of the dominant sedimentary processes, interpreted both from modern and
ancient sedimentary facies and their distribution. Three main groups of alluvial fans, characterized by different
dominant sedimentary processes, have been distinguished on the basis of lithological characteristics of
the catchment area. The dominant catchment lithologies are_
1 massive and/or crudely stratified carbonate rocks (dolomite and massive limestones);
2 fine-grained sedimentary and metamorphic rocks (schists, calc-schists, mica schists, slate, phyllites and
quartzites);
3 massive crystalline rocks (granites, granodiorites).
Their main characteristics are illustrated by three case studies concerning large debris-flow events that
occurred in the recent past. The comparison of sediment texture and grain-size distribution indicates that
important differences in the sedimentological features of debris flows are generated by the three different
rock types in the catchments. Colluvium lithology strongly controls the grain-size distribution of the debris
available on the catchment that is mobilized, transported and accumulated on the fan during catastrophic
flood events. The proportion of fine-grained particles (clay and fine silt) within the colluvium plays a key role
in controlling the dominant primary sedimentary processes. The study of 23 flood events over the past 30 yr
indicates that the catchments of group 1 and 2 fans produce large amounts of clay and fine silt, which
typically can lead to the generation of cohesive sediment gravity flows. Group 3 fan catchments produce
colluvium free of clay and fine silt that can be mobilized and transported by water flow processes, and which
in extreme flood events usually are associated with non-cohesive sediment gravity flows.
Govi M. 1, Gullà G. 2, Nicoletti P.G. 3., 2002, Val Pola rock avalanche of July 28, 1987, in Valtellina (Central Italian Alps),
. Boulder_ Geological Society Of America, Inc., 2002,
Mortara G. et alii, 2002, Proposta di una metodologia inerente la mappatura e caratterizzazione dei processi di instabilità dei versanti da sperimentarsi sui bacini dell’alto Toce e della Maggia,
Torino: Regione Piemonte, 2002,
Mortara G., 2002, Les dinamiques des systemés phisyques,
Aosta: Musumeci, 2002,
Bois M., Mortara G., 2002, La protection contre les risques géologiques,
Aosta: Musumeci, 2002,
Luino F., Bassi M., Bossuto P., Fassi P., Belloni A., Padovan N., 2002, Individuazione a fini urbanistici delle zone potenzialmente inondabili_ ricerca storica e analisi geomorfologica. Fiume Oglio-Valcamonica,
2002,
D'Alessandro L., Genevois R., Berti M., Tecca P.R., Urbani A., 2002, Geomorphology, stability analyses and stabilisation works on the Montepiano Travertinous cliff (Central Italy),
2002,
Mortara G. et alii, 2002, Definizione di una metodologia per la valutazione della pericolosità dei versanti in relazione a processi inerenti la coltre superficiale, impiegando parametri idrologici, geotecnici e morfologici e da sperimentarsi in alcuni bacini campione,
Torino: Regione Piemonte, 2002,
Gullà G., Niceforo D., 2002, Il rilievo del dissesto idrogeologico ed il relativo piano,
Roma: Presidenza del Consiglio dei Ministri, 2002,
Pasuto A., Soldati M., 2002, A new mapping technique for landslide management_ a case study in the Italian Dolomites,
Engineering Geology for Developing Countries 9th Congress of the International Association for Engineering Geology and the Environment, Durban, South Africa, 2002,
Mantovani F., Pasuto A., Silvano S, 2002, Definition of the elements at risk and mitigation measures of the Cancia debris flow (Dolomites, northeastern Italy),
Engineering Geology for Developing Countries 9th Congress of the International Association for Engineering Geology and the Environment, Durban, South Africa, 2002,
Corsini A., Pasuto A., Soldati M., Zannoni A., 2002, Technical guidelines for the definition of a conceptual and geotechnical model pf the Corvara landslide (Dolomites, Italy),
Geomorphology: from Expert Opinion to Modelling (CERG), Strasbourg, 2002,
Moramarco T., Saltalippi C., Singh V.P., 2002, Estimating the cross-sectional mean velocity in natural channels by the entropy approach,
Water Resources Management in Arid Regions, Kuwait, 2002,
Moramarco T., Melone F., 2002, Accuracy of kinematic wave and diffusion wave for flood process in natural channels,
Flood Estimation, Berne, Switzerland, 2002,
Barbetta S., Melone F., Moramarco T., 2002, Sullaccuratezza dei metodi di stima delle scale di deflusso,
Atti XXVIII Convegno di Idraulica e Costruzioni Idrauliche, Potenza, 2002,
Moramarco T., Saltalippi C., 2002, Stima della velocità media in sezioni di un corso dacqua naturale,
Atti XXVIII Convegno di Idraulica e Costruzioni Idrauliche, Potenza, 2002,
Corradini C., Morbidelli R., Saltalippi C., Melone F., 2002, Un modello adattivo semidistribuito per la previsione delle piene su bacini di medie dimensioni,
Atti XXVIII Convegno di Idraulica e Costruzioni Idrauliche, Potenza, 2002,
Polemio M.; Limoni P.P.; Mitolo D.; Santaloia F., 2002, Characterisation of Ionian-Lucanian coastal aquifer and seawater intrusion hazard,
17th SWIM Meeting, Delft, Olanda, 6-10/5/2002,
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,
Ardizzone F. 1, Cardinali M. 2, Carrara A. 3, Guzzetti F. 4, Reichenbach P. 5, 2002, Impact of mapping errors on the reliability of landslide hazard maps,
2_1-2 (2002): 3–14.,
Cardinali M. 1, Reichenbach P. 2, Guzzetti F. 3, Ardizzone F. 4, Antonini G. 5, Galli M. 6 , Cacciano M. 7, Castellani M. 8, Salvati P. 9, 2002, A geomorphological approach to estimate landslide hazard and risk in urban and rural areas in Umbria, central Italy,
2_1-2 (2002): 57–72.,
Antonini G. 1, Ardizzone F. 2, Cardinali M. 3, Galli M. 4, Guzzetti F. 5, Reichenbach P. 6, 2002, Surface deposits and landslide inventory map of the area affected by the 1997 Umbria-Marche earthquakes,
Bollettino della Società Geologica Italiana (Online) Sp.1 (2002): 843–853.,
Parise M., Wasowski J., 2002, Slope movements triggered by the 1980 Irpinia earthquake,
4 (2002): 77–83.,
Ubertini L., Napolitano F., 2002, Gestione del rischio per la difesa del territorio,
7/9 (2002): 43–47.,
Tropeano D.,Turconi L., 2002, Effetti geomorfologici connessi all’evento alluvionale del 15 luglio 2002 nelle Valli Cuneesi (Piemonte meridionale),
GEAM. Geoingegneria ambientale e mineraria 106 (2002): 13–49.,
Reina A., Parise M., 2002, La successione stratigrafica delle Grotte di Castellana,
4 (2002): 31–41.,
Parise M., Proietto G., Savino G., Tartarelli M., 2002, Ripresa delle attività esplorative alle Grotte di Castellana_ primi risultati e prospettive future,
4 (2002): 179–186.,
