Govi M., Maraga F., Pelissero C_, 2007, Sediment source from river bank erosion,
FIST Geoitalia 2007, Rimini, 2007,
SURIAN N., RINALDI M., PELLEGRINI L., AUDISIO C., MARAGA F., TERUGGI L., TURITTO O. & ZILIANI L., 2007, Channel adjustments in Italian rivers_ evolutionary trend, causes and management implications,
GSA Annual Meeting & Exposition, Topical Session T17 Management and Restoration of Fluvial Systems with Broad Historical Changes and Human Impacts, Denver, 2007,
TURITTO O., AUDISIO C. & GERVASIO A., 2007, The role of severe foods in the adjustment of river channel geometry,
FIST Geoitalia 2007, Rimini, 2007,
Allasia P., Denasi S., Quaglia G., 2007, Misura mediante telecamere di piccoli spostamenti nel monitoraggio di fenomeni di dissesto naturale,
V Congresso, Torino, 2007,
Lollino G., Baldo M., Giordan D., Godone F., 2007, La Cittadella Inca di Machu Picchu_ monitoraggio di potenziali instabilità di versante.,
XI conferenza Nazionale ASITA, Torino, 2007,
Lollino G., Pasculli A., Sciarra N., Baldo M., Giordan D., 2007, An integrated methodology based on LIDAR, GPS and photogrammetric surveys applied to large landslide in San Martino sulla Marrucina (Central Italy).,
1st North American Landslide Conference, Vail, Vail - Colorado - USA, 2007,
Godone F., Godone D., Tamburini A., Mortara G., 2007, La valanga di roccia della Cima Thürwieser (SO): determinazione del volume con tecniche di fotogrammetria digitale,
XI conferenza Nazionale ASITA, Torino, 2007,
Godone F., Godone D., Maraga F., 2007, Ricostruzione topografica di paleo-superfici alluvionali sepolte,
XI conferenza Nazionale ASITA, Torino, 2007,
Godone D., Tamburini A., Godone F., Chiabrando R., 2007, Ghiacciaio del Belvedere misure di spostamento e ablazione nel biennio 2006,
XI conferenza Nazionale ASITA, Torino, 2007,
Godone D., Tamburini A., Godone F., Chiabrando R., 2007, Ghiacciaio del Belvedere misure di spostamento e ablazione (stagione 2006),
Conferenza Nazionale 2007 Cambiamenti Climatici, Roma 13-13 settembre 2007., Roma, 2007,
Maraga F., Godone F., Govi M., 2007, Cambiamenti di forma dalveo nellalta Pianura Padana_ caso limite nel Fiume Stura di Lanzo (Provincia di Torino),
FIST Geoitalia 2007, Rimini, 2007,
Giardino M., Pogliotti P., Mortara G., Orombelli G., 2007, I fenomeni di rotta glaciale nel bacino del Rutor_ documentazione storica e indagine geomorfologia,
Convegno Nazionale AIGEO, Torino, 2007,
TURCONI L., RIGANO L., ASCHERO R., 2007, Ricostruzione degli effetti di piena torrentizia in ambiente Alpino,
XI conferenza Nazionale ASITA, Torino, 2007,
Chiarle M., Giardino M., Giuliano M., Mortara G., 2007, Proposta di itinerari geomorfologici per la conservazione e la valorizzazione del patrimonio geologica all’interno del Vallone glaciale di Verra (Ayas, Valle d’Aosta),
Congresso Nazionale "Geologia e Turismo", Bologna, 2007,
Mortara G., Chiarle M., Cordola M., Federici P., Fisher L., Huggel C., Kaab A., Semino P., Tamburini A., Viazzo G., 2007, Molteplicità dei rischi associati all’attività geodinamica in atto sul versante orientale del Monte Rosa (Val d’Ossola),
Convegno Nazionale AIGEO, Torino, 2007,
Pau R., Chiarle M., Mortara G., Giulietto W., Arattano M., 2007, Crolli in pareti rocciose d’alta quota_ creazione ed implementazione di un GIS-Database per il Monte Bianco,
Convegno Nazionale AIGEO, Torino, 2007,
Chiarle M., Arattano M., Deline P., Giulietto W., Herry G., Mortara G., Pau R., Ravello M., Vagliasindi M., Voyat I., 2007, Recording and analysis high mountain rockfall events in relation to cryosphere changes,
European Geosciences Union, Wien, 2007,
Delle Rose M, 2007, Valutazioni dei rischi di allagamento per incremento degli eventi meteorici estremi in bacini endoreici della Puglia centro-meridionale.,
Cambiamenti climatici e rischi geologici in Puglia, pp. 49–60, Sannicandro di Bari, 2007,
Abstract
La regimazione delle acque superficiali stagnanti o non corrivate da impluvi naturali e la funzione ...
La regimazione delle acque superficiali stagnanti o non corrivate da impluvi naturali e la funzione regolatrice dei deflussi operata da inghiottitoi carsici hanno costituito, per le genti apule, importanti aspetti per l'antropizzazione del paesaggio e per l'organizzazione degli insediamenti. La crescita dei parametri di pericolosità ambientale, vulnerabilità ed esposizione di strutture ed attività antropiche al rischio idrogeologico impone, anche alla luce dei cambianti climatici in atto, una rinnovata attenzione su queste problematiche. Infatti, aumenti dei tassi di erosione sono prevedibili in regioni che, come la Puglia, presentano aree con caratteri di aridità. Maggiori trasporti solidi potrebbero incrementare la tendenza all'ostruzione degli inghiottiti e, quindi, la pericolosità ambientale di allagamento dei bacini endoreici. In questo studio vengono esposte, con particolare riguardo ad aspetti di Protezione Civile, ricerche speleogenetiche e studi dei reticoli idrografici limitrofi o afferenti a_ Grave del Pompiere (Grumo Appula), Inghiottitoio Calderoni (Mesagne), Vora del Parlatano (Nardò), Aviso Neviera (Sogliano) e Vore Spedicaturo (Surano).
LUINO F. & CIRIO G.C., 2007, Rock block slides in the Langhe Hills of Piedmont Region (Northwest Italy),
1st North American Landslide Conference, Vail, Vail - Colorado - USA, 2007,
Maraga F., Pelissero C., 2007, Esperienze di studio sui cambiamenti fluviali in situazioni a confronto,
Convegno Nazionale AIGEO, Torino, 2007,
Maraga F., Di Nunzio F., Godone F., Massobrio R., Rivelli G., 2007, Processi di trasporto dei sedimenti nellalveo di un piccolo bacino sperimentale attrezzato,
Convegno Nazionale AIGEO, Torino, 2007,
IOVINE G. (1), DI GREGORIO S. (2), D'AMBROSIO D. (2), LUPIANO V. (1), MERENDA L. (1) & NARDI G. (3), 2007, Valutazione e cartografazione della suscettibilità da colata detritica mediante un modello ad automi cellulari.,
La mitigazione del rischio da colate di fango a Sarno e negli altri comuni colpiti dagli eventi del maggio 1998., pp. 175–185, Napoli e Sarno, 2-5 maggio 2005,
O.Terranova, L.Antronico, R.Coscarelli, P.Iaquinta, G.Aramini, C.Colloca, A.Corea, R.Paone, 2007, Water soil erosion risk assessment under different conditions in Calabria (Southern Italy),
International Conference : Soil and Hillslope Management using scenario analysis and runoff-erosion models_ a critical evaluation of current techniques, COST 634, pp. 61–64, Firenze, 7th-9th May 2007,
Abstract
The study presents some assessments of water soil erosion in Calabria (Southern Italy) that
contribute to ...
The study presents some assessments of water soil erosion in Calabria (Southern Italy) that
contribute to improving measures to reduce and mitigate the effects of the factors affecting land
degradation processes. In fact, in the Mediterranean area increasing climate variability - more
frequent droughts and floods than in the past - and the ever stronger human influence on the
territory lead to land degradation phenomena and aggravate the conditions of stress on land
resources. In particular, during the last few decennia in some areas of Southern Italy, water soil
erosion has been responsible for desertification processes. Wide areas are, in fact, prone to
desertification and characterised by on the one hand i) semi-arid climate, ii) seasonal droughts
and iii) heavy rainfall events and, in the other, by iv) wildfires that decrease vegetation coverage,
v) agricultural crisis with the consequent neglect of farms and vi) land degradation.
Delle Rose M, 2007, Sedimentological features of the Plio-Quaternary Aquifers of Salento (Puglia),
Memorie descrittive della Carta Geologica d'Italia, Workshop "Development in aquifer sedimnetology and groundwater flow studies in Italy", pp. 137–145, Parma, 2007,
Abstract
Salento, the southern part of the Apulia Carbonate Platform, presents a horst and graben tectonics. ...
Salento, the southern part of the Apulia Carbonate Platform, presents a horst and graben tectonics. The uplifted blocks are made up by Cretaceous rocks, while
Pliocene and Pleistocene deposits occupy mainly the lowered blocks. Due to the predominance of calcareous rocks, landforms are characterized by karst morphology.
About 70% of drinking water demand of the Salento is provided by a Cretaceous carbonatic aquifer which contains a huge mass of fresh water floating over salt water intruded by the Ionian and Adriatic Seas. Several shallow aquifers, used only for irrigation, lie in the Pliocene and Pleistocene units.
The current resource management is based on studies connected with groundwater hydrological regimen indicating an overall drawing possibility of about 190 x 106 m3 year, against a recharge volume of 880 x 106 m3 related to the six "wet months" embracing fall and winter. This model does not consider the role of the Pliocene and
Pleistocene aquifers in draining a large portion of effective infiltration and pouring out resident water into the Cretaceous aquifer.
A critical situation for the Cretaceous aquifer of Salento has to be stated. Increasing withdrawal induced a strong salinization of the water exploited from wells. Furthermore,
several cases of shallow aquifer pollution have been identified. These aquifers are not considered strategic resources and, as a consequence, their management is missing. However, Pliocene and Pleistocene aquifers must be strongly safeguarded especially in presence of karst system, pollutant substances may reach the Cretaceous aquifer within few hours or days. Three study areas are dealt with. In the Torre dell'Orso coastal area, fresh water is a few meters below the surface and it was drawn since the Bronze Age. Differences in permeability in the local Upper Pliocene deposits create a multilayered aquifer system. A considerable volume of groundwater is discharged into the sea instead of supplying the deep aquifer. In the Burgesi area, karst systems and faulted zones drain waters from the Lower-Middle Pleistocene shallow aquifer into the deep ones strongly increasing groundwater vulnerability. In Contrada Triglio a marly unit act as permeability barrier at the base of the local aquifer which sourced the town of Taranto by means of a Roman-Medioeval aqueduct; this unconfined aquifer is particularly sensitive to climatic changes.
Considering the role of shallow aquifers in recharging the deep ones, as well as the possibility of pollutants spreading, a detailed study of their hydrogeological properties is today necessary. This research provides new evidence of the importance of the sedimentological analysis for a better management of the Salento groundwaters.
Wasowski J., Ferretti A., Colesanti C., 2007, Space-borne SAR interferometry for long term monitoring of slope instability hazards,
Proceedings 1st North American Landslide Conference, Vail (Colorado), 2007,
Polemio M. Limoni P.P., 2007, Surveying and flow velocity measurements in a karstic and coastal aquifer (Bari, southern Italy),
XXXVI IAH Congress, Int. Ass. of HydrogeologistS, Lisbona, September 2007,
M. Polemio; V. Dragone; P.P. Limoni, 2007, Drought and discharge effects on groundwater availability of a wide semiarid region_ the case of Apulian region (Southern Italy),
Groundwater and Ecosystems, edited by Ribeiro, L. Chambel, A. Condesso de Melo, M. T., 2007,
Abstract
The Apulian region is characterized by very low availability of surface water resources due to ...
The Apulian region is characterized by very low availability of surface water resources due to the its widespread karstic nature. Considerable groundwater resources are located in large carbonate coastal aquifers. Groundwater for domestic, irrigation and industrial use has been withdrawn in large and increasing quantities over the years, it still allows the
development of local population. Groundwater is affected by two types of degradation risks_ quality and quantity degradation. Starting by the analysis of long hydrological time series, the dramatic decreasing trend of groundwater availability is characterised and the negative effect in terms of groundwater quality is highlighted.
Voudouris K.; Manos B.; Adamidou K.; Patrikaki O.; Trikilidou E.; Goutzios B.; Arabatzis S.; Papadopoulou O.; Polemio M., 2007, Development and utilization of vulnerability maps for the monitoring and management of groundwater resources in the ARCHIMED areas_presentation of an INTERREG III B project,
7th Int. Scientific Conf. SGEM 2007, Bulgaria, 2007,
Abstract
WATER-MAP is a 2-year project funded under the Community Initiative INTERREG III B ARCHIMED and ...
WATER-MAP is a 2-year project funded under the Community Initiative INTERREG III B ARCHIMED and implemented by nine partners from six countries (Greece, Italy, Malta, Cyprus, Turkey, and Palestinian Authority). The project looks at the topic of integrated groundwater resources management. The aim is to provide scientifically reliable information to the local authorities in order to develop optimal spatial development strategies. Within the framework of the project, vulnerability maps are generated in order to determine areas where aquifers are in high risk of pollution and thus, support the spatial development planning process. The method used to produce the vulnerability maps is the DRASTIC; the most widely used method. Regional assessment of groundwater vulnerability is a useful tool for groundwater resources management and protection zoning. In addition, a Decision Support System (DSS) with information on land uses, populations etc will also be developed and implemented so as to facilitate and optimize the decision-making process involving the problems of land use, water management and environmental protection. This paper presents the project's objectives, the general characteristics of the Archimed areas and the DRASTIC model in GIS environment including data required and initially encountered problems. Based on preliminary results, it is concluded that, regional assessment of groundwater vulnerability is a useful tool for groundwater resources management and protection zoning.
Ventura B., Casarano D., Notarnicola C., Posa F., 2007, Double-layer backscattering model and Bayesian inversion for retrieval of Titan’s surface parameters from CASSINI radar data,
Proceedings of 5th International Symposium on Retrieval of Bio and Geophysical Parameters from SAR Data for Land Applications, ESA conference, Bari, 2007,
Casarano D.,Ventura B., Notarnicola C., Posa F., 2007, CASSINI Radar_ Observations of Titan’s surface features,
Proceedings of 5th International Symposium on Retrieval of Bio and Geophysical Parameters from SAR Data for Land Applications, ESA conference, Bari, 2007,
Ventura B., Casarano D., Notarnicola C., Janssen, M., Posa F, 2007, Inferring Titan’s surface features by means of Bayesian inversion algorithm applied to radar data,
Proceedings of International Symposium on Remote Sensing, Firenze, 2007,
Ventura B., Casarano D., Notarnicola C., Posa F., 2007, Cassini RADAR_ investigation of Titans surface parameters by means of Bayesian inversion technique and gravity-capillary waves modeling of liquid hydrocarbons surfaces,
Proceedings IGARSS07, Barcellona (Spagna),, 2007,
Wasowski J., Casarano D., Lamanna C., 2007, Is the current landslide activity in the Daunia region (Italy) controlled by climate or land use change?,
Landslides and climate changes, Ventnor, Isola di Wight (Gran, 2007,
Amorosi A., Elia G., Boldini D., Lollino P., Sasso M., 2007, Sull’analisi della risposta sismica locale mediante codici di calcolo numerico,
Incontro Annuale Ricercatori di Geotecnica, Salerno, 2007,
Cotecchia F., Lollino P., Vitone C., Mitaritonna G., Santaloia F., 2007, Progetto strategico per la valutazione del rischio da frana nell’appennino pugliese dauno_ approccio metodologico e risultati preliminari,
Incontro Annuale Ricercatori di Geotecnica, Salerno, 2007,
Molerio Leon L., Parise M. & Aldana Vilas C., 2007, Principali font di inquinamento degli acquiferi carsici cubani.,
Campania speleologica, Oiveto Citra (SA),, 2007,
Calcaterra D., Parise M., Strumia S. & Mazzella E., 2007, Relations between fire, vegetation and landslides in the heavily populated metropolitan area of Naples, Italy.,
Proceedings 1st North American Landslide Conference, Vail (Colorado),, 2007,
Montenegro V., Campanella G. & Parise M., 2007, Le grotte di Pozzo Cucù (Pu 1200): un nuovo progetto di ricerca finalizzato al monitoraggio e alla salvaguardia del sito carsico.,
Stato e conservazione delle aree carsiche, Martina Franca, 2007,
Coppola D. & Parise M., 2007, La grotta S. Maria di Agnano (Pu 1201) a Ostuni.,
Stato e conservazione delle aree carsiche, Martina Franca, 2007,
Parise M., Rizzi A. & Trocino A., 2007, Esplorazioni nella zona umida di Grave Grubbo (Calabria).,
Stato e conservazione delle aree carsiche, Martina Franca, 2007,
F. Tagliavini, M. Mantovani, A. Pasuto, and S. Silvano, 2007, An integrated approach for landslide hazard and susceptibility assessment_ a case study in the Dolomites, North-eastern Italy.,
first north american landslide conference, Vail, 2007,
Anselmo V., Maraga F., Pelissero C., 2007, Sediment delivery from a small river basin,
XXIV General Assembly International Union Geodesy and Geophysics (IUGG) Earth: our changing planet, Perugia, 2007,
Angeli M.G., Gasparetto P., Pedol L., Pontoni F., & Silvano S., 2007, The Tessina Landslide and the Civil Defence Plan.,
Landslides and Climate Change - Challenges and Solutions, Ventnor, Isle of Wight, UK, 21-24 maggio 2007,
Abstract
Italian law provides that all the municipalities should have a Civil Defence Plan against major ...
Italian law provides that all the municipalities should have a Civil Defence Plan against major risk, and the Mayor is the local authority for Civil Defence. In April 1992 a dangerous mass movement named Tessina landslide caused a high-risk situation for two villages (Funes and Lamosano). On that occasion, adequate measures to safeguard the people exposed to the risk had to be considered, besides the need to monitor and check the movement evolution. The Ministry for Civil Defence assigned funds for the installation of a monitoring and warning systems and during critical events various automatic alarm levels can be determined (i.e. Pre-alarm, Normal Alarm, Serious Alarm). These different alarm levels are directly integrated in a Civil Defence Plan which includes evacuation of the population from the residential areas in case of possible dan-ger, by ensuring collaboration from several other boards and institutions.The Plan identifies the procedures to be activated in order to attain an optimised preparedness in case of re-activation of the landslide. This Plan provides the involvement of the national and local government offices, and volunteers, according to the out-line here reported. Such a plan may face any possible evolution of this phenomenon even in relation to its negative increase caused by current climate changes.
L. Borselli, 2007, Field Trip Guide – (L. Borselli Editor),
Soil and Hillslope Management using scenario analysis and runoff-erosion models_ a critical evaluation of current techniques, firenze, 2007,
Tecca P.R., Armento M.C., Genevois R., Deganutti A.M., 2007, Numerical modelling of two debris flows in the Dolomites (Italian Alps).,
The 4th International Conference on debris-flow hazard mitigation_ Mechanics, prediction, and assessment., Chengdu (China), 2007,
Moscariello A, Deganutti A. M., 2007, Hydrological and sedimentary processes related to a high intensity debris-flow catchment in the Dolomites (Italian Alps),
The 4th International Conference on debris-flow hazard mitigation_ Mechanics, prediction, and assessment., Chengdu (China), 2007,
Davies, T.R, McSaveney, M.J., Deganutti, A.M., 2007, Dynamic fragmentation causes low rock-on-rock friction,
1st Canada-U.S. Rock Mechanics Symposium, Vancouver, 2007,
Magri, O., Mantovani, M., Pasuto, A., Soldati, M., 2007, Field guide of the north-west coast of Malta – Landslide monitoring and hazard prevention.,
Integration of the geomorphological environment and cultural heritage for tourism promotion and hazard prevention, Valletta, Malta, 2007,
Marcato, G., Borgatti, L., Corsini, A., Pasuto, A., Silvano, S., Zabuski, L.,, 2007, Numerical analysis of the effectiveness of countermeasure works on earth slide stabilization_ a case study in South Tyrol (Italy).,
1st North American Landslide Conference, Vail, Colorado, 2007,
Angeli M.G., Castelli S., Galvani A., Gasparetto P., Marabini F., Mertzanis A., & Pontoni F., 2007, Erosive processes and related hazards in the Coastal Zone.,
'Landslides and Climate Change - Challenges and Solutions', Ventnor, Isle of Wight, UK, 21-24 maggio 2007,
Abstract
The aim of this work, considering the evolution of the Adriatic Coastal area during the ...
The aim of this work, considering the evolution of the Adriatic Coastal area during the last 50 years, is to show how it is possible to face and contrast the erosive phenomena at the beginning of the event. A tardy intervention is, of course, more expensive without possibility to guarantee the final result. The selected area permits to consider different physiographic coastal units_ the Venice lagoon, the Po river delta, the sandy littoral with the padan plain on the back and the cliff from Cattolica to Ancona.
