DOCSLIB.ORG

The Civil Protection Framework

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text
The Civil Protection Framework Presidency of the Council of Ministers – Department of Civil Protection ABRUZZO EARTHQUAKE RESPONSE ANALISY CIVIL PROTECTION AND ITALIAN RED CROSS THE ITALIAN CIVIL PROTECTION EMERGENCY MANAGEMENT SYSTEM Castiglione delle Stiviere, June 23th 2010 Fabrizio Curcio “The Italian Civil Protection : a good answer following decades of mistakes …” 9th October 1963 1968 Belice earthquake 4rd November 1966 HISTORY In November 1980, a strong earthquake struck Southern Italy. About 3,000 people were killed and some 10,000 injured. During the event, national assistance was not coordinated by a central authority. The Italian Department of Civil Protection was established in 1982. Presidency of the Council of Ministers – Department of Civil Protection CIVIL PROTECTION 1919 - 1969 The Ministry of PUBBLIC WORKS is in charge of coordinating all the interventions to face the emergency Ottobre 1963 - Vajont 1968 Belice earthquake 1966 Arno flood 1970 Law n. 996 – regulation about first assistance to the people affected by disasters – Civil Protection The Ministry of Internal Affairs is in charge of coordinating all the interventions to face the emergency Presidency of the Council of Ministers – Department of Civil Protection CIVIL PROTECTION 1976 Friuli earthquake 1980 Irpinia earthquake 1981 D.P.R. n. 66 – regulation regarding the esecution of the Law 996/70 1992 Law n. 225 - Setting up of the Italian Civil Protection Sistem COSTITUTIONAL LAW 3/2001 Presidente di Regione 8 – Valle d’Aosta, Provincia Autonoma Bolzano, Provincia Autonoma Trento, Toscana, Umbria, Lazio, Sicilia, Calabria Assessorato Ambiente 4– Sardegna,Piemonte,Liguria,Abruzzo REGIONAL COMPETENCE Assessorato Difesa del suolo 1 – Emilia Romagna Assessorato Urbanistica, Beni ambientali, culturali, Istruzione, Protezione Civile 1 – Molise Assessorato Infrastrutture, Opere Pubbliche e Mobilità 2 – Basilicata, Friuli Assessorato Protezione Civile, Polizia Locale e Sicurezza 1 – Lombardia Assessorato Identità Veneta, Protezione Civile e Caccia 1 - Veneto Assessorato Lavori Pubblici, Protezione Civile 1 - Campania Assessorato Opere Pubbliche, Protezione Civile, Lavori Pubblici, Difesa del suolo 1 - Puglia Presidency of the Council of Ministers – Department of Civil Protection TYPOLOGY OF EVENTS AND COMPETENCE AREAS L. 225/92 For the purposes of civil protection, events are divided into: a) events which can be solved by applying available resources of single administrations; b) events which can be faced with additional co- ordinated resources of more administrations; c) events which, because of their intensity and size, require the intervention of extraordinary means and authority. Presidency of the Council of Ministers – Department of Civil Protection PRIME MINISTER The civil protection framework HEAD OF THE DEPARTMENT OF CIVIL PROTECTION INSTITUTIONS SUPPORT OPERATIONAL STRUCTURES INTERIOR National Fire-fighters Corp, Police DEFENCE Army, Navy, Air Force, Carabinieri HEALTH Medical Emergency ENVIRONMENT, SEA AND TERRITORY SAFEGUARD Coast Guard TRANSPORT AND INFRASTRUCTURES Road maintenance, Highways and Railways Companies EDUCATION, UNIVERSITY AND RESEARCH National Institute for geophysics and volcanology ECONOMY AND FINANCE National research Council ECONOMIC DEVELOPMENT Finance Police CULTURAL HERITAGE AND ACTIVITIES Electrical power supply companies JUSTICE Penitentiary police AGRICULTURAL POLICY AND FORESTRY State Forest Corp FOREIGN AFFAIRS TERRITORIAL STRUCTURES OF CIVIL PROTECTION Volunteer Organizations Regions Provinces Municipalities NATIONAL OPERATIONAL STRUCTURES National Fire Fighters Corps National Institute of Geoph. and Volc. Army Technical and scientific community Navy Italian Red Cross Air Force National health service structures Carabinieri Volunteer organisations Costal Guard National Alpine Aid Corps Police State Forest Corps Presidency of the Council of Ministers – Department of Civil Protection The mission The Civil Protection National Service aims at safeguarding human life and health, goods, national heritage, human settlements and the environment from all natural or man-made disasters, through a complex system of structures and competences. Forecasting ANALYSIS OF CAUSES AIMED AT IDENTIFYING RISK TYPOLOGIES AND AREAS AFFECTED BY RISKS •REDUCING/MITIGATING DAMAGES Prevention •RAISING POPULATION AWARENESS TO ENHANCE SELF PROTECTION MEASURES OPERATIONS AIMED AT FULFILLING THE BASIC NEEDS Emergency OF THE POPULATION AFFECTED BY THE EVENT BASED relief ON PREVIOUSLY ELABORATED EMERGENCY RELIEF PLANS Emergency INTERVENTIONS AIMED AT RESTORING NORMAL LIFE overcoming CONDITIONS Seismic Zoning of Italy till 2003 2004 HAZARD LEVEL MUNICIPALITIES HAZARD LEVEL MUNICIPALITIES 1a cat. (high) 368 zone 1 (high) 708 2a cat. (medium) 2498 zone 2 (medium) 2345 3a cat. (low) 99 zone 3 (low) 1560 N.C. (aseismic) 5135 zone 4 (very low) 3488 TOTAL 8100 TOTAL 8101 VOLCANIC ACTIVITY Exposed Volcano Last eruption population Stromboli Always active 500-5.000 Etna 2007 2.000-200.000 Vesuvio 1944 600.000 Pantelleria 1891 7.000 Vulcano 1888-1890 700-10.000 Ferdinandea 1831 0 C.Flegrei 1538 300.000 Ischia 1302 45.000 Lipari VI-VII sec. 10.000 Lipari Ferdinandea Etna, 27 October 2002 Stromboli, 30 December 2002 FLOODS AND LANDSLIDES Calabria, Cerzeto, March 2005 6.630 municipalities (= 82% of total) and 29.435 kmq (= 10% of total) exposed at risk Friuli, August 2003 Puglia, October 2005 40 mld euro need to mitigation activity 200 mil euro available in 2007 Presidency of the Council of Ministers – Department of Civil Protection Forest fires risks July 24th 2007 TRANSPORTATION RISK INDUSTRIAL AND ENVIRONMENTAL RISKS RECLAMATION OF WRECK Presidency of the Council of Ministers – Department of Civil Protection Operations rooms and Network of Technologic and Scientific regional structures centres for risk analisys Centri Funzionali EARLY WARNING AND REAL TIME COMMUNICATIONS SISTEMA ITALIA NATIONAL CIVIL PROTECTION OPERATIONS ROOM NATIONAL EMERGENCY PROCEDURES START-UP COMUNICAZIONE DELL’EVENTO E FLUSSO DELLE INFORMAZIONI CF C SALE OPERATIVE SALE REGIONALI OPERATIVE E NAZIONALI PROVINCIAL I SALA SITUAZIONE ITALIA - SISTEMA SALE OPERATIVE NAZIONALI DEI SERVIZI SALE OPERATIVE DELLE COMPONENTI E STRUTTUREPrefetture - UTG OPERATIVE Law no. 225/1992 which, because of its intensity and size, shall require extraordinary means and authorities EVENT meeting of Council of Ministers Declaration of the “ State of Emergency” and assignment of the Head Commissioner Law no. 286/2002 emergency state of major entity to be assessed on the basis of its life threatening potential risk EVENT The President of the Council of Ministers before declaring the state of emergency decides the activation of the civil protection national system The Head of the Civil Protection Department is in charge of coordinating all the interventions to face the emergency Presidency of the Council of Ministers – Department of Civil Protection The system at work – the Operational Committee Army Air Force State Forest Corp Navy Carabinieri Police National Fire-fighters TRANSPORT Corp SERVICES •Road maintenance, Highway and Railway Italian Red Cross Companies Head of Civil Protection •Agency for flight control OTHER COMMUNICATIO SERVICES Alpine Rescue N SERVICES •National Corps National •Italian television postal service Health System •Telecommunicat •Electrical ion companies power supply companies National Research Council Environment Protection Agency Regions and territorial Volunteer structures of Organizatio civil ns protection Presidency of the Council of Ministers – Department of Civil Protection Distribution of Civil Protection’s National Resources over the territory Bolzano • E. I. Venegono Bellun • C.C. • G.d.F. o Varese • G.d.F. Orio al Serio •C.F.S. • VV.F. Casarsa • C.C. Volpiano Vicenza • E.I. • C.C. • A.M. Treviso Linate • C.C. • A.M. Venaria Venezia Malpensa • E.I. Padova • G.d.F. • P.S. • E.I. • P.S. Bologna • VV.F Torino Forlì • P.S. • VV.F. • C.C. Rimini Genova • VV.F. • G.d.F. • A.M. - E.I. Albenga • VV.F. Firenze • G.d.F. • C.C. Luni Sarzana • P.S. Falconara • M.M. - C.P. Pisa Arezzo • C.C. • E.I. Ceci • VV.F. • C.C. na Pescara • G.d.F. Viterbo •C.F.S • G.d.F. - P.S. - VV.F. Grosseto • E.I. Rieti . • C.P. - C.F.S. • A.M. •C.F.S Bracciano . Ciampinio • E.I. Urbe Bari • VV.F. – C.F.S. •C.F.S • C.C. - G.d.F. Frosinone Olbia • A.M. • P.S. - VV.F. • C.C. Pratica di Mare • A.M. - M.M. Grazzanise Brindisi Alghero • C.C. – G.d.F. • A.M. • A.M. • VV.F. • P.S. Napoli Taranto • G.d.F. Pontecagnano • G.d.F. Salto di Quirra • C.C. • P.S. Grottaglie Abbasanta • A.M. • VV.F. • C.C. Decimomannu • M.M. • P.S. • A.M. Lamezia terme • E.I. - G.d.F. Cagliari Palermo • C.F.S. • E.I. Vibo Valentia • C.C. • C.C. • C.C. • G.d.F. • G.d.F. • P.S. Reggio Calabria • P.S. Catania AIR BASES Trapani • M.M. • A.M. • C.C. • G.d.F. • VV.F • C.P. Air Force Carabinieri National Fire-fighters Corp Navy Finance Police Coast Guard Army State Police State Forest Corp Presidency of the Council of Ministers – Department of Civil Protection Regional response units Independent Provinces Trento and Bolzano NATIONAL RESOURCES PresidencyPresidency ofof thethe CouncilCouncil ofof MinistersMinisters –– DepartmentDepartment ofof CivilCivil ProtectionProtection Memorandum of understanding D.P.C. – C.R.I. 29 August 2003 Objective: to enhance the safety and security of the citizens in case of emergency, through the sinergy and the operative efficiency in the use of common resources Costant contact beetween the Centrale Operativa C.R.I. and Sala Situazione Italia - D.P.C. Availability
Load more

Recommended publications
  • First Results of an INGV Project for the Integrated Analysis of the Active Tectonics in SW Sicily M
    GNGTS 2016 SESSIONE 1.1 FIRST RESULTS OF AN INGV PROJECT FOR THE INTEGRATED ANALYSIS OF THE ACTIVE TECTONICS IN SW SICILY M. Mattia1, G. Barreca2, C. Bottari3, V. Bruno1, P. Burrato3, F. Cultrera2, L. Dardanelli4, S. De Gregorio5, L. Ferranti6, L. Guzzetta7, P. Madonia5, C. Monaco2, C. Pipitone4, F. Pepe8 1 Istituto Nazionale di Geofisica e Vulcanologia, Osservatorio Etneo - Sezione di Catania, Italy 2 Dip. di Scienze Biologiche, Geologiche e Ambientali, Sezione di Scienze della Terra, Università di Catania, Italy 3 Istituto Nazionale di Geofisica e Vulcanologia, Roma, Italy 4 Dip. di Ingegneria Civile, Ambientale, Aerospaziale dei Materiali (DICAM), Università di Palermo, Italy 5 Istituto Nazionale di Geofisica e Vulcanologia, Sezione di Palermo, Italy 6 Dip. di Scienze della Terra, dell’Ambiente e delle Risorse (DiSTAR), Università “Federico II”, Napoli, Italy 7 INAF - Istituto di Astrofisica e Planetologia spaziali (IAPS), Rome, Italy 8 Dip. di Scienze della Terra e del Mare (DISTEM), Università di Palermo, Italy We present the first results of a project financed by the “Struttura Terremoti” of INGV to study the potential sources of earthquakes in south-western Sicily, including the area hit by the 1968 Belice earthquake sequence and the archaeological area of Selinunte, affected by two earthquakes in historical times. We adopt in this project a multi-disciplinary approach with the goal of addressing the following points: 1) define the active tectonic framework of south- western Sicily, 2) investigate and characterize on-shore and off-shore faults, potential sources of damaging earthquakes, and 3) evaluate the current deformation rates. To do this, we collected a new set of geodetic (GPS and InSAR) and geochemical data, and performed geological and geomorphological surveys on-land in the area between Mazara, Castelvetrano and Selinunte.
    [Show full text]
  • Copertina Vol. 31 Suppl 1
    doi: 10.3301/ROL.2014.140 ISSN 2035-8008 RENDICONTI Online della Società Geologica Italiana RENDICONTI Online Volume 31, Supplemento n. 1 - Settembre 2014 della Società Geologica Italiana Volume 31, Supplemento n. 1 - Settembre 2014 The Future of the Italian Geosciences - The Italian Geosciences of the Future Vol. 31, Suppl. n. 1 (2014) pp. 1-816. Vol. 87° Congresso della Società Geologica Italiana e 90° Congresso della Società Italiana di Mineralogia e Petrologia Abstract Book Milan, Italy, September 10-12, 2014 main partner edited by: B. Cesare, E. Erba, B. Carmina, L. Fascio, F.M. Petti, A. Zuccari. RENDICONTI ONLINE DELLA SOCIETÀ GEOLOGICA ITALIANA Direttore responsabile: DOMENICO CALCATERRA Iscrizione ROC 18414. ROMA Pubblicato online il 1 Agosto 2014. Rendiconti Online della Società Geologica Italiana - SOCIETÀ GEOLOGICA ITALIANA 2014 www.socgeol.it Rend. Online Soc. Geol. It., Suppl. n. 1 al Vol. 31 (2014) CONGRESSO SGI-SIMP 2014 © Società Geologica Italiana, Roma 2014 Seismotectonics of the active thrust front in southwestern Sicily: hints on the Belice and Selinunte seismogenic sources Ferranti L.*1, Guzzetta L.1, Pepe F.2, Burrato P.3, Barreca G.4, Mattia M.5, Monaco C.4 & V. Bruno5 1. Dipartimento di Scienze della Terra, dell’Ambiente e delle Risorse (DiSTAR), Università di Napoli "Federico II". 2. Dipartimento di Scienze della Terra e del Mare, Università di Palermo. 3. Istituto Nazionale di Geofisica e Vulcanologia, Sezione di Roma. 4. Dipartimento di Scienze Biologiche, Geologiche e Ambientali, Sezione di Scienze della Terra, Università di Catania. 5. Istituto Nazionale di Geofisica e Vulcanologia, Osservatorio Etneo - Sezione di Catania. Corresponding email: [email protected] Keywords: Active thrust system, southwestern Sicily, fault segment parameters, historical earthquakes.
    [Show full text]
  • Towards a Revised Framework for Participatory Planning in the Context of Risk
    sustainability Article Towards a Revised Framework for Participatory Planning in the Context of Risk Paola Rizzi 1,* and Anna Por˛ebska 2 1 Department of Architecture, Design and Urban Planning, University of Sassari, 07100 Sassari, Italy 2 Faculty of Architecture, Cracow University of Technology, 31-155 Kraków, Poland; [email protected] * Correspondence: [email protected] Received: 30 April 2020; Accepted: 7 July 2020; Published: 9 July 2020 Abstract: Community participation is widely acknowledged to be crucial in both mitigation and reconstruction planning, as well as in community-based disaster risk reduction (CBDRR) and community-based disaster mitigation (CBDM) processes. However, despite decades of experience, an efficient framework that is acceptable for all actors and suitable for all different phases of the process—ranging from planning to post-disaster recovery—is lacking. The examples presented in this paper shed light on the different dynamics of participatory design processes and compare situations in which participatory design and community planning were introduced before, during, or after a disastrous or potentially disastrous event. Others emphasize the consequences of participation not being introduced at all. Analysis of these processes allows the authors to speculate on a revised, universal model for participatory planning in vulnerable territories and in the context of risk. By emphasizing intrinsic relations of different elements of the process, particularly the responsibility that different actors are prepared—or forced—to take, this article offers insight towards a framework for post-2020 participatory planning. Keywords: participatory design; design for risk reduction (DRR); disaster mitigation (DM); risk awareness; resilience 1. Introduction 1.1.
    [Show full text]
  • Tectonic Evolution and Current Deformation of the NW Sicily Channel and the Lampedusa Plateau Based on Multi-Resolution Seismic Profiles Analysis
    PhD School in Earth, Environment and Resources Sciences - XXX Cycle - PhD Thesis Tectonic evolution and current deformation of the NW Sicily Channel and the Lampedusa Plateau based on multi-resolution seismic profiles analysis Melania Meccariello Advisor Prof. L. Ferranti PhD Coordinator Prof. M. Fedi Co-advisor Prof. F. Pepe 2017 INDEX ABSTRACT ...................................................................................................... 5 INTRODUCTION .......................................................................................... 12 1. BACKGROUND GEOLOGICAL SETTING ..................................... 18 1.1 The Sicily Channel in the regional geological contest ................... 18 1.2 Structural setting and active deformation of SW Sicily ............... 21 1.3 Regional distribution of lithostratigraphic units ........................... 29 1.4 Structural frame of the Sicily Channel ........................................... 31 1.5 Seismo-tectonic frame of the Sicily Channel .................................. 40 1.6 Volcanism in the Sicily Channel ...................................................... 41 2. FUNDAMENTALS OF SEISMIC REFLECTION ACQUISITION AND INTERPRETATION ............................................................................ 43 2.1 The seismic reflection analysis ........................................................ 43 2.2 Techniques of acquisition of the analysed seismic reflection profiles ........................................................................................................
    [Show full text]
  • Accepted Manuscript
    Accepted Manuscript Geothermal resources within carbonate reservoirs in western Sicily (Italy): A review D. Montanari, A. Minissale, M. Doveri, G. Gola, E. Trumpy, A. Santilano, A. Manzella PII: S0012-8252(16)30462-7 DOI: doi: 10.1016/j.earscirev.2017.04.016 Reference: EARTH 2415 To appear in: Earth-Science Reviews Received date: 21 December 2016 Revised date: 21 March 2017 Accepted date: 29 April 2017 Please cite this article as: D. Montanari, A. Minissale, M. Doveri, G. Gola, E. Trumpy, A. Santilano, A. Manzella , Geothermal resources within carbonate reservoirs in western Sicily (Italy): A review, Earth-Science Reviews (2017), doi: 10.1016/ j.earscirev.2017.04.016 This is a PDF file of an unedited manuscript that has been accepted for publication. As a service to our customers we are providing this early version of the manuscript. The manuscript will undergo copyediting, typesetting, and review of the resulting proof before it is published in its final form. Please note that during the production process errors may be discovered which could affect the content, and all legal disclaimers that apply to the journal pertain. ACCEPTED MANUSCRIPT Geothermal resources within carbonate reservoirs in western Sicily (Italy): a review D. Montanari, A. Minissale, M. Doveri, G. Gola, E. Trumpy, A. Santilano, A. Manzella Institute of Geosciences and Earth Resources, National Research Council of Italy (CNR) Keywords: Geothermal systems; Carbonate reservoirs; Temperature Modeling; Fluid geochemistry; Groundwater flow paths; Sicily; Structural Geology; Italy Abstract Low-to-medium temperature fluid reservoirs hosted in carbonate rocks are some of the most promising and unknown geothermal systems.
    [Show full text]
  • Reconstruction and Conservation in the Post-Truth Era. Historical Lies, Authenticity, Material Evidence
    Reconstruction And Conservation In The Post-Truth Era. Historical Lies, Authenticity, Material Evidence Nino Sulfaro1 Doc: Now remember, according to my theory, you interfered with your parents first meeting. If they don't meet, they won't fall in love, they won't get married and they won't have kids. That's why your older brother's disappearing from that photograph. Your sister will follow, and unless you repair the damage, you'll be next. Marty: Sounds pretty heavy! Back to the future (Robert Zemeckis, 1985) In a famous 1980’s movie, the main character, Marty McFly, catapulted thirty years back into the past by a time machine, accidentally prevents his parents from meeting, causing a chain of events that puts his very existence at risk. As in all happy endings, the risk is overcome, and Marty can go back to the future without having caused any damage to the time line (fig. 1). Figure 1. A frame of the movie Back to the future (Robert Zemeckis, 1985) in which Doc ‘fights’ against the time. Sulfaro, Nino (2018). Reconstruction And Conservation In The Post-Truth Era. Historical Lies, Authenticity, Material Evidence. In: A contemporary provocation: reconstructions as tools of future-making. Selected papers from the ICOMOS University Forum Workshop on Authenticity and Reconstructions, Paris, 13 – 15 March 2017, eds C. Holtorf, L. Kealy, T. Kono. Paris: ICOMOS. 1 The plot was based on the well-known ‘paradox’ of the time traveller, according to which making variations in the past means altering the temporal fabric: after a short period of transition, the fabric achieves a new arrangement in which all that does not conform to it is destined to vanish.
    [Show full text]
  • XI Inqua Congress
    APAT AN INNOVATIVE APPROACH FOR ASSESSING EARTHQUAKE INTENSITIES: THE PROPOSED INQUA SCALE BASED ON SEISMICALLY-INDUCED GROUND EFFECTS IN THE ENVIRONMENT Working Group under the INQUA Subcommission on Paleoseismicity PRESENTED AT THE XVI INQUA CONGRESS RENO, USA JULY 23 – 30, 2003 INQUA Scale XVI INQUA Congress, Reno, July 23 – 30, 2003 AN INNOVATIVE APPROACH FOR ASSESSING EARTHQUAKE INTENSITIES: THE PROPOSED INQUA SCALE BASED ON SEISMICALLY-INDUCED GROUND EFFECTS IN THE ENVIRONMENT Working Group under the INQUA Subcommission on Paleoseismicity Michetti A. M.1, E. Esposito2, J. Mohammadioun3, B. Mohammadioun3, A. Gürpinar4, S. Porfido2, E. Rogozhin5, L. Serva6, R. Tatevossian5, E. Vittori6, F. Audemard7, V. Comerci6, S. Marco8, J. McCalpin9, and N.A. Morner10. 1Università dell’Insubria, Como, Italy; [email protected]; 2CNR-IAMC, Napoli, Italy; 3Robinswood Consultant, Saint Martin de Nigelles, France; 4IAEA, Vienna, Austria; 5Russian Academy of Sciences, Moscow, Russia; 6APAT, Roma, Italy; 7FUNVISIS, Caracas, Venezuela; 8University of Tel Aviv, Israel; 9GEO-HAZ Consulting, Crestone, CO, USA; 10University of Stockholm, Sweden. INDEX Introduction 2 Intensity — Why today? 4 The shortcomings of earlier scales — Why Intensity should be evaluated using ground effects 6 General statements 9 The INQUA scale 13 Definitions of intensity degrees 14 Intensity - fault parameter relationships: discussion and conclusions 21 References 22 Appendix 1: References for earthquakes listed in Table 2 and 3 41 Appendix 2: distribution of ground
    [Show full text]
  • Seismogenic Evidence of Ongoing Compression in Eastern-Central Italy and Mainland Sicily: a Comparison
    06 133-20 06(209-222) 25-06-2007 14:24 Pagina 209 Queste bozze, corrette e accompagnate dall’al- legato preventivo firmato e dal buono d’ordine, SGI Bollettino 20/06-133 debbono essere restituite immediatamente alla Segreteria della Società Geologica Italiana c/o Dipartimento di Scienze della Terra Piazzale Aldo Moro, 5 – 00185 ROMA Boll.Soc.Geol.It. (Ital.J.Geosci.), Vol. 126, No. 2 (2007), pp. 209-222, 5 figs., 3 tabs. Seismogenic evidence of ongoing compression in eastern-central Italy and mainland Sicily: a comparison GIUSY LAVECCHIA (*), RITA DE NARDIS (***), FRANCESCO VISINI (*), FEDERICA FERRARINI (***) & MARIA SERAFINA BARBANO (****) ABSTRACT dall’area padana alla Sicilia. Numerosi autori ritengono che l’attività del fronte sia terminata nel Pleistocene inferiore (PATACCA et alii, We compare the seismogenic role played by two crustal-scale 1990; BUTLER et alii, 1992; LICKORISH et alii, 1999; DI BUCCI & MAZ- reverse-type shear zones located at the outer border of the Apennine- ZOLI, 2002; PATACCA & SCANDONE, 2004), ma altri riportano, almeno Maghrebian fold-and-thrust belt system: the westward-dipping Adriatic per l’Italia centrale e la Sicilia, evidenze di deformazione compressi- Basal Thrust (ABT) in eastern-central Italy and the northward-dipping va tardo pleistocenica-olocenica (BOUSQUET & LANZAFAME, 1986; Sicilian Basal Thrust (SBT) in southern Sicily. The epicentral and MONACO et alii, 1996; FREPOLI & AMATO, 1997; LAVECCHIA et alii, hypocentral distributions and, whenever possible, the kinematics of a 2003; VANNOLI et alii, 2004; MONTONE et alii, 2004; NERI et alii, merged dataset of pre-instrumental (1600 to 1900), early instrumental 2005; CATALANO et alii, 2004 and 2006).
    [Show full text]
  • Download Download
    ANNALS OF GEOPHYSICS, 63, 1, SE101, 2020; doi:10.4401/ag-8327 An integrated geodetic and InSAR technique for the monitoring and detection of active faulting in southwestern Sicily Giovanni Barreca3, Valentina Bruno1, Gino Dardanelli1, Francesco Guglielmino1, 2 ,1 1 1 Mauro Lo Brutto , Mario Mattia* , Claudia Pipitone and Massimo Rossi (1) Istituto Nazionale di Geofisica e Vulcanologia, Osservatorio Etneo, Piazza Roma 2, 95123 Catania, Italy (2) Università degli Studi di Palermo, Dipartimento di Ingegneria, Palermo, Italy (3) Università degli Studi di Catania, Dipartimento di Scienze Geologiche, Biologiche ed Ambientali, Catania, Italy Article history: received July 31, 2019; accepted September 3, 2019 Abstract We present the results of the analysis of GNSS (Global Navigation Satellite System) and InSAR (Interferometric synthetic-aperture radar) data collected in the frame of a project financed by the “Struttura Terremoti” of INGV (Istituto Nazionale di Geofisica e Vulcanologia). Combined investigations pointed out for potential seismogenic sources for destructive earthquakes recorded in southwestern Sicily, including the 1968 Belice earthquake sequence and that supposed to have destroyed the Greek city of Selinunte which, according to geoarcheological data experienced two earthquakes in historical times. Our approach is aimed to evaluate the current deformation rate in SW Sicily and to improve the knowledge about the seismic potential of this area. The geodetic data proposed in this paper show that the Campobello di Mazara–Castelvetrano alignment (CCA) is currently deforming with a vertical and horizontal displacements of 2 mm/yr and 0.5 mm/yr respectively, according to the tectonic setting of the area. Keywords: Belice earthquake; GNSS data; InSar data: Geodesy.
    [Show full text]
  • Overview BELICE Project
    BELICE Building Experience to Lead Initial assesment Challenging Emergency On-line Final Conference - 23rd March 2021 Giuseppe Romano, Project leader BELICE and Regional Director for Tuscany, CNVVF - IT The 1968 Belice earthquake sequence took place in Sicily between 14 and 15 January. The largest shock measured 5.5 on the moment magnitude scale, with five others of magnitude 5+. The maximum perceived intensity was X (Extreme) on the Mercalli intensity scale. The earthquake sequence, centred between the towns of Gibellina, Salaparuta and Poggioreale, killed at least 231 people, about 1,000 injured and left 100,000 homeless. The Cretto di Burri, the "land art" work of the sculptor Alberto Burri that covers the ruins of old Gibellina in the Belice valley. In the Belice valley, old Poggioreale, one of the towns hit by the 1968 earthquake, abandoned with the transfer of the population to the new town; this is the place for the field exercises of the BELICE project, but the pandemic did not allow BENEFICIARIES With the Support of UN-OCHA, INSARAG Secretariat, and Sicily Region, Civil Protection Department France Germany Italy • CNVVF National Fire Corps (Italy) • THW German Federal Agency for Technical Relief (Germany) • EcASC Scoool of Application of Civil Safety (France) • Timesis Srl (Italy) • DPC Italian Department of Civil Protection (Italy) PROJECT BUDGET 75% Co-fin EU TOTAL 937.085,25 € 702.813,92 € Dates Initially foreseen (20 months) June 2019 January 2021 Post COVID (22 months) June 2019 March 2021 INITIAL STRATEGY Drafting and speading
    [Show full text]
  • Paleoseismological Off- Fault Analyses in Eastern Sicily: a Contribute to the Characterization of Seismic Sources”
    UNIVERSITÀ DEGLI STUDI DI CATANIA Facoltà di Scienze Matematiche, Fisiche e Naturali Dipartimento di Scienze Geologiche DOTTORATO DI RICERCA in “Evoluzione geologica di orogeni di tipo mediterraneo” XXIII CICLO “Paleoseismological off- fault analyses in eastern Sicily: a contribute to the characterization of seismic sources” Tesi di dottorato di: Coordinatore: Prof. C. Monaco Claudia Pirrotta Tutor: Prof.ssa M.S. Barbano Anno Accademico 2009/10 Tesi di dottorato in “Evoluzione geologica di orogeni di tipo mediterraneo” di Claudia Pirrotta PALEOSEISMOLOGICAL OFF- FAULT ANALYSES IN EASTERN SICILY: A CONTRIBUTE TO THE CHARACTERIZATION OF SEISMIC SOURCES Riassunto …………………………………………………….……........................................i Abstact ……………………………………………………………........................................i Chapter 1 1- Geological and seismological features of Sicily……………………………………..…...1 1.1- Geological and structural setting of eastern Sicily…………………………...………...2 1.2- Eastern Sicily historical earthquakes and related seismogenic sources ……..…………7 Chapter 2 2- Earthquake Geology……………………………………………...……………………..18 2.1- Primary effects…………………………………………………………………..........20 2. 2- Secondary effects ……………………………………………………………...……..22 2.2.1- Landslides and rock-falls ……………………………………………………...…....23 2.2.2- Ground deformations ………………………………………………………..……...26 2.2.3- Liquefactions: soft sediment deformations …………………………………….…...30 2.2.4- Hydrological anomalies ……………………………………………………...……..34 2.2.5- Tsunami deposits ……………………………………………………………..…… 35 Chapter 3 3- Paleoseismology
    [Show full text]
  • Correlation Between Seismic and Volcanic
    Chapter 2 Correlation between Seismic and Volcanic Activity at a Large Spatial Scale in Italy: Examples from the Neapolitan Volcanic District (Vesuvius Volcano, Southern Italy) Pier Luigi Bragato PierAdditional Luigi information Bragato is available at the end of the chapter Additional information is available at the end of the chapter http://dx.doi.org/10.5772/intechopen.71977 Abstract The time correlation between the eruptions of Mt Vesuvius and the occurrence of strong earthquakes in Italy has been revised using new and improved catalogs and data made available in the last decade. It has been shown that this correlation is statistically signifi- cant and involves also the earthquakes located very far from the volcanic edifice (hun- dreds of kilometers). In particular, the earthquakes and the Vesuvius’ eruptions agree on a transient of accelerated activity between 1600 and 1900. A similar correlation has been found between the seismicity and the uplift episodes at the nearby Campi Flegrei caldera occurred in the last 70 years: there is strict similarity between the two cycles, the first one centered around 1970–1980 and the second one started on 2004 and still continuing and involving recent strong earthquakes (2009 L’Aquila earthquake, 2012 Emilia earthquake and 2016 Central Italy earthquake). The synchronization to such a long distance has sug- gested the occurrence of large-scale climatic processes controlling both the earthquakes and the volcanism. The comparison with climatic indexes like the global surface tempera- ture and the extension of glaciers in western-central Europe has indicated a possible role of climatic parameters in controlling volcanism and seismicity.
    [Show full text]