DOCSLIB.ORG

Geo-Risks in the Mediterranean and Their Mitigation

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text

Load more

Geo-Risks in the Mediterranean and their Mitigation 1 Geo-Risks in the Mediterranean and their Mitigation Proceedings of the International Conference: GEORISKS IN THE MEDITERRANEAN AND THEIR MITIGATION University of Malta - Valletta Campus 20-21 July 2015 Organizing Committee Volume Edited by: Galea P., Borg Dr. Pauline Galea R.P., Farrugia D., Agius M.R., Dr. Sebastiano D‘Amico D'Amico S., Torpiano A., Bonello M.. Dr. Ruben P. Borg Dr. Matthew R. Agius Ms. Daniela Farrugia Prof. Alex Torpiano Dr. Marc Bonello Ms Ann-Marie Ellul Ms Alison Darmanin Ms. Lucienne Bugeja An international scientific conference organised jointly by the Seismic Monitoring and Research Unit, Department of Geoscience, Faculty of Science and Department of Civil and Structural Engineering, Faculty of the Built Environment, University of Malta. Part of the SIMIT project: Integrated civil protection system for the Italo-Maltese cross-border area. Italia-Malta Programme – Cohesion Policy 2007-2013 A sea of opportunities for the future Tender part-financed by the European Union European Regional Development Fund (ERDF) Co-financing rate: 85% EU Funds; 15% National Funds. Investing in your future. 2 Geo-Risks in the Mediterranean and their Mitigation Proceedings of the International Conference: GEORISKS IN THE MEDITERRANEAN AND THEIR MITIGATION Edited by: Galea P., Borg R.P., Farrugia D., Agius M.R., D'Amico S., Torpiano A., Bonello M. Published by Mistral Service sas, Via U. Bonino, 3, 98100 Messina (Italy) Printed by Gutenberg Press Ltd, Gudja Road, Tarxien, GXQ 2902, Malta, This book is distributed as an Open Access work. All users can download copy and use the present volume as long as the author and the publisher are properly cited. Important Notice The publisher does not assume any responsibility for any damage or injury to property or persons arising out of the use of any materials, instructions, methods or ideas contained in this book. Opinions and statements expressed in this book are those of the authors and not those of the publisher. Furthermore, the publisher does not take any responsibility for the accuracy of information contained in the present volume. For interpretation of the references to colour, the reader is referred to the web version of the book. A free online copy of this book is available at www.mistralservice.it First published: July, 2015 Prepared in Italy Proceedings of the International Conference: GEORISKS IN THE MEDITERRANEAN AND THEIR MITIGATION Edited by: Galea P., Borg R.P., Farrugia D., Agius M.R., D'Amico S., Torpiano A., Bonello M. ISBN:978-88-98161-20-1 (pdf) ISBN:978-88-98161-22-5 (paper back) 3 Geo-Risks in the Mediterranean and their Mitigation Table of contents A NEW EARTHQUAKE MONITORING STRATEGY IN A CROSS-BORDER SEISMIC ZONE Mucciarelli, M 13 DERIVATION OF SEISMIC FRAGILITY CURVES FOR MASONRY BUILDINGS WITH THE AID OF ADVANCED ANALYSIS TOOLS Kappos, A.J. 17 RE-EVALUATION OF THE SEISMICITY AND SEISMIC HAZARD ASSESSMENT OF LIBYA Abdunnur Ben-Suleman, Abdalmonam A.Swissi 25 STRATIGRAPHIC FEATURES OF THE MALTESE ARCHIPELAGO: A SYNTHESIS Baldassini, N., Di Stefano, A 26 HUNTING FOR PAST EARTHQUAKES IN THE CENTRAL MEDITERRANEAN; SOME EMBLEMATIC CASES FROM THE SICILIAN COLLISION ZONE Barreca, G., Guzzetta, L. Ferranti, L., Monaco, C 33 SEISMOLOGICAL AND SEISMIC REFLECTION EVIDENCE FOR ACTIVE TECTONICS IN THE EASTERN ALBORAN BASIN Bouskri, G., Elabbassi, M., El Ouai, D., Ammar, A., Harnafi, M. 40 COMBINING GEOLOGICAL AND GEOPHYSICAL DATA: NEW INSIGHTS ABOUT WESTERN CATANZARO TROUGH (CALABRIA, SE TYRRHENIAN SEA) Brutto, F., Muto, F., Loreto, M.F., CritelliS., Tripodi V. 42 THE LITHOSPHERIC STRUCTURE OF THE GIBRALTAR ARC AND POSSIBLE IMPLICATIONS FOR SEISMIC HAZARD IN THE WESTERN MEDITERRANEAN Carbonell, R, J. Díaz, J. Gallart and PICASSO working group 48 NEOGENE TECTONIC REACTIVATION IN THE NORTH-CENTRAL SECTOR OF THE SICILY CHANNEL IN THE FRAME OF THE SOUTHWARD ADVANCING OF THE GELA NAPPE Cavallaro, D., Monaco, C., Polonia, A., Sulli, A., Di Stefano, A. 50 GEOLOGY AND SEISMIC ACTIVITY AND THEIR INDUCED EFFECTS IN THE NORTH-WEST OF ALGERIA Louni Chahira , Belhai Djelloul 57 GEOLOGICAL AND SEISMOLOGICAL CONSTRAINTS FOR FAULT REACTIVATION IN THE HYBLEAN FORELAND (SE SICILY, ITALY) Cultrera, F., Barreca, G., Scarfì, L., Monaco, C. 58 NEW INSIGHTS ON THE TECTONIC EVOLUTION OF THE LAMPEDUSA SHELF FROM INTERPRETATION OF SEISMIC REFLECTION PROFILES AND FIELD DATA Meccariello, M., Ferranti, L., Barreca, G., Di Stefano, A., Monaco, C. 66 4 Geo-Risks in the Mediterranean and their Mitigation CURRENT TECTONIC ACTIVITY IN THE NW SECTOR OF THE SICILY CHANNEL BASED ON SEISMIC PROFILE ANALYSIS Meccariello, M., Ferranti, L., Pepe, F. 68 NEOTECTONIC DEFORMATION MODEL FOR THE NORTHERN ALGERIA: PALEOMAGNETIC AND STRUCTURAL CONSTRAINTS. Derder, M., Maouche, S., Henry, B., Bayou, B., Amenna, M., Ayache, M. 70 MEDITERRANEAN SEISMICITY IN A FRAME OF GLOBAL SEISMIC ACTIVITY Sandu, I. 72 TESTING THE MOMENT RATIO METHOD IN FORECASTING WORLDWIDE SEISMICITY Talbi, A., Mobarki, M 73 GROUND MOTION SCALING IN THE SICILY CHANNEL: IMPLICATIONS FOR SEISMIC HAZARD ASSESSMENT Akinci, A., D‘Amico S., M.,Pischiutta M. 76 SEISMIC SOURCES MAPPING CASES OF STUDIES: CONSTANTINE REGION (NORTH-EASTERN ALGERIA) Aourari, S 77 EXTREME WAVES IMPACT ON MALTA (MEDITERRANEAN SEA) Biolchi, S., Furlani, S., Antonioli, F., Baldassini, N., Cucchi, F., Deguara, J., Devoto S., Di Stefano, A., Evans, J.,Gambin, T., Gauci, R., Mastronuzzi, G.A., Monaco, C., Scicchitano, G. 83 THE BLIND FAULT MOSTAGANEM BOUKHEDIMI (PLATEAU OF MOSTAGANEM) NORTHWESTERN OF ALGERIA Boukhedimi M Amine., Benhamouche, A., Machane, D. 91 EVIDENCE OF EXTREME WAVE EVENTS FROM BOULDER DEPOSITS ON THE SOUTH-EAST COAST OF MALTA: STORM OR TSUNAMI? Causon Deguara, J., Gauci, R. 94 FORECASTING MODERATE EARTHQUAKES A STEP TOWARDS SEISMIC RISK REDUCTION IN NORTHERN ALGERIA AND MOROCCO M. Hamdache M., Peláez J.A. 98 SEISMIC HAZARD PARAMETERS OF MAIN SEISMOGENIC SOURCE ZONE MODEL IN THE ALGERIA-MOROCCO REGION Hamdache, M , Pelaez J. A., Kijko A., Smit A., Sawires R. 99 FAULT RUPTURE HAZARD ALONG A SECTOR WITH ASEISMIC CREEP IN URBAN AREA (EASTERN SICILY) Imposa, S., De Guidi, G.,Scudero, S., Grassi, S. 102 SEISMIC AND TSUNAMI HAZARD ASSESSMENT OF A COASTAL ACTIVE FAULT CONSTRAINED WITH THE HISTORICAL CALABRIA 1905 EARTHQUAKE (SE TYRRHENIAN SEA) Loreto, M.F., Brutto, F., Muto, F., Armigliato, A., Pagnoni, G., Sandron, D., Tiberi, L., Tinti, S., Zgur F. 110 5 Geo-Risks in the Mediterranean and their Mitigation SUBMARINE LANDSLIDES OF THE CENTRAL MEDITERRANEAN SEA: STATE-OF- THE-ART AND CURRENT CHALLENGES 118 Micallef, A., Cunarro Otero, D. SITE CHARACTERIZATION AT ALGIERS CITY USING PEAK GROUND AND SPECTRAL ACCELRATIONS 120 Mobarki, M., Talbi, A. THE MOST IMPORTANT ENVIRONMENTAL EFFECTS TRIGGERED BY HISTORICAL EARTHQUAKES FROM 17TH TO 19TH CENTURY IN THE APULIA REGION (CENTRAL MEDITERRANEAN SEA) 123 Nappi, R., Gaudiosi, G., Alessio, G., De Lucia, M., Porfido, S. LEARNING MORE ABOUT 1990 DECEMBER 13TH IN SOUTH-EASTERN SICILY: EARTHQUAKE SCENARIOSIN THE SIRACUSA URBAN AREA, ITALY Panzera, F., D‘Amico, S., Lombardo, G. 132 A REGIONAL EARTHQUAKE EARLY WARNING SYSTEM: PRESTO@CE RN Pesaresi, D., Picozzi, M., Ţivčić, M., Lenhardt, W., Mucciarelli, M., Elia, L., Zollo, A., Gosar, A. 137 SUBMARINE EARTHQUAKE GEOLOGY AS A TOOL FOR SEISMIC HAZARD ASSESSMENT IN THE CENTRAL MEDITERRANEAN SEA: POTENTIAL, LIMITS, TECHNIQUES AND RESULTS Polonia, A., Romano, S., Vaiani, S., Gasparotto, G., Torelli, L., Gasperini, L. 142 THE 1976 GUATEMALA EARTHQUAKE REVISED. MACROSEISMIC DATA FOR AN APPROPRIATE SEISMIC HAZARD ASSESSMENT Porfido S., Caccavale M., Spiga E., Sacchi M. 146 PROBABILISTIC SEISMIC HAZARD ANALYSIS FOR MOLDAVIAN AND TURKEY TERRITORIES Burtiev, R. 154 PROS AND CONS OF SEISMIC HAZARD ANALYSIS Romeo, R.W. 156 SEISMIC HAZARD DEAGGREGATION FOR SELECTED EGYPTIAN CITIES Sawires, R., Fat-Helbary, R.E., Peláez, J.A., Ibrahim, H.A., Hamdache, M., Panzera, F. 158 AN INTEGRATED APPROACH FOR LANDSLIDE HAZARD ASSESSMENT ON THE NW COAST OF MALTA Soldati, M., Devoto, S., Foglini, F., Forte, E., Mantovani, M., Pasuto, A., Piacentini, D., Prampolini, M. 160 SCENARIOS OF DEBRIS FLOW MODELLING BEFORE AND AFTER THE BUILDING OF MITIGATION WORKS: CASE STUDY IN VAL CANALE VALLEY (FRIULI VENEZIA GIULIA, ITALY) Boccali C., Calligaris C., Lapasin R., Zini L., Cucchi F. 168 SITE CHARACTERISATION AND RESPONSE STUDY IN RABAT, MALTA Farrugia, D., Paolucci, E., D‘Amico S., Galea P. 174 6 Geo-Risks in the Mediterranean and their Mitigation SEISMIC CHARACTERIZATION OF SOILS IN THE CITY OF LORCA (SE SPAIN) FROM AMBIENT NOISE MEASUREMENTS Garcia-Fernandez, M., Albarello, D., Jimenez, MJ ,Massini, F., Lunedei, E. 180 GEOPHYSICAL SURVEYS TO STUDY A LANDSLIDE BODY (NORTH-EASTERN SICILY) Imposa, S., Fazio, F., Grassi, S., Cino, P., Rannisi, G. 182 SEISMIC SITE RESPONSE AT LAMPEDUSA ISLAND, ITALY Panzera, F., Sicali, S., Lombardo, G. 188 DYNAMIC CHARACTERIZATION AND DECONVOLUTION ANALYSIS FOR SOME SITES OF THE ITALIAN ACCELEROMETRIC NETWORK (RAN) Paolucci, E., Albarello, D., Lunedei, E., Peruzzi, G., Papasidero, M. P., Francescone, M. 194 PRELIMINARY RESULTS FROM AN INTEGRATED SHALLOW GEOPHYSICAL INVESTIGATION IN THE NORTH-EASTERN SECTOR OF THE MALTA ISLAND Pischiutta, M., Villani, F., Vassallo, M., Galea, P., D'Amico, S., Amoroso, S., Cantore, L., Di Naccio D., Mercuri, A., Rovelli, A., Famiani, D., Cara, F., Di Giulio, G., Akinci, A. 199 SALTWATER INTRUSION IN FRIULI LOW PLAIN Zavagno, E.,Zini, L., Cucchi F. 205 GPR PROSPECTING ON LARGE BURIED CRYPTS: THE CASE HISTORY OF THE CHURCH OF SANTA MARIA DEL SUFFRAGIO IN GRAVINA IN PUGLIA (APULIA, SOUTHERN ITALY) Matera, L., Ciminale, M., Leucci, G., De Giorgi, L., Piro, S., Persico, R. 212 ON THE DEFINITION OF SEISMIC VULNERABILITY MAPS IN CROSS-BORDER MEDITERRANEAN AREAS Cavaleri, L., Di Trapani, F., Macaluso, G., Bilello, C. 221 PRELIMINARY ASSESSMENT OF THE SEISMIC VULNERABILITY OF LOAD- BEARING MASONRY BUILDINGS IN MALTA THROUGH NUMERICAL MODELLING. Cicero, C., Borg., R. P., Bonello, M., Lombardo, G. 229 ANALYSIS AND EVALUATION OF THE SEISMIC VULNERABILITY OF THE STRUCTURAL AGGREGATE.THE STUDY CASE OF ORTIGIA Cicero, C., Lombardo, G.
Recommended publications
  • Flood Loss Modelling with FLF-IT: a New Flood Loss Function for Italian Residential Structures

    Flood Loss Modelling with FLF-IT: a New Flood Loss Function for Italian Residential Structures

    Nat. Hazards Earth Syst. Sci. Discuss., doi:10.5194/nhess-2017-92, 2017 Manuscript under review for journal Nat. Hazards Earth Syst. Sci. Discussion started: 6 March 2017 c Author(s) 2017. CC-BY 3.0 License. Flood loss modelling with FLF-IT: A new Flood Loss Function for Italian residential structures Roozbeh Hasanzadeh Nafari1,2, Mattia Amadio3,4, Tuan Ngo5 and Jaroslav Mysiak3,4 1Centre for Disaster Management and Public Safety (CDMPS), Department of Infrastructure Engineering, University of 5 Melbourne, Melbourne, 3010, Australia 2Bushfire & Natural Hazards Cooperative Research Centre, Melbourne, 3002, Australia 3Fondazione Eni Enrico Mattei (FEEM) and Euro-Mediterranean Centre on Climate Change (CMCC), San Giorgio Maggiore, Venice, Italy 4Ca’ Foscari University, Venice Centre for Climate Studies (VICCS), Venice, Italy 10 5Director of the Advanced Protective Technologies for Engineering Structures (APTES) Group, Department of Infrastructure Engineering, University of Melbourne, Melbourne, 3010, Australia Correspondence to: R. Hasanzadeh Nafari ([email protected]) Abstract. The damage triggered by different flood events costs the Italian economy millions of dollars each year. This cost is likely to increase in the future due to climate variability and economic development. In order to avoid or reduce such 15 significant financial losses, risk management requires tools which can provide a reliable estimate of potential flood impacts across the country. Flood loss functions are an internationally accepted method for estimating physical flood damage in urban areas. In this study, we derived a new Flood Loss Function for Italian residential structures (FLF-IT), on the basis of empirical damage data collected from a recent flood event in the region of Emilia-Romagna.
  • Social and Material Vulnerability in the Face of Seismic Hazard: an Analysis of the Italian Case

    Social and Material Vulnerability in the Face of Seismic Hazard: an Analysis of the Italian Case

    Social and material vulnerability in the face of seismic hazard: an analysis of the Italian case Oleksandr Didkovskyiy;], Giovanni Azzone∗;], Alessandra Menafoglioy, Piercesare Secchiy;] y MOX - Dipartimento di Matematica, Politecnico di Milano, Italy ∗ Dipartimento di Ingegneria Gestionale, Politecnico di Milano, Italy ] Center for Analysis, Decisions and Society, Human Technopole, Italy Abstract The assessment of the vulnerability of a community endangered by seismic hazard is of paramount importance for planning a precision policy aimed at the prevention and reduction of its seismic risk. We aim at measuring the vulnerability of the Italian municipalities exposed to seismic hazard, by analyzing the open data offered by the Mappa dei Rischi dei Comuni Italiani provided by ISTAT, the Italian National Institute of Statistics. Encompassing the Index of Social and Material Vulnerability already computed by ISTAT, we also consider as referents of the latent social and material vulnerability of a community, its demographic dynamics and the age of the building stock where the community resides. Fusing the analyses of different indicators, within the context of seismic risk we offer a tentative ranking of the Italian municipalities in terms of their social and material vulnerability, together with differential profiles of their dominant fragilities which constitute the basis for planning precision policies aimed at seismic risk prevention and reduction. 1 Introduction After the tragic sequence of earthquakes near Amatrice in 2016, the Italian government set up the Casa Italia task force1 to develop a plan for housing and land care directed to the better protection of citizens, and public and private goods, against natural risks. One of the first activities of Casa Italia was aimed at integrating and enhancing the rich information on natural risks already available as the result of numerous and continuing investigations carried out by several national institutions2.
  • Spatiotemporal Pattern of Social Vulnerability in Italy

    Spatiotemporal Pattern of Social Vulnerability in Italy

    Int J Disaster Risk Sci (2018) 9:249–262 www.ijdrs.com https://doi.org/10.1007/s13753-018-0168-7 www.springer.com/13753 ARTICLE Spatiotemporal Pattern of Social Vulnerability in Italy 1 2 1 1 Ivan Frigerio • Fabio Carnelli • Marta Cabinio • Mattia De Amicis Published online: 30 April 2018 Ó The Author(s) 2018 Abstract Evaluation of social vulnerability (SV) against periods. The SVI of many areas in the center and the south natural hazards remains a big challenge for disaster risk of the peninsula remained stable, and the people living reduction. Spatiotemporal analysis of SV is important for there have continued to be potentially vulnerable to natural successful implementation of prevision and prevention hazards. measures for risk mitigation. This study examined the spatiotemporal pattern of SV in Italy, and also analyzed Keywords Bivariate Moran’s index Á Cluster socioeconomic factors that may influence how the Italian analysis Á Italy Á Natural hazards Á Social vulnerability population reacts to catastrophic natural events. We iden- tified 16 indicators that quantify SV and collected data for the census years 1991, 2001, and 2011. We created a social 1 Introduction vulnerability index (SVI) for each year by using principal component analysis outputs and an additive method. Reading the special report of the IPCC (2012)on Exploratory spatial data analysis, including global and Managing the Risks of Extreme Events and Disasters to local autocorrelations, was used to understand the spatial Advance Climate Change Adaptation and the more recent patterns of social vulnerability across the country. Specif- Climate Change 2014: Impacts, Adaptation, and Vulnera- ically, univariate local Moran’s index was performed for bility (IPCC 2014), it is evident that remarkable progress in the SVI of each of the three most recent census years in research has been made in integrating social vulnerability, order to detect changes in spatial clustering during the natural hazards, and climate change.
  • (Globigerina Limestone Formation): New Preliminary Data Based on Calcareous Plankton

    (Globigerina Limestone Formation): New Preliminary Data Based on Calcareous Plankton

    Bollettino della Società Paleontologica Italiana, 46 (2-3), 2007, 175-181. Modena, 15 gennaio 2008175 Biostratigraphy and chronostratigraphy of the Maltese Lower Globigerina Limestone Member (Globigerina Limestone Formation): new preliminary data based on calcareous plankton Luca Maria FORESI, Roberto MAZZEI, Gianfranco SALVATORINI & Francesca DONIA L.M. Foresi, Dipartimento di Scienze della Terra, Università di Siena, Via Laterina 8, I-53100 Siena, Italy; [email protected] R. Mazzei, Dipartimento di Scienze della Terra, Università di Siena, Via Laterina 8, I-53100 Siena, Italy; [email protected] G. Salvatorini, Dipartimento di Scienze della Terra, Università di Siena, Via Laterina 8, I-53100 Siena, Italy. F. Donia, Dipartimento di Scienze della Terra, Università di Siena, Via Laterina 8, I-53100 Siena, Italy; [email protected] KEY WORDS - Calcareous plankton biostratigraphy, Chattian, Lower Globigerina Limestone, Maltese Islands. ABSTRACT - The preliminary results of the study carried out on calcareous plankton (foraminifera and nannofossils) assemblages from the Maltese Lower Globigerina Limestone are presented here. The Lower Globigerina Limestone (LGL) is the lowermost member of the Globigerina Limestone Formation, widely outcropping in the Maltese Archipelago; this member has been generally referred to the Early Miocene (Aquitanian). The investigation of 78 samples from 11 sections (encompassing the whole succession of the unit) on Gozo and Malta islands (one of them close to the type section of the formation) has allowed us to assign a Chattian age (Late Oligocene) to the Lower Globigerina Limestone Member (LGLM). Globigerinoides primordius, Paragloborotalia opima nana, P. pseudokugleri, Subbotina gortanii, Globoturborotalita angulisuturalis, G. anguliofficinalis, and Coccolithus miopelagicus, Cyclicargolithus abisectus, Dictyococcites bisectus, D. scrippsae, Helicosphaera recta, Sphenolithus cf.
  • Karst Heritage

    Karst Heritage

    Unit 4 – Karst Heritage Dirk De Ketelaere, Josianne Vella and Anna Spiteri Preamble In this unit, we examine the relation between hydrological processes, the geology of karst rock and the resultant landforms. While being described as ‘unusual’, the landforms may take such dramatic proportions that they merit the designation of a World Heritage Conservations Site. The Qawra/Dwejra area in Gozo is presented as a case study. “The importance of conserving representative karst areas for science and recreation has been recognized in many countries by the designation of national parks and reserves” (Ford et al., 1989) “Some of the best examples of normal faulting, karstification and solution subsidence, cliff recession, cave formation as a result of marine erosion, and incision of steep-sided valleys to be found in the Maltese Islands occur here” (Cassar et al, 2004) on the Qawra/Dwejra area in Gozo Karst Landscapes Karst landscapes or terrains represent a distinctive topography in which the landscape is largely shaped by the dissolving action of water on carbonate bedrock. This geological process, occurring over many thousands of years, results in unusual surface and subsurface features ranging from sinkholes, dolines, vertical shafts, disappearing streams and springs, to complex underground drainage systems and caves. The ‘engine’ that powers this natural process is the hydrological cycle, starting with the constant flow of rainfall over the rock surface which causes the chemical dissolution of the rock along fissures. Over time, these fissures gradually enlarge into veritable shafts and conduits, which allow a larger part of the rainwater to feed into the aquifers within a shorter period of time.
  • Earthquake Potential Along the Hayward Fault, California

    Earthquake Potential Along the Hayward Fault, California

    Missouri University of Science and Technology Scholars' Mine International Conferences on Recent Advances 1991 - Second International Conference on in Geotechnical Earthquake Engineering and Recent Advances in Geotechnical Earthquake Soil Dynamics Engineering & Soil Dynamics 10 Mar 1991, 1:00 pm - 3:00 pm Earthquake Potential Along the Hayward Fault, California Glenn Borchardt USA J. David Rogers Missouri University of Science and Technology, [email protected] Follow this and additional works at: https://scholarsmine.mst.edu/icrageesd Part of the Geotechnical Engineering Commons Recommended Citation Borchardt, Glenn and Rogers, J. David, "Earthquake Potential Along the Hayward Fault, California" (1991). International Conferences on Recent Advances in Geotechnical Earthquake Engineering and Soil Dynamics. 4. https://scholarsmine.mst.edu/icrageesd/02icrageesd/session12/4 This work is licensed under a Creative Commons Attribution-Noncommercial-No Derivative Works 4.0 License. This Article - Conference proceedings is brought to you for free and open access by Scholars' Mine. It has been accepted for inclusion in International Conferences on Recent Advances in Geotechnical Earthquake Engineering and Soil Dynamics by an authorized administrator of Scholars' Mine. This work is protected by U. S. Copyright Law. Unauthorized use including reproduction for redistribution requires the permission of the copyright holder. For more information, please contact [email protected]. Proceedings: Second International Conference on Recent Advances In Geotechnical Earthquake Engineering and Soil Dynamics, March 11-15, 1991 St. Louis, Missouri, Paper No. LP34 Earthquake Potential Along the Hayward Fault, California Glenn Borchardt and J. David Rogers USA INTRODUCTION TECTONIC SETI'ING The Lorna Prieta event probably marks a renewed period of The Hayward fault is a right-lateral strike-slip fea­ major seismic activity in the San Francisco Bay Area.
  • A Landscape Assessment Study of the South Gozo Fault Area Mariella Xuereb James Madison University

    A Landscape Assessment Study of the South Gozo Fault Area Mariella Xuereb James Madison University

    James Madison University JMU Scholarly Commons Masters Theses The Graduate School Fall 12-18-2010 A landscape assessment study of the South Gozo Fault area Mariella Xuereb James Madison University Follow this and additional works at: https://commons.lib.jmu.edu/master201019 Part of the Environmental Sciences Commons Recommended Citation Xuereb, Mariella, "A landscape assessment study of the South Gozo Fault area" (2010). Masters Theses. 434. https://commons.lib.jmu.edu/master201019/434 This Thesis is brought to you for free and open access by the The Graduate School at JMU Scholarly Commons. It has been accepted for inclusion in Masters Theses by an authorized administrator of JMU Scholarly Commons. For more information, please contact [email protected]. A Landscape Assessment Study of the South Gozo Fault Area Mariella Xuereb Master of Science in Sustainable Environmental Resource Management University of Malta 2010 A Landscape Assessment Study of the South Gozo Fault Area A dissertation presented in part fulfillment of the requirements for the Degree of Master of Science in Sustainable Environmental Resource Management Mariella Xuereb November 2010 Supervisor: Dr. Louis. F. Cassar Co-Supervisors: Ms. Elisabeth Conrad; Dr. Maria Papadakis University of Malta – James Madison University ii. This research work disclosed in this publication is partly funded by the Strategic Educational Pathways Scholarship (Malta). Operational Programme II – Cohesion Policy 2007-2013 Empowering People for More Jobs and a Better Quality of Life Training part-financed by the European Union European Social Fund Co-financing rate: 85% EU Funds; 15% National Funds Investing in your future iii. ABSTRACT Mariella Xuereb A Landscape Assessment Study of the South Gozo Fault Area The South Gozo Fault region features a heterogeneous landscape which extends from Ras il-Qala on the east, to „Mgarr ix-Xini‟ on the south-eastern littoral.
  • Transactions of the Botanical Society of Edinburgh I. Notes on the Botany

    Transactions of the Botanical Society of Edinburgh I. Notes on the Botany

    This article was downloaded by: [UQ Library] On: 14 March 2015, At: 14:07 Publisher: Taylor & Francis Informa Ltd Registered in England and Wales Registered Number: 1072954 Registered office: Mortimer House, 37-41 Mortimer Street, London W1T 3JH, UK Transactions of the Botanical Society of Edinburgh Publication details, including instructions for authors and subscription information: http://www.tandfonline.com/loi/tped18 I. Notes on the Botany and Agriculture of Malta and Sicily H. Cleghorn M.D. Published online: 01 Dec 2010. To cite this article: H. Cleghorn M.D. (1870) I. Notes on the Botany and Agriculture of Malta and Sicily , Transactions of the Botanical Society of Edinburgh, 10:1-4, 106-139, DOI: 10.1080/03746607009468660 To link to this article: http://dx.doi.org/10.1080/03746607009468660 PLEASE SCROLL DOWN FOR ARTICLE Taylor & Francis makes every effort to ensure the accuracy of all the information (the “Content”) contained in the publications on our platform. However, Taylor & Francis, our agents, and our licensors make no representations or warranties whatsoever as to the accuracy, completeness, or suitability for any purpose of the Content. Any opinions and views expressed in this publication are the opinions and views of the authors, and are not the views of or endorsed by Taylor & Francis. The accuracy of the Content should not be relied upon and should be independently verified with primary sources of information. Taylor and Francis shall not be liable for any losses, actions, claims, proceedings, demands, costs, expenses, damages, and other liabilities whatsoever or howsoever caused arising directly or indirectly in connection with, in relation to or arising out of the use of the Content.
  • GEOLOGY of MALTA Victoria Griffiths

    GEOLOGY of MALTA Victoria Griffiths

    GEOLOGY OF MALTA Victoria Griffiths The Maltese Archipelago consists of a group of point on the archipelago is 253m above mean small, low-lying islands located in the central sea level and is situated at Dingli Cliffs on the Mediterranean, approximately 96km South of south-western coast. The tilt of the archipelago Sicily and 320km north of North Africa. The is responsible for the predominant north- archipelago extends for 45km in a NW-SE eastern trend of drainage channels on Malta. direction. The largest islands are Malta and Gozo. The other islands of the archipelago are Malta is crossed by two main fault systems much smaller and comprise Comino, St Paul's representing the effects of two separate rifting Islands, Cominotto, Filfla and General's Rock. episodes in the vicinity of the archipelago. The older of the two, the Great Fault, trends SW to The rocks of the Maltese Islands are all NE, while the Maghlaq Fault system trends sedimentary and result from the accumulation approximately NW to SE along the southern of carbonate sediments in a relatively shallow coast of the island and has been responsible for marine environment. Various types of rocks the downthrow of Filfla to sea level. A system correspond to different palaeo-environments of of horst and graben structures of East- deposition. A second class of rocks, quaternary Northeast trend characterises Malta north of the deposits, represent sediments that were Great Fault. These structures are indicated by deposited in a terrestrial environment prominent ridges and valleys. No well-defined following the emergence of the Maltese Islands horst and graben systems occur south of the above sea level.
  • The Implications of Fault Zone Transformation on Aseismic Creep

    The Implications of Fault Zone Transformation on Aseismic Creep

    PUBLICATIONS Journal of Geophysical Research: Solid Earth RESEARCH ARTICLE The implications of fault zone transformation on aseismic 10.1002/2016JB013803 creep: Example of the North Anatolian Fault, Turkey Key Points: Maor Kaduri1, Jean-Pierre Gratier1, François Renard1,2 , Ziyadin Çakir3, and Cécile Lasserre1 • Massive limestones deform seismically; aseismic creep is 1ISTerre, University Grenoble Alpes and CNRS, Grenoble, France, 2Department of Geosciences, Physics of Geological observed only in volcanic rocks 3 with clay gouges Processes, University of Oslo, Oslo, Norway, Department of Geology, Istanbul Technical University, Istanbul, Turkey • Clay gouges result from transformations of rocks during seismic and aseismic deformation Abstract Aseismic creep is observed at surface along several segments of the North Anatolian right-lateral • Aseismic creep mechanism is a active fault in Turkey, a major plate boundary between Eurasia and Anatolia. Identifying the mechanisms that combination of pressure solution viscous creep and grain frictional control creep and their temporal and spatial change represents a major challenge for predicting the sliding mechanical evolution of active faults, the interplay between creep and earthquakes, and the link between short-term observations from geodesy and the long-term fault zone evolution. We combine geological Supporting Information: observations, laboratory analyses, and imaging techniques, shedding new light on the mechanism of fault • Supporting Information S1 creep along the North Anatolian Fault (NAF) and its time-dependent change. A clear correlation is shown between shallow creep and near-surface fault gouge composition: locked segments of the NAF are mostly Correspondence to: composed of massive limestones without clay gouges, whereas creeping segments comprise clay gouges F. Renard, [email protected] that contain low-friction minerals.
  • Landslide Occurances at Maierato, Italy. an Engineering Geological View

    Landslide Occurances at Maierato, Italy. an Engineering Geological View

    University of Pennsylvania ScholarlyCommons Master of Science in Applied Geosciences Department of Earth and Environmental Project Designs Science 8-1-2010 Landslide Occurances at Maierato, Italy. An Engineering Geological View Jaithish John University of Pennsylvania Follow this and additional works at: https://repository.upenn.edu/msag_projects Part of the Earth Sciences Commons John, Jaithish, "Landslide Occurances at Maierato, Italy. An Engineering Geological View" (2010). Master of Science in Applied Geosciences Project Designs. 2. https://repository.upenn.edu/msag_projects/2 A Project design submitted to the Graduate Faculty of The University of Pennsylvania partial fulfillment of the Requirements for the Degree of Master of Science in Applied Geosciences Summer 2010. This paper is posted at ScholarlyCommons. https://repository.upenn.edu/msag_projects/2 For more information, please contact [email protected]. Landslide Occurances at Maierato, Italy. An Engineering Geological View Abstract This paper focuses on the 15th February, 2010 Maierato landslide in the Calabria region of Italy. The slide is believed to have been induced by heavy rainfall and happened just west of the town. The Italian basin of the Mediterranean and the peninsula are often affected by patterns of intense precipitation. About 2300 people have been evacuated just before the slide happened. No deaths or injuries have been reported. The authorities have predicted that a landslide could be happening as they have indicated the signs on the road (Figure A1) The town of Maierato was affected by slope instability not only due to the heavy rainfall but also due to the existing geological structure, the plastic properties of soil of sliding surface, infiltration of water into the soil , erosion of soil at the toe of the slide and increasing ground water level.
  • Factors of Vulnerability in the Case of Multiple Hazards

    Factors of Vulnerability in the Case of Multiple Hazards

    Munich Personal RePEc Archive Be (and have) good neighbours! Factors of vulnerability in the case of multiple hazards Pagliacci, Francesco and Russo, Margherita Dipartimento di Economia Marco Biagi, and CAPP (Centro Analisi Politiche Pubbliche), Università degli Studi di Modena e Reggio Emilia. Viale Berengario 51, 41121 Modena, Italy 17 December 2018 Online at https://mpra.ub.uni-muenchen.de/98044/ MPRA Paper No. 98044, posted 11 Jan 2020 11:15 UTC Accepted manuscript Ecological Indicators 2020 https://doi.org/10.1016/j.ecolind.2019.105969 CC-BY-NC-ND license Be (and have) good neighbours! Factors of vulnerability in the case of multiple hazards Francesco Pagliacci1*, Margherita Russo2 Dipartimento di Economia Marco Biagi, and CAPP (Centro Analisi Politiche Pubbliche), Università degli Studi di Modena e Reggio Emilia. Viale Berengario 51, 41121 Modena, Italy 1e-mail: [email protected]; ORCID: 0000-0002-3667-7115 2 e-mail [email protected]; ORCID: 0000-0002-7277-1002 * Correspondence to be sent to: Francesco Pagliacci, Department of Economics “Marco Biagi”, Università di Modena e Reggio Emilia, Viale Berengario 51, 41121 Modena, MO, Italy e-mail address: [email protected], Phone number: +39 059 205 6844 Acknowledgment A preliminary version of this paper was presented at the XXXIX Scientific Conference of Associazione Italiana di Scienze Regionali (AISRe) in Bolzano, Italy (17-19 September 2018). The authors would like to thank the discussant and the audience for the useful suggestions received. The authors also thank the editor and the anonymous referees for their precious suggestions that have led to a great improvement in the overall quality of the paper.