Graziano Ferrari
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Journal Pre-proof From Historical Seismology to seismogenic source models, 20 years on: Excerpts from the Italian experience Gianluca Valensise, Paola Vannoli, Pierfrancesco Burrato, Umberto Fracassi PII: S0040-1951(19)30296-3 DOI: https://doi.org/10.1016/j.tecto.2019.228189 Reference: TECTO 228189 To appear in: Tectonophysics Received date: 1 April 2019 Revised date: 20 July 2019 Accepted date: 5 September 2019 Please cite this article as: G. Valensise, P. Vannoli, P. Burrato, et al., From Historical Seismology to seismogenic source models, 20 years on: Excerpts from the Italian experience, Tectonophysics(2019), https://doi.org/10.1016/j.tecto.2019.228189 This is a PDF file of an article that has undergone enhancements after acceptance, such as the addition of a cover page and metadata, and formatting for readability, but it is not yet the definitive version of record. This version will undergo additional copyediting, typesetting and review before it is published in its final form, but we are providing this version to give early visibility of the article. 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. © 2019 Published by Elsevier. Journal Pre-proof From Historical Seismology to seismogenic source models, 20 years on: excerpts from the Italian experience Gianluca Valensise, Paola Vannoli, Pierfrancesco Burrato & Umberto Fracassi Istituto Nazionale di Geofisica e Vulcanologia, Rome, Italy Contents 1. Introduction 1.1. Why Historical Seismology 1.2. A brief history of Historical Seismology 1.3. Representing and exploiting Historical Seismology data 2. -
Ferrara Di Ferrara
PROVINCIA COMUNE DI FERRARA DI FERRARA Visit Ferraraand its province United Nations Ferrara, City of Educational, Scientific and the Renaissance Cultural Organization and its Po Delta Parco Urbano G. Bassani Via R. Bacchelli A short history 2 Viale Orlando Furioso Living the city 3 A year of events CIMITERO The bicycle, queen of the roads DELLA CERTOSA Shopping and markets Cuisine Via Arianuova Viale Po Corso Ercole I d’Este ITINERARIES IN TOWN 6 CIMITERO EBRAICO THE MEDIAEVAL Parco Corso Porta Po CENTRE Via Ariosto Massari Piazzale C.so B. Rossetti Via Borso Stazione Via d.Corso Vigne Porta Mare ITINERARIES IN TOWN 20 Viale Cavour THE RENAISSANCE ADDITION Corso Ercole I d’Este Via Garibaldi ITINERARIES IN TOWN 32 RENAISSANCE Corso Giovecca RESIDENCES Piazza AND CHURCHES Trento e Trieste V. Mazzini ITINERARIES IN TOWN 40 Parco Darsena di San Paolo Pareschi WHERE THE RIVER Piazza Travaglio ONCE FLOWED Punta della ITINERARIES IN TOWN 46 Giovecca THE WALLS Via Cammello Po di Volano Via XX Settembre Via Bologna Porta VISIT THE PROVINCE 50 San Pietro Useful information 69 Chiesa di San Giorgio READER’S GUIDE Route indications Along with the Pedestrian Roadsigns sited in the Historic Centre, this booklet will guide the visitor through the most important areas of the The “MUSEO DI QUALITÀ“ city. is recognised by the Regional Emilia-Romagna The five themed routes are identified with different colour schemes. “Istituto per i Beni Artistici Culturali e Naturali” Please, check the opening hours and temporary closings on the The starting point for all these routes is the Tourist Information official Museums and Monuments schedule distributed by Office at the Estense Castle. -
Geochemical Monitoring of the 2012 Po Valley Seismic Sequence: a Review and Update
CHEMGE-18183; No of Pages 16 Chemical Geology xxx (2016) xxx–xxx Contents lists available at ScienceDirect Chemical Geology journal homepage: www.elsevier.com/locate/chemgeo Geochemical monitoring of the 2012 Po Valley seismic sequence: A review and update G. Martinelli a,⁎,A.Dadomob, F. Italiano c,R.Petrinid,F.F.Slejkoe a ARPAE Environmental Protection Agency, Emilia Romagna Region, 42100 Reggio Emilia, Italy b Geoinvest Srl, Piacenza, Italy c INGV Istituto Nazionale Geofisica Vulcanologia, Palermo, Italy d University of Pisa, Dept. Earth Sciences, Pisa, Italy e University of Trieste, Dept. Mathematics and Geosciences, Trieste, Italy article info abstract Article history: A seismic swarm characterized by a Ml = 5.9 mainshock occurred in the Po Valley, northern Italy, in 2012. The Received 15 July 2016 area has been studied for active compressional tectonics since the beginning of the twentieth century. A variety Received in revised form 24 November 2016 of geophysical and geochemical parameters have been utilized with the purpose of identifying possible precur- Accepted 2 December 2016 sory signals. This paper considers groundwater level data and geochemical data both in groundwaters and in Available online xxxx gases. All considered parameters have led to the conclusion that possible long and medium precursory trends have been identified in geofluids. No short-term precursors have been clearly identified. Hydrogeological and Keywords: Earthquake precursor geochemical monitoring could be more effectively utilized in a different geological context, and seismic hazard Earthquake effect reduction procedures could benefitfromgeofluid monitoring. Geofluid monitoring © 2016 Elsevier B.V. All rights reserved. Geochemical monitoring Emilia earthquake Po Valley 1. Introduction 2. -
On the Potential for Induced Seismicity at the Cavone Oilfield: Analysis of Geological and Geophysical Data, and Geomechanical Modeling
July, 2014 ON THE POTENTIAL FOR INDUCED SEISMICITY AT THE CAVONE OILFIELD: ANALYSIS OF GEOLOGICAL AND GEOPHYSICAL DATA, AND GEOMECHANICAL MODELING BY Luciana Astiz - University of California San Diego James H. Dieterich - University of California Riverside Cliff Frohlich - University of Texas at Austin Bradford H. Hager - Massachusetts Institute of Technology Ruben Juanes - Massachusetts Institute of Technology John H. Shaw –Harvard University 1 July, 2014 TABLE OF CONTENTS EXECUTIVE SUMMARY ……………………………………………………….... 5 INTRODUCTION ………………………………………………………………….9 1. TECTONIC FRAMEWORK OF THE EMILIA-ROMAGNA REGION .................... 11 1.1 SEISMOTECTONIC SETTING ............................................................................................................................ 11 1.1.1 HISTORICAL SEISMICITY IN THE EMILIA‐ROMAGNA REGION .................................................................... 12 1.2 CAVONE STRUCTURE ....................................................................................................................................... 19 1.3 GEOLOGIC EVIDENCE FOR TECTONIC ACTIVITY OF STRUCTURES IN THE FERRARESE‐ROMAGNOLO ARC ..................................................................................................................... 24 1.4 SEISMOTECTONIC ANALYSIS .......................................................................................................................... 26 1.5 GPS CONSTRAINTS ON TECTONICS — PRE‐EARTHQUAKE REGIONAL DEFORMATION RATES ............ 30 1.6 CONCLUSIONS OF -
The Earthquake of the 30 October 1930
1 The source of the 30 October 1930, Mw 5.8, Senigallia (central Italy) earthquake: a 2 convergent solution from instrumental, macroseismic and geological data 3 4 Paola Vannoli1*, Gianfranco Vannucci2, Fabrizio Bernardi1, Barbara Palombo1, Graziano Ferrari2 5 6 7 (1) Istituto Nazionale di Geofisica e Vulcanologia, sezione Roma 1, Via di Vigna Murata, 605, I- 8 00143, Rome, Italy 9 (2) Istituto Nazionale di Geofisica e Vulcanologia, sezione di Bologna, Via Donato Creti, 12, I- 10 40127, Bologna, Italy 11 12 * Corresponding author 13 14 15 Electronic Supplement collects methods, data and elaborations to make transparent the 16 seismotectonic characterization. In particular it provides a short description of the method used 17 for moment tensor computation, all the available focal mechanisms, the list of the available 18 stations, with specification of those used or not used for hypocenter and moment tensor 19 computation, maps of seismic flux showing areas of larger energy release, and detailed maps of 20 the uncertainties for each realization of the macroseismic epicenter. 21 22 1 23 Abstract 24 25 On 30 October 30 1930 a Mw 5.8 earthquake hit the northern Marche coastal area (central 26 Italy), causing significant damage (Io VIII-IX degree MCS) along a 40 km stretch of the Adriatic 27 coast between Pesaro and Ancona centered on the town of Senigallia. This area is characterized 28 by relatively infrequent and moderate-size earthquakes and by elusive active faults. In spite of 29 the presence of well-known NW-SE trending, NE verging fault-propagation folds forming the 30 outer thrusts of the Apennines, the current state of activity and the kinematics of these coastal 31 structures is still controversial. -
Catalog of Earthquakes, 2000 B.C.–1979, 1981
WORLD DATA CENTER A for Solid Earth Geophysics CATALOG OF SIGNIFICANT EARTHQUAKES 2000 B.C. - 1979 Including Quantitative Casualties and Damage July 1981 WORLD DATA CENTER A National Academy of Sciences 2101 Constitution Avenue, N.W. Washington, D.C., U.S.A., 20418 World Data Center A consists of the Coordination Office and seven Subcenters: World Data Center A Coordination Office National Academy of Sciences 2101 Constitution Avenue, N.W. Washington, D.C., U.S.A., 20418 [Telephone: (202) 389-6478] Gtaciology [Snow and Ice]: Rotation of the Earth: World Data Center A: Glaciology World Data Center A: Rotation [Snow and Ice] of the Earth Inst. of Arctic 6 Alpine Research U.S. Naval Observatory University of Colorado Washington, D.C., U.S.A. 20390 Boulder, Colorado, U.S.A. 80309 [Telephone: (202) 254-4023] [Telephone: (303) 492-5171] Solar-TerrestriaZ Physics (Solar and Meteorology (and NucZear Radiation) : Interplanetary Phenomena, Ionospheric Phenomena, Flare-Associated Events, World Data Center A: Meteorology Geomagnetic Variations, Magnetospheric National Climatic Center and Interplanetary Magnetic Phenomena, Federal Building Aurora, Cosmic Rays, Airglow): Asheville, North Carolina, U.S.A. 28801 [Telephone: (704) 258-2850] World Data Center A for Solar-Terrestrial Physics Oceanography : NOAA/EI)IS 325 Broadway World Data Center A: Oceanography Boulder, Colorado, U.S.A. 80303 National Oceanic and Atmospheric [Telephone: (303) 499-1000, Ext. 64671 Administration Washington, D.C., U.S.A. 20235 Solid-Earth Geophysics (Seismology, [Telephone: (262) 634-72491 Tsunamis, Gravimetry, Earth Tides, Recent Movements of the Earth's Rockets and SateZZites: Crust, Magnetic Measurements, Paleomagnetism and Archeomagnetism, World Data Center A: Rockets and Volcanology, Geothermics): Satellites Goddard Space Flight Center World Data Center A Code 601 for Solid-Earth Geophysics Greenbelt, Maryland, U.S.A. -
Pure and Applied Geophysics
Pure and Applied Geophysics The seismotectonics of the Po Plain (northern Italy): tectonic diversity in a blind faulting domain --Manuscript Draft-- Manuscript Number: PAAG-D-14-00070R1 Full Title: The seismotectonics of the Po Plain (northern Italy): tectonic diversity in a blind faulting domain Article Type: Report-Top.Vol. Crustal Fault Zones Keywords: Blind faulting; seismogenic source; active tectonics; seismic hazard; inherited faults; Po Plain. Corresponding Author: Paola Vannoli, Ph.D. Istituto Nazionale di Geofisica e Vulcanologia Roma, ITALY Corresponding Author Secondary Information: Corresponding Author's Institution: Istituto Nazionale di Geofisica e Vulcanologia Corresponding Author's Secondary Institution: First Author: Paola Vannoli, Ph.D. First Author Secondary Information: Order of Authors: Paola Vannoli, Ph.D. Pierfrancesco Burrato, M.D. Gianluca Valensise, Ph.D. Order of Authors Secondary Information: Abstract: We present a systematic and updated overview of a seismotectonic model for the Po Plain (northern Italy). This flat and apparently quiet tectonic domain is in fact rather active as it comprises the shortened foreland and foredeep of both the Southern Alps and the Northern Apennines. Assessing its seismic hazard is crucial due to the concentration of population, industrial activities and critical infrastructures, but it is also complicated because a) the region is geologically very diverse, and b) nearly all potential seismogenic faults are buried beneath a thick blanket of Pliocene-Pleistocene sediments, and hence can be investigated only indirectly. Identifying and parameterizing the potential seismogenic faults of the Po Plain requires proper consideration of their depth, geometry, kinematics, earthquake potential and location with respect to the two confronting orogens. To this end we subdivided them into four main homogeneous groups. -
On the Threshold of Poems: a Paratextual Approach to the Narrative/Lyric Opposition in Italian Renaissance Poetry
This is a repository copy of On the Threshold of Poems: a Paratextual Approach to the Narrative/Lyric Opposition in Italian Renaissance Poetry. White Rose Research Online URL for this paper: http://eprints.whiterose.ac.uk/119858/ Version: Accepted Version Book Section: Pich, F (2019) On the Threshold of Poems: a Paratextual Approach to the Narrative/Lyric Opposition in Italian Renaissance Poetry. In: Venturi, F, (ed.) Self-Commentary in Early Modern European Literature, 1400-1700. Intersections, 62 . Brill , pp. 99-134. ISBN 9789004346864 https://doi.org/10.1163/9789004396593_006 © Koninklijke Brill NV, Leiden, 2019. This is an author produced version of a paper published in Self-Commentary in Early Modern European Literature, 1400-1700 (Intersections). Uploaded in accordance with the publisher's self-archiving policy. Reuse Items deposited in White Rose Research Online are protected by copyright, with all rights reserved unless indicated otherwise. They may be downloaded and/or printed for private study, or other acts as permitted by national copyright laws. The publisher or other rights holders may allow further reproduction and re-use of the full text version. This is indicated by the licence information on the White Rose Research Online record for the item. Takedown If you consider content in White Rose Research Online to be in breach of UK law, please notify us by emailing [email protected] including the URL of the record and the reason for the withdrawal request. [email protected] https://eprints.whiterose.ac.uk/ 1 On the Threshold of Poems: a Paratextual Approach to the Narrative/Lyric Opposition in Italian Renaissance Poetry Federica Pich Summary This contribution focuses on the presence and function of prose rubrics in fifteenth- and sixteenth-century lyric collections. -
Relazione Geologica, Geomorfologica, Idrogeologica E
COMMITTENTE: PROGETTAZIONE: DIREZIONE TECNICA U.O. GEOLOGIA, GESTIONE TERRE E BONIFICHE PROGETTO DEFINITIVO ITINERARIO NAPOLI-BARI RADDOPPIO TRATTA CANCELLO – BENEVENTO II LOTTO FUNZIONALE FRASSO TELESINO – VITULANO 2° LOTTO FUNZIONALE TELESE – SAN LORENZO RELAZIONE GEOLOGICA, GEOMORFOLOGICA ED IDROGEOLOGICA SCALA: - COMMESSA LOTTO FASE ENTE TIPO DOC. OPERA/DISCIPLINA PROGR. REV. I F 0 H 2 2 D 6 9 R G G E 0 0 0 1 0 0 1 B X Rev. Descrizione Redatto Data Verificato Data Approvato Data Autorizzato Data A Emissione esecutiva S. Romano giu. 2017 A. Salvagnini giu. 2017 F. Cerrone giu. 2017 F. Marchese ott. 2017 S. Romano B Emissione esecutiva ott. 2017 A. Salvagnini ott. 2017 F. Cerrone ott. 2017 File: IF0H 22 D69 RG GE0001 001 B.docx n. Elab 2L 008 ITINERARIO NAPOLI-BARI RADDOPPIO TRATTA CANCELLO – BENEVENTO II LOTTO FUNZIONALE FRASSO TELESINO – VITULANO 2° LOTTO FUNZIONALE TELESE – SAN LORENZO COMMESSA LOTTO CODIFICA DOCUMENTO REV. FOGLIO RELAZIONE GEOLOGICA, GEOMORFOLOGICA ED IDROGEOLOGICA IF0H 22 D 69 RG GE 00 01 001 B 2 di 164 INDICE 1 PREMESSA .......................................................................................................................................................................... 6 2 SCOPO DEL DOCUMENTO ............................................................................................................................................... 6 3 DOCUMENTI DI RIFERIMENTO ..................................................................................................................................... -
Food, Culture and Politics at the Este Court of Ferrara - a Pseudoscientific Approach to Reigning
European Scientific Journal September 2014 /SPECIAL/ edition Vol.2 ISSN: 1857 – 7881 (Print) e - ISSN 1857- 7431 BETWEEN HISTORY AND LEGEND: FOOD, CULTURE AND POLITICS AT THE ESTE COURT OF FERRARA - A PSEUDOSCIENTIFIC APPROACH TO REIGNING. Andrea Guiati, PhD Distinguished Teaching Professor Director, Muriel A. Howard Honors Program Coordinator, Italian Section SUNY Buffalo State Abstract Gastronomy, by which I mean the pleasure and the luxury ofthe dinner table, was always a passion of the ambitious Este family. They were rulers of Ferrara from the beginning of the 13th to the end of the 16th centuries. The Estensi, as they were called, fancied fine clothes, elaborate ceremonies, beautiful art works and succulent food. Today's Ferraresi have adopted many of their customs and habits. If they can afford it, that is. The Este laid a splendid table. Famous chefs, such as Cristoforo Messibugo, whose name is still revered in culinary circles, spent their time inventing dishes for the many courses that typically made up one of these gargantuan feasts. And what a sparkling life was lived in those splendid times! When I grew up in Ferrara in the 1960s and early 1970s very few people seemed to remember the city‘s glorious past, the castle moat had become one of the favorite dumping grounds to rebellious teenagers who would throw in it outdoor bar furniture, bicycles and whatever else they found lying around late at night. The breathtaking castle was in need of repairs. Via delle Volte with its arches and cobblestones had become home to prostitutes and small-time thieves, the wall surrounding the city was crumbling down. -
Sandro Maragno Mille Anni
SANDRO MARAGNO MILLE ANNI Villa Litiza, una comunità dispersa dalla diversione del P o In copertina: Le colonne monolitiche di Villa Litiza - fotoelaborazione di Marco Maragno - MILLE ANNI Villa Litiza, una comunità dispersa dalla diversione del Po Di Sandro Maragno L’insediamento urbano di Polesella con la sua chiesa parrocchiale e le sue varie componenti di sistema, rappresenta il punto di arrivo di una sequenza di migrazioni di Ville, intese nell’accezione medievale di centro abitato 1, che ha avuto inizio nel XII secolo. Contestualmente o quasi anche i loro abitanti si sono trasferiti e sono state traslate le chiese plebane con le funzioni e i titoli. Il particolare processo evolutivo ha preso l’abbrivio in seguito alla Rotta di Ficarolo (detta talora anche del Sicardo), la rupta, registrata press’a poco verso la metà del XII secolo e i cui effetti principali furono compiutamente definiti solo nel XVI secolo, come esito anche del sisma del 1570. La sede pievana più antica si adattò alle fluttuazioni del popolamento spostandosi da un sito rimasto isolato in posizione periferica e paludosa ad uno in via di sviluppo, più protetto dalle esondazioni. L’effetto iniziale più evidente della diversione dell’alveo del Po fu l’accumulo di sedimenti fluviali con la formazione di nuove quote altimetriche sopraelevate rispetto al territorio circostante. In conseguenza si accrebbero le garanzie di permanenza stabile nell’area così privilegiata, con la crescita di nuovi interessi economici e politici. E’ il risultato della continua ricerca di un luogo sicuro dagli effetti estremi degli sconvolgimenti provocati dalla natura sul fondovalle padano. -
Deliverable 5
NEtwork of Research Infrastructures for European Seismology Deliverable D5 The European Earthquake Catalogue (1000-1600), demo version Part 1 – The NA4 Calibration Initiative (april 2009) Activity: Distributed Archive of Historical Earthquake Data Activity number: NA4 Deliverable: The Europena Earthquake Catalogue (1000- 1600), demo version. Part 1, The NA4 Calibration Initiative Deliverable number: D5 Responsible activity leader: Massimiliano Stucchi Responsible participant: INGV Author: A.A. Gomez Capera, C. Meletti, R. Musson and M. Stucchi with the collaboration of S. Alvarez Rubio, J. Batllo, A. Cassera, V. D’Amico, D. Faeh, M. Locati, C. Mirto, C. Papaioannou, A. Rovida, C. Ventouzi, P. Gasperini, O. Scotti and D. Giardini reviewed by W. Bakun, june 2009 Sixth Framework Programme EC project number: 026130 NA4 Distributed Archive of Historical Earthquake Data Index 0. Introduction 1. Methods and software 2. Calibration: input data 3. Calibration: procedures and results 4. Validation: data 5. Validation: procedures and results 6. Conclusion References Review by W. Bakun Tables A to F Annexes 1 to 6 Abstract The aim of this initiative was to calibrate, in a homogeneous way, three methods for determining earthquake parameters from macroseismic data, Boxer, Meep, Bakun & Wentworth, in five European areas: Aegean, Iberian, Italian, Great Britain and Switzerland. For each area a dataset of about fifteen earthquakes of the 20th century, selected to cover the largest magnitude range, was compiled according to homogeneous procedures. The Boxer and Meep methods are accompanied by codes which provide calibrated coefficients from the input dataset. The Bakun & Wentworth method requires an intensity attenuation relation as function of the moment magnitude and hypocentral distance.