Fucino Basin, Central Italy)
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FUCINO2015PROGRAMME.Pdf
Organizing Committee Anna Maria Blumetti (ISPRA) Francesca Romana Cinti (INGV) Paolo Marco De Martini (INGV) Fabrizio Galadini (INGV) Luca Guerrieri (ISPRA) Alessandro Maria Michetti (Univ. degli Studi dell’Insubria) Daniela Pantosti (INGV) Eutizio Vittori (ISPRA) Marco De Nicola (Comune di Pescina) Dear Participants, welcome to Fucino 2015! Scientific Committee As mayor of Pescina, and also on behalf of the 1915-2015 Pescina Committee Alfonsi L., Amit R., Audemard F., Baize S., Boncio P., Bosi C., Comerci V., Costa C., Doglioni C., Galli P., I am very honoured to host this international workshop in our small town. Grutzner C., Hinzen K., Karakhanian A., Kim Y.S., Livio F., Masana E., Mc Calpin J., Messina P., Okumura K., Papanikolaou I., Perez Lopez R., Piccardi L., Porfido S., Reicherter K., Roberts G., Rockwell T., Saroli M., We are in the epicentral area of the 1915 Fucino earthquake: this event was a Schwartz D., Scotti O., Serva L., Silva P.G., Smedile A., Szczucinski W., Tatevossian R. and Villani F. catastrophe for Pescina and other surrounding villages that changed our history for ever with a remarkable social impact. Acknowledgements: One hundreds years later we wish to keep the memory of such a tragic event.Thus, Sara Amoroso, Filippo Bernardini, Riccardo Civico, Laura Graziani, Francesco Potenza, we are very glad to promote this workshop as an action for sharing and discussing Stefano Pucci, Andrea Tertulliani, Giacomo Tironi, Federica Innocenzi, Anna Maria Mattei, Gianna Naruli, Donatella Provenza, Rita Uncini, Sabina Vallati, Anna Maria Valvona (INGV), Francesca Ferrario, the most recent scientific developments in the seismic hazard assessment. -
Travelling to Naples: Drawings and Views by Robert Adam’, the Georgian Group Journal, Vol
Maria Celesta Cola, ‘Travelling to Naples: drawings and views by Robert Adam’, The Georgian Group Journal, Vol. XXV, 2017, pp. 151–166 TEXT © THE AUTHORS 2017 TRAVELLING TO NAPLES: DrawingS AND ViewS BY RObert ADAM MARIA CELESTE COLA The journey to Naples was an essential part of the the ruins was a wonderful opportunity to review programme of study and experience for all young preconceived ideas and to experiment with new artists living in Rome in the mid eighteenth century. models.3 The foremost aim of his trip to Italy was For Robert Adam, exposure to the archaeological to gather as many drawings as possible in order to remains there brought a deeper understanding of create a documentary ‘archive museum’ on his return the ancient buildings he had seen and recorded in to England, sparked by his desire to go beyond the Rome, and served to stimulate his development as a beaten paths of the Grand Tourists. He spent three Neoclassical architect. This article aims to re-create, years in Rome, from 1755 to 1757, accumulating a through his many drawings and views, the journey he store of knowledge and making sketches, but Italy took from Rome to Naples in the company of Charles- boasted several other important artistic centers. Louis Clérisseau, and his interest in the antiquities He had already visited Florence in 1755, where, in shared with other British and French artists. the home of Ignazio Hugford, he had met Charles- Louis Clérisseau. That experience influenced obert Adam’s journey to Rome in April everything that followed in his career. -
War and Society in the Roman World
Leicester-Nottingham Studies in Ancient Society Volume 5 WAR AND SOCIETY IN THE ROMAN WORLD WAR AND SOCIETY IN THE ROMAN WORLD Edited by JOHN RICH and GRAHAM SHIPLEY London and New York First published 1993 by Routledge 11 New Fetter Lane, London EC4P 4EE This edition published in the Taylor & Francis e-Library, 2002. Simultaneously published in the USA and Canada by Routledge Inc. 29 West 35th Street, New York, NY 10001 © 1993 John Rich, Graham Shipley and individual contributors All rights reserved. No part of this book may be reprinted or reproduced or utilized in any form or by any electronic, mechanical, or other means, now known or hereafter invented, including photocopying and recording, or in any information storage or retrieval system, without permission in writing from the publishers. British Library Cataloguing in Publication Data A catalogue record for this book is available from the British Library. Library of Congress Cataloging in Publication Data War and society in the Roman world/edited by John Rich and Graham Shipley. p. cm.—(Leicester-Nottingham studies in ancient society; v. 5) Selected, revised versions of papers from a series of seminars sponsored by the Classics Departments of Leicester and Nottingham Universities, 1988–1990. Includes bibliographical references and index. 1. Military art and science—Rome—History. 2. Rome—History, Military. 3. Sociology, Military—Rome—History. I. Rich, John. II. Shipley, Graham. III. Series. U35.W34 1993 355′.00937–dc20 92–36698 ISBN 0-203-07554-4 Master e-book ISBN ISBN 0-203-22120-6 -
The April 2009 L'aquila Earthquake: a Retrospective Discussion On
The April 2009 L’Aquila earthquake: a retrospective discussion on scientific knowledge Istituto Nazionale di Geofisica e Vulcanologia INGV ‐ processoaquila.wordpress.com Outlines 1 What we knew and we did in the years preceding the earthquake 2 What we knew and we did in the months preceding the earthquake 3 What happened between March 29th and April 5th 2009 4 April 6th earthquake: which improvements are needed 5 Forethoughts on the verdict INGV ‐ processoaquila.wordpress.com What we knew in the years preceding the 1 earthquake Seismic hazard for the region (Hazard Map updated in 2004 Historical seismicity and active strain indicate high earthquake potential Probability of occurrence of a M 5+ earthquake was relatively high (≈10-15%) Vulnerability of several building and historical heritage in L’Aquila city was known [GNDT-LSU, 1999; SIGOIS, 2006]. Amato e Ciaccio 2012 Censimento di vulnerabilità degli edifici pubblici strategici e speciali nelle regioni Abruzzo, Basilicata, Calabria, Campania, Molise, Puglia e Sicilia Orientale. There were several seismic sequences in the area with main shocks M≅4 not followed by any destructive event (i.e., 1985) INGV ‐ processoaquila.wordpress.com The seismic hazard Map 1 The seismic hazard map of Italy (2004) L’Aquila has been classified as an high seismic hazard region after the 1915 Avezzano earthquake. All the houses built after that date should take into account the seismic code. INGV ‐ processoaquila.wordpress.com Medium-long term probability models of 1 occurence of a M>5 earthquake Different models [Pace et al., 2006; Faenza et al., 2003; Cinti et al., 2006] gave a probability of occurrence of about 10%-15% in 10- 50 years Seismogenic region used in the probability evaluations (dark colors are higher probability. -
Quaternary Geology and Paleoseismology in the Fucino and L’Aquila Basins
Geological Field Trips Società Geologica Italiana 2016 Vol. 8 (1.2) ISPRA Istituto Superiore per la Protezione e la Ricerca Ambientale SERVIZIO GEOLOGICO D’ITALIA Organo Cartografico dello Stato (legge N°68 del 2-2-1960) Dipartimento Difesa del Suolo ISSN: 2038-4947 Quaternary geology and paleoseismology in the Fucino and L’Aquila basins 6th INQUA International Workshop on Active Tectonics Paleoseismology and Archaeoseismology Pescina (AQ) - Italy DOI: 10.3301/GFT.2016.02 Quaternary geology and paleoseismology in the Fucino and L’Aquila basins S. Amoroso-F. Bernardini-A.M. Blumetti-R. Civico-C. Doglioni-F. Galadini-P. Galli-L. Graziani-L. Guerrieri-P. Messina-A.M. Michetti-F. Potenza-S. Pucci-G. Roberts-L. Serva-A. Smedile-L. Smeraglia-A. Tertulliani-G. Tironi-F. Villani-E. Vittori GFT - Geological Field Trips geological fieldtrips2016-8(1.2) Periodico semestrale del Servizio Geologico d'Italia - ISPRA e della Società Geologica Italiana Geol.F.Trips, Vol. 8 No.1.2 (2016), 88 pp., 79 figs, 1 tab. (DOI 10.3301/GFT.2016.02) Quaternary geology and Paleoseismology in the Fucino and L’Aquila basins 6th INQUA, 19-24 April 2015, Pescina (AQ) - Fucino basin Sara Amoroso1, Filippo Bernardini2, Anna Maria Blumetti3, Riccardo Civico4, Carlo Doglioni5, Fabrizio Galadini1, Paolo Galli6, Laura Graziani4, Luca Guerrieri3, Paolo Messina7, Alessandro Maria Michetti8, Francesco Potenza9, Stefano Pucci4, Gerald Roberts10, Leonello Serva11, Alessandra Smedile1, Luca Smeraglia5, Andrea Tertulliani4, Giacomo Tironi12, Fabio Villani1, Eutizio Vittori3 1 INGV, L’Aquila. 2 INGV, Bologna. 3 ISPRA, Rome. 4 INGV, Rome. 5 Dip. Sc. della Terra, Univ. “La Sapienza”, Rome. 6 Dip. -
Seismological Database Methodological Approach
H4.SMR/1645-1 "2nd Workshop on Earthquake Engineering for Nuclear Facilities: Uncertainties in Seismic Hazard" 14 - 25 February 2005 Seismological Database Methodological Approach G.F. Panza1, 2 1 Department of Earth Sciences University of Trieste 2 ICTP SAND Group, Trieste Engineering Geology 66 (2002) 315–317 www.elsevier.com/locate/enggeo Opinion paper PSHA: is it science? Heriberta Castan˜os a, Cinna Lomnitz b,* aInstituto de Investigaciones Econo´micas, National University of Mexico, Mexico bInstituto de Geofı´sica, National University of Mexico (UNAM), 04510 D.F., Mexico Accepted 18 February 2002 Abstract Probabilistic seismic hazard analysis (PSHA) is beginning to be seen as unreliable. The problem with PSHA is that its data are inadequate and its logic is defective. Much more reliable, and more scientific, are deterministic procedures, especially when coupled with engineering judgment. D 2002 Elsevier Science B.V. All rights reserved. Keywords: Probabilistic seismic hazard analysis; Deterministic seismic hazard analysis; Earthquakes 1. Introduction what extent are these results based on sound science? Should earthquake hazard be assumed as high in First it was the turn of earthquake prediction. Memphis as it is in San Francisco, and where does Not that it was all that unscientific. True, the probability come in? The criterion of ‘‘2% in 50 years’’ science in earthquake prediction might have fitted has been sanctioned by the International Code Council into Peter Potter’s cocked hat, and there were all the (2000) as being realistic for the central United States. jokes about Chinese cookies and Parkfield capers Why 50 years? Is it conservative or the opposite? making the rounds among seismologists (Lomnitz, People are beginning to wonder, ‘‘Is this science?’’ 1994). -
Basin and Range Province Seismic Hazards Summit III Invited Paper
Basin and Range Province Seismic Hazards Summit III Utah Geological Survey and Western States Seismic Policy Council Invited Paper Guide to Luminescence Dating Techniques and Their Application for Paleoseismic Research: Harrison J. Gray, Shannon A. Mahan, Tammy Rittenour, and Michelle S. Nelson Utah Geological Survey GUIDE TO LUMINESCENCE DATING TECHNIQUES AND THEIR APPLICATION FOR PALEOSEISMIC RESEARCH Harrison J. Gray 1, 2*, Shannon A. Mahan 1, Tammy Rittenour 3, 4, and Michelle S. Nelson 3 1 U.S. Geological Survey, Luminescence Geochronology Laboratory, Denver, Colorado 2 Cooperative Institute for Research in Environmental Sciences, University of Colorado, Boulder, Colorado 3 USU Luminescence Laboratory, Utah State University, Logan, Utah 4 Department of Geology, Utah State University, Logan, Utah Senior author’s email [email protected] ABSTRACT Over the past 25 years, luminescence dating has become a key tool for dating sediments of interest in paleoseismic research. The data obtained from luminescence dating has been used to determine timing of fault displacement, calculate slip rates, and estimate earthquake recurrence intervals. The flexibility of luminescence is a key complement to other chronometers such as radiocarbon or cosmogenic nuclides. Careful sampling and correct selection of sample sites exert two of the strongest controls on obtaining an accurate luminescence age. Factors such as partial bleaching and post-depositional mixing should be avoided during sampling and special measures may be needed to help correct for associated problems. Like all geochronologic techniques, context is necessary for interpreting and calculating luminescence results and this can be achieved by supplying participating labs with associated trench logs, photos, and stratigraphic locations of sample sites. -
The Holocene Paleoearthquakes on the 1915 Avezzano Earthquake Faults (Central Italy): Implications for Active Tectonics in the Central Apennines
ELSEVIER Tectonophysics 308 (1999) 143±170 www.elsevier.com/locate/tecto The Holocene paleoearthquakes on the 1915 Avezzano earthquake faults (central Italy): implications for active tectonics in the central Apennines F. Galadini a,Ł,P.Gallib a CNR, Istituto di Ricerca sulla Tettonica Recente, Area di Ricerca di Roma-Tor Vergata, via del Fosso del Cavaliere, 00133 Rome, Italy b Servizio Sismico Nazionale, via Curtatone 3, 00185 Rome, Italy Received 4 October 1998; accepted 27 November 1998 Abstract Extensive paleoseismological research was conducted in the Fucino Plain (central Italy) in order to better understand the seismogenic characteristics of the fault responsible for the 1915 Avezzano earthquake .Ms D 7:0/ and improve the general knowledge regarding active tectonics in the central Apennines. Evidence for Late Pleistocene±Holocene surface faulting events was obtained through the study of thirteen sites across four different fault branches. The paleoseismological analysis outlined the occurrence of ten surface faulting events in the past 33,000 years, seven of which occurred during the Holocene. Radiocarbon, thermoluminescence and archaeological dating permitted the de®nition of an event chronology and the estimation of a recurrence interval for surface faulting events ranging between 1400 and 2600 years. On the basis of the observed offsets it was possible to calculate vertical slip rates for the individual fault branches, ranging between 0.24 mm yr1 and 0.5 mm yr1 and an extension rate across the Fucino Plain ranging between 0.6 and 1 mm yr1. The chronology of surface faulting events appears linearly distributed in time, and the observed recurrence times are similar to those inferred by other paleoseismological studies along different active Apennine faults. -
University Microfilms International 300 N
INFORMATION TO USERS This reproduction was made from a copy of a document sent to us for microfilming. While the most advanced technology has been used to photograph and reproduce this document, the quality of the reproduction is heavily dependent upon the quality of the material submitted. The following explanation of techniques is provided to help clarify markings or notations which may appear on this reproduction. 1.The sign or “target” for pages apparently lacking from the document photographed is “Missing Page(s)”. If it was possible to obtain the missing page(s) or section, they are spliced into the film along with adjacent pages. This may have necessitated cutting through an image and duplicating adjacent pages to assure complete continuity. 2. When an image on the film is obliterated with a round black mark, it is an indication of either blurred copy because of movement during exposure, duplicate copy, or copyrighted materials that should not have been filmed. For blurred pages, a good image of the page can be found in the adjacent frame. If copyrighted materials were deleted, a target note will appear listing the pages in the adjacent frame. 3. When a map, drawing or chart, etc., is part of the material being photographed, a definite method of “sectioning” the material has been followed. It is customary to begin filming at the upper left hand comer of a large sheet and to continue from left to right in equal sections with small overlaps. If necessary, sectioning is continued again—beginning below the first row and continuing on until complete. -
IAEA TECDOC SERIES the Contribution of Palaeoseismology to Seismic Hazard for Nuclearassessment in Site Evaluation Installations
208 pgs = 10.81 mm IAEA-TECDOC-1767 IAEA-TECDOC-1767 IAEA TECDOC SERIES The Contribution of Palaeoseismology to Seismic Hazard Assessment in Site Evaluation for Nuclear Installations Assessment in Site Evaluation for Nuclear to Seismic Hazard The Contribution of Palaeoseismology IAEA-TECDOC-1767 The Contribution of Palaeoseismology to Seismic Hazard Assessment in Site Evaluation for Nuclear Installations International Atomic Energy Agency Vienna ISBN 978–92–0–105415–9 ISSN 1011–4289 @ IAEA SAFETY STANDARDS AND RELATED PUBLICATIONS IAEA SAFETY STANDARDS Under the terms of Article III of its Statute, the IAEA is authorized to establish or adopt standards of safety for protection of health and minimization of danger to life and property, and to provide for the application of these standards. The publications by means of which the IAEA establishes standards are issued in the IAEA Safety Standards Series. This series covers nuclear safety, radiation safety, transport safety and waste safety. The publication categories in the series are Safety Fundamentals, Safety Requirements and Safety Guides. Information on the IAEAs safety standards programme is available at the IAEA Internet site http://www-ns.iaea.org/standards/ The site provides the texts in English of published and draft safety standards. The texts of safety standards issued in Arabic, Chinese, French, Russian and Spanish, the IAEA Safety Glossary and a status report for safety standards under development are also available. For further information, please contact the IAEA at PO Box 100, 1400 Vienna, Austria. All users of IAEA safety standards are invited to inform the IAEA of experience in their use (e.g. -
Analysis of Geological, Seismological and Gravimetric Data for the Identification of Active Faults in Abruzzo Area (Central Italy) P
GNGTS 2015 SESSIONE 1.2 ANALYSIS OF GEOLOGICAL, SEISMOLOGICAL AND GRAVIMETRIC DATA FOR THE IDENTIFICATION OF ACTIVE FAULTS IN ABRUZZO AREA (CENTRAL ITALY) P. Luiso1, V. Paoletti1, G. Gaudiosi2, R. Nappi2, F. Cella3, M. Fedi1 1 Dipartimento di Scienze della Terra, Università degli Studi «Federico II», Napoli, Italy 2 Istituto Nazionale di Geofisica e Vulcanologia, Sezione OV, Napoli, Italy 3 Dipartimento di Scienze della Terra, Università degli Studi della Calabria, Arcavacata di Rende (CS), Italy Introduction. The aim of the study is to identify and better constrain the geometry of the seismogenic structures (active,active, outcroppingoutcroppingand andburied buriedfault faultsystemssystems)) ininin thethethe AbruzzoAbruzzoAbruzzo areaareaarea (central Italy), through an integratedintegrated analysis of geo-structural,geo-structural, seismicseismicseismic andandand gravimetricgravimetricgravimetric data.data.data. The studied area is one of the most active zones from a geodynamic point of view of the Italian Apennines, characterized by the occurrence of intense and widely spread seismic activity. The integrated analysis of structural, seismic and gravimetric data (Gaudiosi et al., 2012) of the areas was carried out through the use of Geographic Information System (GIS). 107 GNGTS 2015 SESSIONE 1.2 More specifically, the analysis consisted of the following main steps: (a) collection and acquisition of aerial photos, numeric cartography, Digital Terrain Model (DTM) data, geological and geophysical data; (b) generation of the vector cartographic database and alpha-numerical data; c) image processing and features classification; d) cartographic restitution and multi- layers representation. Three thematic data sets have been generated: “faults”, “earthquakes” and “gravimetric” data. The fault dataset was built by merging all Plio- Quaternary structural data extracted from the available structural and geological maps, and many geological studies (Boncio et al., 2004; Galadini et al., 2000, 2003; Falcucci et al., 2011; Moro et al., 2013). -
An Economic History of Rome Second Edition Revised
An Economic History of Rome Second Edition Revised Tenney Frank Batoche Books Kitchener 2004 Originally published in 1927. This edition published 2004 Batoche Books Limited [email protected] Contents Preface ...........................................................................................................................5 Chapter 1: Agriculture in Early Latium.........................................................................6 Chapter 2: The Early Trade of Latium and Etruria .....................................................14 Chapter 3: The Rise of the Peasantry ..........................................................................26 Chapter 4: New Lands For Old ...................................................................................34 Chapter 5: Roman Coinage .........................................................................................41 Chapter 6: The Establishment of the Plantation..........................................................52 Chapter 7: Industry and Commerce ............................................................................61 Chapter 8: The Gracchan Revolution..........................................................................71 Chapter 9: The New Provincial Policy........................................................................78 Chapter 10: Financial Interests in Politics ..................................................................90 Chapter 11: Public Finances......................................................................................101