On the Rainfall Triggering of Phlegraean Fields Volcanic Tremors
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Documento Di Sintesi Torre Del Greco
Città di Torre del Greco DOS - Documento di Sintesi CITTA’ DI TOR R E DEL GR ECO PROVINCIA DI NAPOLI 4 A - AMBIENTE TERTERRITORIO R ITOR IO E INFRINFRASTRUTTURE ASTR UTTUR E UFFICIO “TEAM PROGETTO” COORDINATORE 4a AREA Sindaco Ing. Giovanni Salerno On.le Dott. Ciro Borriello Documento elaborato da: Assessore all’Urbanistica Arch. Michele Sannino Sig. Giuseppe Speranza PO FESR 2007- 2013 ProgrPr ogr amma Int egr at o UrbanoUr bano “Riqualificazione della zona portuale e connessioni con la struttura urbana” Documento di Orientamento Strategico Documento di sintesi e di avvio del processo Data: maggio/2008 Aggiornato Sostituisce l’allegato n. ELAB. ottobre/2008 Scala: N. 1 Sostituito dall’allegato n. DDD_464_Allegato_A Pagina 1 di 79 Città di Torre del Greco DOS - Documento di Sintesi CITTÀ DI TORRE DEL GRECO (PROVINCIA DI NAPOLI) 4a AREA AMBIENTE TERRITORIO E INFRASTUTTURE Ufficio “Team Progetto” PO FESR 2007-2013 Programma Integrato Urbano “Riqualificazione della zona portuale e connessioni con la struttura urbana” Documento di Orientamento Strategico Documento di sintesi e di avvio del processo Ottobre 2008 DDD_464_Allegato_A Pagina 2 di 79 Città di Torre del Greco DOS - Documento di Sintesi INDICE PREMESSA 1. ANALISI DI CONTESTO 1.1 Descrizione del contesto urbano 1.1.1 Caratteristiche generali del territorio 1.1.2 Rete dei trasporti 1.1.3 Patrimonio storico-architettonico ed ambientale 1.1.4 Aspetti demografici 1.1.5 Andamento socio-economico 1.2 Analisi SWOT 1.3 Conclusioni dell’analisi di contesto 2. CONTESTO DI RIFERIMENTO E STRUMENTI NORMATIVI 2.1 Contesto di riferimento 2.2 Regime urbanistico e vincolistico vigente 2.3 Strumenti di pianificazione sovracomunali 2.4 Programmazione regionale in materia di PIU’ 3. -
Resignations and Appointments
N. 210522b Saturday 22.05.2021 Resignations and Appointments Resignation and succession of metropolitan archbishop of Agrigento, Italy Appointment of metropolitan archbishop of Lubumbashi, Democratic Republic of the Congo Appointment of bishop of Ischia, Italy, and union in persona Episcopi of the dioceses of Pozzuoli and Ischia Appointment of auxiliary bishop of Busan, Korea Resignation and succession of metropolitan archbishop of Agrigento, Italy The Holy Father has accepted the resignation from the pastoral care of the metropolitan archdiocese of Agrigento, Italy, presented by His Eminence Cardinal Francesco Montenegro. He is succeeded by Archbishop Alessandro Damiano, until now coadjutor archbishop of the same archdiocese. Appointment of metropolitan archbishop of Lubumbashi, Democratic Republic of the Congo The Holy Father has appointed as metropolitan archbishop of Lubumbashi, Democratic Republic of the Congo, Bishop Fulgence Muteba Mugalu, transferring him from the diocese of Kilwa-Kasenga. Curriculum vitae Bishop Fulgence Muteba Mugalu was born on 9 July 1962 in the diocese of Kongolo, was ordained a priest on 5 August 1990 and appointed bishop of Kilwa-Kasenga on 18 March 2005. 2 After graduating in pastoral theology from the University of Montreal in Canada, he was professor of theology in Lubumbashi and at the Catholic University of Kinshasa; secretary of the Episcopal Commission for the Doctrine of the Faith of the National Episcopal Conference of Congo (CENCO) and later secretary general of the same Episcopal Conference. As a bishop he served as coordinator of the Inter-Diocesan Commission for Justice and Peace of the Ecclesiastical Province of Lubumbashi and president of the Episcopal Commission for the Doctrine of Faith of the CENCO. -
Multiple Sclerosis in the Campania Region (South Italy): Algorithm Validation and 2015–2017 Prevalence
International Journal of Environmental Research and Public Health Article Multiple Sclerosis in the Campania Region (South Italy): Algorithm Validation and 2015–2017 Prevalence Marcello Moccia 1,* , Vincenzo Brescia Morra 1, Roberta Lanzillo 1, Ilaria Loperto 2 , Roberta Giordana 3, Maria Grazia Fumo 4, Martina Petruzzo 1, Nicola Capasso 1, Maria Triassi 2, Maria Pia Sormani 5 and Raffaele Palladino 2,6 1 Multiple Sclerosis Clinical Care and Research Centre, Department of Neuroscience, Reproductive Science and Odontostomatology, Federico II University, Via Sergio Pansini 5, 80131 Naples, Italy; [email protected] (V.B.M.); [email protected] (R.L.); [email protected] (M.P.); [email protected] (N.C.) 2 Department of Public Health, Federico II University, 80131 Naples, Italy; [email protected] (I.L.); [email protected] (M.T.); raff[email protected] (R.P.) 3 Campania Region Healthcare System Commissioner Office, 80131 Naples, Italy; [email protected] 4 Regional Healthcare Society (So.Re.Sa), 80131 Naples, Italy; [email protected] 5 Biostatistics Unit, Department of Health Sciences, University of Genoa, 16121 Genoa, Italy; [email protected] 6 Department of Primary Care and Public Health, Imperial College, London SW7 2AZ, UK * Correspondence: [email protected] or [email protected]; Tel./Fax: +39-081-7462670 Received: 21 April 2020; Accepted: 12 May 2020; Published: 13 May 2020 Abstract: We aim to validate a case-finding algorithm to detect individuals with multiple sclerosis (MS) using routinely collected healthcare data, and to assess the prevalence of MS in the Campania Region (South Italy). To identify individuals with MS living in the Campania Region, we employed an algorithm using different routinely collected healthcare administrative databases (hospital discharges, drug prescriptions, outpatient consultations with payment exemptions), from 1 January 2015 to 31 December 2017. -
Human Responses to the 1906 Eruption of Vesuvius, Southern Italy
ÔØ ÅÒÙ×Ö ÔØ Human responses to the 1906 eruption of Vesuvius, southern Italy David Chester, Angus Duncan, Christopher Kilburn, Heather Sangster, Carmen Solana PII: S0377-0273(15)00061-X DOI: doi: 10.1016/j.jvolgeores.2015.03.004 Reference: VOLGEO 5503 To appear in: Journal of Volcanology and Geothermal Research Received date: 19 December 2014 Accepted date: 4 March 2015 Please cite this article as: Chester, David, Duncan, Angus, Kilburn, Christopher, Sangster, Heather, Solana, Carmen, Human responses to the 1906 eruption of Vesu- vius, southern Italy, Journal of Volcanology and Geothermal Research (2015), doi: 10.1016/j.jvolgeores.2015.03.004 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 March 3 2014 Human responses to the 1906 eruption of Vesuvius, southern Italy David Chestera,b, Angus Duncanb, Christopher Kilburnc, Heather Sangsterb and Carmen Solanad,e a Department of Geography and Environmental Science, Liverpool Hope University, Hope Park Liverpool L16 9JD, UK; bDepartment of Geography and Planning, University of Liverpool, Liverpool L69 3BX, UK; cAon Benfield UCL Hazard Research Centre, University College London, Gower Street, London WC1E 6BT, UK; dSchool of Earth and Environmental Sciences, University of Portsmouth, Portsmouth PO1 2UP; eInstituto Volcanológico de Canarias (INVOLCAN), Puerto de la Cruz, Canary Islands, Spain. -
131218 - OGS.Atti.32 Vol.3.27.Indd 175 04/11/13 10.39 GNGTS 2013 Sessione 3.3
GNGTS 2013 SES S IONE 3.3 MaRINE GEOLOGICAL MappING OF THE CaMpaNIA REGION at THE 1:10,000 SCALE: THE EXAMPLE OF THE GEOLOGICAL Map N. 465 “ISOLA DI PROCIDA” (NapLES BaY, SOUTHERN TYRRHENIAN SEA, ItaLY) G.Aiello Institute of Marine Environmental and Coastal Area (IAMC), National Research Council of Italy (CNR), Naples, Italy Introduction. Marine geological mapping of the Campania Region at the 1:10.000 scale is herein presented, focussing, in particular, on the geological map n. 465 “Isola di Procida” (Ispra, 2011). The geological map n. 465 “Isola di Procida” covers the Naples Bay from the Sorrento Peninsula up to the Procida island. In this geological map a total amount of 622 km2 of surface about 10 km2 are represented by emerged areas and 612 km2 by marine areas. The bathymetric belt 0/200 extends for 378 km2 and represents about the 60.8% of the total surface of the map. Sidescan sonar data have been calibrated by numerous sea bottom samples. The geological structures overlying the outcrop of acoustic basement, both carbonate (in correspondence to the Sorrento Peninsula) and volcanic (in correspondence to the Phlegrean Fields) have been investigated using Subbottom Chirp, Sparker and Watergun profiles. The interpretation of seismic data lends support for the reconstruction of the stratigraphic and structural setting of Quaternary continental shelf and slope successions and correlation to outcrops of acoustic basement, Mesozoic carbonate in the Sorrento Peninsula structural high and Quaternary volcanic in the Phlegrean Fields and Procida island. These areas result from the seaward prolongation of the stratigraphic and structural units widely cropping out in the surrounding emerged sector of the Sorrento Peninsula (Cinque et al., 1997), Naples town, Phlegrean Fields and Procida island (Scarpati et al., 1993; Perrotta et al., 2010; Ispra, 2011). -
Geomorphological Evolution of Phlegrean Volcanic Islands Near Naples, Southern Italy1
Berlin .Stuttgart Geomorphological evolution of Phlegrean volcanic islands near Naples, southern Italy1 by G.AIELLO, D.BARRA, T.DE PIPPO, C.DONADIO, and C.PETROSINO with 9 figures and 5 tables Summary. Using volcanological, morphological, palaeoecological and geoarchaeological data we reconstructed the complex evolution of the island volcanic system of Procida-Vivara, situated west of Naples betweenthe lsland of lschia and the PhlegreanFields, far the last 75 ky. Late Pleistocenemorphological evolution was chiefly controlled by a seriesof pyroclas tic eruptions that resulted in at least eight volcanic edifices, mainly under water. Probably the eruptive centresshifted progressively clockwise until about 18 ky BP when volcanic develop ment on the islands ceased. The presenceof stretches of marine terraces and traces of wave cut notches, both be low and abovè'current sea levels, the finding of exposed infralittoral rnicrofossils, and the identification of three palaeo-surfacesburied by palaeosoilsindicates at least three differen tial uplift phases.These phases interacted with postglacial eustaticfIuctuations, and were sep arated by at least two periods of generai stability in vertical movements. A final phase of ground stability, characterisedby the deposition of Phlegrean and lschia pyroclastics, start ed in the middle Holocene. Finally, fIattened surfacesand a sandy tombolo developedup to the present-day. Recent archaeological surveys and soil-borings at Procida confirm the presence of a lagoon followed by marshland at the back of a sandy tombolo that were formed after the last uplift between the Graeco-Roman periodandthe15di_16dicentury. These areaswere gradu ally filled with marine and continental sedimentsup to the 20di century. ' Finally, our investigation showed that the volcanic sector of Procida-Vivara in the late Pleistocene-Holocenewas affected by vertical displacementswhich were independent of and less marked than the concurrent movement in the adjacent sectors of lschia and of the Phle grean Fields. -
Summary of the Periodic Report on the State of Conservation, 2006
State of Conservation of World Heritage Properties in Europe SECTION II discovered, such as the Central Baths, the Suburban Baths, the College of the Priests of ITALY Augustus, the Palestra and the Theatre. The presence, in numerous houses, of furniture in carbonised wood due to the effects of the eruption Archaeological Areas of Pompei, is characteristic of Herculaneum. Hercolaneum and Torre The Villa of Poppea is preserved in exceptional way Annunziata and is one of the best examples of residential roman villa. The Villa of Cassius Tertius is one of Brief description the best examples of roman villa rustica. When Vesuvius erupted on 24 August A.D. 79, it As provided in ICOMOS evaluation engulfed the two flourishing Roman towns of Pompei and Herculaneum, as well as the many Qualities: Owing to their having been suddenly and wealthy villas in the area. These have been swiftly overwhelmed by debris from the eruption of progressively excavated and made accessible to Vesuvius in AD 79, the ruins of the two towns of the public since the mid-18th century. The vast Pompei and Herculaneum are unparalleled expanse of the commercial town of Pompei anywhere in the world for their completeness and contrasts with the smaller but better-preserved extent. They provide a vivid and comprehensive remains of the holiday resort of Herculaneum, while picture of Roman life at one precise moment in the superb wall paintings of the Villa Oplontis at time. Torre Annunziata give a vivid impression of the Recommendation: That this property be inscribed opulent lifestyle enjoyed by the wealthier citizens of on the World Heritage List on the basis of criteria the Early Roman Empire. -
GRADUATORIA SCORRIMENTO Cacciatori Non
ATC 2 POTENZA - ANNATA VENATORIA 2016 / 2017 - ELENCO DOMANDE REGOLARI DEI NON RESIDENTI COMPRESIVO DELLE ASSEGNAZIONI DEL MESE DI NOVEMBRE no. numero p. data cognome nome data nascita comune nascita comune residenza questura rilascio p. d'armi mesi settimane giornalieri ord d'armi compilazione 511 SPAGNUOLO VITTORIO 06/04/1942 AVELLINO (AV) AVELLINO (AV) AVELLINO 29/08/2014 750460 - N 19/02/2016 NOVEMBRE 512 SQUADRITTI RAFFAELE 17/04/1983 SUMMONTE (AV) SUMMONTE (AV) AVELLINO 29/07/2015 750335-N 22/02/2016 NOVEMBRE 513 TERMINIELLO LUIGI 19/08/1971 MASSA MASSA SORRENTO 24/07/2015 302573-O 03/02/2016 NOVEMBRE LUBRENSE (NA) LUBRENSE (NA) 514 TURCO MARIO 03/09/1966 TARANTO (TA) TARANTO (TA) TARANTO 25/11/2011 610264-N 22/02/2016 NOVEMBRE 515 VINCI ASTOLFO 14/05/1966 TORRE DEL TORRE DEL TORRE DEL 11/09/2010 392704-N 18/02/2016 NOVEMBRE GRECO (NA) GRECO (NA) GRECO 516 ACAMPORA MARIO 04/01/1971 AGEROLA (NA) AGEROLA (NA) in attesa rilascio 20/02/2016 NOVEMBRE 517 APA LEONARDO 24/10/1962 QUARTO (NA) QUARTO (NA) POZZUOLI 03/09/2013 186168-O 17/02/2016 NOVEMBRE 518 APICELLA ANIELLO 29/12/1970 CAVA DE' CAVA DE' CAVA DE' TIRRENI 15/07/2013 722250-N 23/02/2016 NOVEMBRE TIRRENI (SA) TIRRENI (SA) 519 APREDA ANTONINO 16/02/1973 VICO EQUENSE SANT'AGNELLO SORRENTO 26/09/2011 695066-N 23/02/2016 NOVEMBRE (NA) (NA) 520 ASCOLI MARIO 28/10/1956 SAN CIPRIANO SAN CIPRIANO SALERNO 15/10/2013 965315-N 22/02/2016 NOVEMBRE PICENTINO (SA) PICENTINO (SA) 521 ATTANASIO ANTONIO 25/12/1969 GRAGNANO (NA) SANTA MARIA LA CASTELLAMMARE 03/08/2011 693785 N 23/02/2016 NOVEMBRE -
High Resolution Seismic Reflection Survey in the Gulf of Pozzuoli
Geophysical Research Abstracts Vol. 12, EGU2010-11052-1, 2010 EGU General Assembly 2010 © Author(s) 2010 High resolution seismic reflection survey in the Gulf of Pozzuoli, Naples, Italy. An example of preliminary interpretation of seismic profiles. Elena D’Aniello (1), Vincenzo Di Fiore (2), Marco Sacchi (2), and Antonio Rapolla (1) (1) Department of Earth Science, University of Naples "Federico II", Naples, Italy. ([email protected]) , (2) Institute for Coastal Marine Environment - National Research Council, Naples, Italy During the cruise CAFE_07 – Leg 3 conducted in the Gulf of Naples and Pozzuoli in January 2008, on board of the R/V URANIA of the CNR it was carried out the acquisition of a grid of ca. 800 km of high-resolution multichannel reflection seismic profiles (Sacchi et al., 2009; Di Fiore et al., 2009). The aim of the cruise was the understanding of the stratigraphic-structural setting of the Pozzuoli Bay area, with specific reference to the major offshore volcanic features, such as Nisida Bank, Pentapalummo Bank, M.Dolce-Pampano Bank and Miseno Bank and others. The Gulf of Pozzuoli is placed in the Volcanic district of Campi Flegrei, an area of active volcanism located at North West of Naples city, along the Tyrrhenian margin, in an extensional collapsed area called Campanian Plain, filled by siliciclastic, epiclastic and volcaniclastic sediments, deposited during Late Pliocene and Quaternary. Several studies present in literature suggest a relation between volcanic system of Campi Flegrei and faults system; in particular, -
An Annotated List of Alien Marine Species of the Ischia Island (Gulf of Naples)
AN ANNOTATED LIST OF ALIEN MARINE SPECIES OF THE ISCHIA ISLAND (GULF OF NAPLES) This contribution was presented as a poster at the BioMarine Workshop “Management of Bioinvasions in the Mediterranean Sea - a way forward”, held on the island of Ischia on 4-5 May 2016, with the aim of updating the information and providing the workshop’s participants with a list of the alien taxa that have been recorded in the area hosting the meeting. The island of Ischia, and the nearby islands of Procida and Vivara (Phlaegrean islands), are located on the northern side of the Gulf of Naples, and are included within the Marine Protected Area of the “Regno di Nettuno” (“Neptune’s Realm”) since April 2008 (Gambi et al., 2003). The Phlaegrean islands are considered a biogeographic boundary which constitutes the distribution limit of most South Mediterranean thermophilous species, since the 14 °C minimum winter surface temperature isotherm (the 14 °C divide) is occurring between Ischia and the Pontine archipelago (e.g., Ventotene island) (Gambi et al., 2009; Gambi, 2014). In the past two decades, due to global warming also detected in the Mediterranean surface waters, we observed a northward shift of the 14° C divide, while the minimum winter isotherm in the area of the Phlaegrean islands is now often rising to the 15 °C divide. Therefore this zone is an interesting observatory for the distribution and migratory pattern of thermophilous species both native and introduced/aliens (Gambi, 2014). Occurrence and increase in the abundance of some native Mediterranean warm-species have been documented for this area (Dappiano and Gambi, 2004; Cigliano et al., 2007; Gambi, 2014), as for the coral Astroides calycularis (Pallas, 1776), the bryozoan Calpensia nobilis (Esper, 1796), and the fishes Sparisoma cretense (L., 1758), Sphoeroides pachygaster (Müller & Troschel, 1848) and Sphyraena viridensis Cuvier, 1829. -
Concorso Denza 2015 Inglese
City of Castellammare di Stabia Department of Culture and Education X INTERNATIONAL COMPETITION FOR YOUNG MUSICIANS Solisti: Piano - Bows - Wind instruments Canto - Guitar - Harp - Percussions - Accordion Chamber music: from duo to orchestra - Jazz Ancient music - Bands - Choirs Primary Schools - Middle Schools Musical Lyceums “LUIGI DENZA” Castellammare di Stabia Reggia di Quisisana May 11th – 16th 2015 Marcio CARNEIRO (President of the jury) Cello teacher at Lausanne Conservatory President of the Summer Courses at “T.Varga” Academy, Sion-Switzerland Concert of the Musicians of Teatro alla Scala Soloist: Francesco DE ANGELIS Saturday, May 16th 6 p.m. GIOVANNI SETARO EXPERT & CONSULTANT PH. +39 349 3713281 Prize Concerts: EMAIL: [email protected] [email protected] Italy- Switzerland - Germany-Greece Violin Prize: “Le Camenae Award” “SANTARPINO PIANOFORTI” Via Martiri d’Ungheria, 224, 84018 Scafati (SA) Bows Prize: “Innocente Lombardi Award” tel. 081 8567413 www.pianofortisantarpino.it Registrations by May 2nd, 2015 “ARCHETTAIO VINCENZO TREMATERRA” Info: Administrative Office Via Palestro, 26, 26100 Cremona Mon. to Fri. 3 p.m. to 8 p.m. tel. 0372 457597 Pompei: Tel. and fax 081 8504746 cell. 3382077572 [email protected] E-mail: [email protected] Web site: www.lecamenae.itw Medal of the Presidency of the Italian Republic Ministry of Foreign Affairs Italian Consulate of Wolfsburg-Germany Presidency of the European Parliament Campania Region Province of Naples City of Castellammare di Stabia M.I.U.R. U.S.R. – Campania Academy of Music “ T. Varga” Sion (Switzerland) Palamas Academy of Music (Greece) Cultural Centre for International Programs of Tobolsk (Russia) Patronage Package Tour Medal Upon request from the candidates and schools who arrive from outside the Region of the Presidency of the Italian Republic of Campania or from other countries and for reasons of logistics and organization participants and schools who require overnight accommodation are invited to Ministry of Foreign Affairs contact our reception representative. -
High Resolution Monitoring of Campi Flegrei (Naples, Italy) by Exploiting Terrasar-X Data: an Application to Solfatara Crater
HIGH RESOLUTION MONITORING OF CAMPI FLEGREI (NAPLES, ITALY) BY EXPLOITING TERRASAR-X DATA: AN APPLICATION TO SOLFATARA CRATER Christian Minet (1), Kanika Goel (1), Ida Aquino (2), Rosario Avino (2), Giovanna Berrino (2), Stefano Caliro (2), Giovanni Chiodini (2), Prospero De Martino (2), Carlo Del Gaudio (2), Ciro Ricco (2), Valeria Siniscalchi (2), Sven Borgstrom (2) (1)German Aerospace Center (DLR) IMF, Münchner Strasse 20, 82234 Wessling, Germany Email: [christian.minet, kanika.goel]@dlr.de (2)Istituto Nazionale di Geofisica e Vulcanologia, sezione di Napoli “Osservatorio Vesuviano” , via Diocleziano, 328, 80124 Naples, Italy Email: [email protected] ABSTRACT by continuous ground deformation (bradyseismic activity) related to its volcanic nature. Geodetic monitoring of Campi Flegrei caldera, west of In particular, we will focus on the Solfatara - Pisciarelli Naples (Italy), is carried out through integrated ground area, which is seat of strong fumarolic activity in the based networks and space-borne Differential InSAR last years. For this reason we also take into account (DInSAR) techniques, exploiting the SAR sensors some information from geochemical measurements. [3]. onboard ERS1-2 (till the end of their lifetime) and The geodetic monitoring of the area has been ENVISAT satellites. Unfortunately, C-band sensors historically carried out by the Osservatorio Vesuviano give no information when dealing with very low [4],[5],[6],[7], presently the Naples branch of the deformation rates and very small deforming areas. Istituto Nazionale di Geofisica e Vulcanologia To overcome these problems, we decided to use (INGV-OV) by ground based networks (levelling, TerraSAR-X from DLR, a high resolution SAR sensor EDM, gravity, tide-gauge, tiltmeter), shown in Fig.