The Phlegrean Fields
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The Rough Guide to Naples & the Amalfi Coast
HEK=> =K?:;I J>;HEK=>=K?:;je CVeaZh i]Z6bVaÒ8dVhi D7FB;IJ>;7C7B<?9E7IJ 7ZcZkZcid BdcYgV\dcZ 8{ejV HVc<^dg\^d 8VhZgiV HVciÉ6\ViV YZaHVcc^d YZ^<di^ HVciVBVg^V 8{ejVKiZgZ 8VhiZaKdaijgcd 8VhVaY^ Eg^cX^eZ 6g^Zcod / AV\dY^EVig^V BVg^\a^Vcd 6kZaa^cd 9WfeZ_Y^_de CdaV 8jbV CVeaZh AV\dY^;jhVgd Edoojda^ BiKZhjk^jh BZgXVidHVcHZkZg^cd EgX^YV :gXdaVcd Fecf[__ >hX]^V EdbeZ^ >hX]^V IdggZ6ccjco^ViV 8VhiZaaVbbVgZY^HiVW^V 7Vnd[CVeaZh GVkZaad HdggZcid Edh^iVcd HVaZgcd 6bVa[^ 8{eg^ <ja[d[HVaZgcd 6cVX{eg^ 8{eg^ CVeaZh I]Z8Vbe^;aZ\gZ^ Hdji]d[CVeaZh I]Z6bVa[^8dVhi I]Z^haVcYh LN Cdgi]d[CVeaZh FW[ijkc About this book Rough Guides are designed to be good to read and easy to use. The book is divided into the following sections, and you should be able to find whatever you need in one of them. The introductory colour section is designed to give you a feel for Naples and the Amalfi Coast, suggesting when to go and what not to miss, and includes a full list of contents. Then comes basics, for pre-departure information and other practicalities. The guide chapters cover the region in depth, each starting with a highlights panel, introduction and a map to help you plan your route. Contexts fills you in on history, books and film while individual colour sections introduce Neapolitan cuisine and performance. Language gives you an extensive menu reader and enough Italian to get by. 9 781843 537144 ISBN 978-1-84353-714-4 The book concludes with all the small print, including details of how to send in updates and corrections, and a comprehensive index. -
F. Pingue , G.. De Natale , , P. Capuano , P. De , U
Ground deformation analysis at Campi Flegrei (Southern Italy) by CGPS and tide-gauge network F. Pingue1, G.. De Natale1, F. Obrizzo1, C. Troise1, P. Capuano2, P. De Martino1, U. Tammaro1 1 Istituto Nazionale di Geofisica e Vulcanologia . Osservatorio Vesuviano, Napoli, Italy 2 Dipartimento di Matematica e Informatica, Università di Salerno, Italy CGPS CAMPI FLEGREI NETWORK TIDE GAUGES ABSTRACT GROUND DEFORMATION HISTORY CGPS data analysis, during last decade, allowed continuous and accurate The vertical ground displacements at Campi Flegrei are also tracked by the sea level using tide gauges located at the Campi Flegrei caldera is located 15 km west of the Campi Flegrei, a caldera characterized by high volcanic risk due to tracking of ground deformation affecting Campi Flegrei area, both for Nisida (NISI), Port of Pozzuoli (POPT), Pozzuoli South- Pier (POPT) and Miseno (MISE), in addition to the reference city of Naples, within the central-southern sector of a the explosivity of the eruptions and to the intense urbanization of the vertical component (also monitored continuously by tide gauge and one (NAPT), located in the Port of Naples. The data allowed to monitor all phases of Campi Flegrei bradyseism since large graben called Campanian Plain. It is an active the surrounding area, has been the site of significant unrest for the periodically by levelling surveys) and for the planimetric components, 1970's, providing results consistent with those obtained by geometric levelling, and more recently, by the CGPS network. volcanic area marked by a quasi-circular caldera past 2000 years (Dvorak and Mastrolorenzo, 1991). More recently, providing a 3D displacement field, allowing to better constrain the The data have been analyzed in the frequency domain and the local astronomical components have been defined by depression, formed by a huge ignimbritic eruption the caldera floor was raised to about 1.7 meters between 1968 and inflation/deflation sources responsible for ground movements. -
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. -
New Seismo-Stratigraphic and Marine Magnetic Data of the Gulf Of
New seismo-stratigraphic and marine magnetic data of the Gulf of Pozzuoli (Naples Bay, Tyrrhenian Sea, Italy): inferences for the tectonic and magmatic events of the Phlegrean Fields volcanic complex (Campania) Gemma Aiello, Ennio Marsella & Vincenzo Di Fiore Marine Geophysical Research An International Journal for the Study of the Earth Beneath the Sea ISSN 0025-3235 Mar Geophys Res DOI 10.1007/s11001-012-9150-8 1 23 Your article is protected by copyright and all rights are held exclusively by Springer Science+Business Media B.V.. This e-offprint is for personal use only and shall not be self- archived in electronic repositories. If you wish to self-archive your work, please use the accepted author’s version for posting to your own website or your institution’s repository. You may further deposit the accepted author’s version on a funder’s repository at a funder’s request, provided it is not made publicly available until 12 months after publication. 1 23 Author's personal copy Mar Geophys Res DOI 10.1007/s11001-012-9150-8 ORIGINAL RESEARCH PAPER New seismo-stratigraphic and marine magnetic data of the Gulf of Pozzuoli (Naples Bay, Tyrrhenian Sea, Italy): inferences for the tectonic and magmatic events of the Phlegrean Fields volcanic complex (Campania) Gemma Aiello • Ennio Marsella • Vincenzo Di Fiore Received: 13 December 2011 / Accepted: 4 April 2012 Ó Springer Science+Business Media B.V. 2012 Abstract A detailed reconstruction of the stratigraphic emplacement of the Neapolitan Yellow Tuff deposits. A and tectonic setting of the Gulf of Pozzuoli (Naples Bay) is thick volcanic unit, exposed over a large area off the Capo provided on the basis of newly acquired single channel Miseno volcanic edifice is connected with the Bacoli-Isola seismic profiles coupled with already recorded marine Pennata-Capo Miseno yellow tuffs, cropping out in the magnetics gathering the volcanic nature of some seismic northern Phlegrean Fields. -
Boccaccio Angioino Materiali Per La Storia Culturale Di Napoli Nel Trecento
Giancarlo Alfano, Teresa D'Urso e Alessandra Perriccioli Saggese (a cura di) Boccaccio angioino Materiali per la storia culturale di Napoli nel Trecento Destini Incrociati n° 7 5 1-6.p65 5 19/03/2012, 14:25 Il presente volume è stato stampato con i fondi di ricerca della Seconda Università di Napoli e col contributo del Dipartimento di Studio delle componenti culturali del territorio e della Facoltà di Lettere e Filosofia. Si ringraziano Antonello Frongia ed Eliseo Saggese per il prezioso aiuto offerto. Toute représentation ou reproduction intégrale ou partielle faite par quelque procédé que ce soit, sans le consentement de l’éditeur ou de ses ayants droit, est illicite. Tous droits réservés. © P.I.E. PETER LANG S.A. Éditions scientifiques internationales Bruxelles, 2012 1 avenue Maurice, B-1050 Bruxelles, Belgique www.peterlang.com ; [email protected] Imprimé en Allemagne ISSN 2031-1311 ISBN 978-90-5201-825-6 D/2012/5678/29 Information bibliographique publiée par « Die Deutsche Nationalbibliothek » « Die Deutsche Nationalbibliothek » répertorie cette publication dans la « Deutsche Nationalbibliografie » ; les données bibliographiques détaillées sont disponibles sur le site http://dnb.d-nb.de. 6 1-6.p65 6 19/03/2012, 14:25 Indice Premessa ............................................................................................... 11 In forma di libro: Boccaccio e la politica degli autori ...................... 15 Giancarlo Alfano Note sulla sintassi del periodo nel Filocolo di Boccaccio .................. 31 Simona Valente Appunti di poetica boccacciana: l’autore e le sue verità .................. 47 Elisabetta Menetti La “bona sonoritas” di Calliopo: Boccaccio a Napoli, la polifonia di Partenope e i silenzi dell’Acciaiuoli ........................... 69 Roberta Morosini «Dal fuoco dipinto a quello che veramente arde»: una poetica in forma di quaestio nel capitolo VIII dell’Elegia di Madonna Fiammetta ................................................... -
Elenco Scuole Disponibili Ad Accogliere Le Gare Regionali - CAMPANIA
Elenco scuole disponibili ad accogliere le gare regionali - CAMPANIA Candidata Candidata polo reg Città Scuola polo reg Secondo Primo Ciclo Ciclo Scisciano Amodeo bethoven EBOLI I.C. ROMANO X CALVIZZANO I.C. MARCO POLO Mignano Monte Lungo I.C. Mignano M.L.- Marzano Bacoli I.C. Plinio il vecchio - Gramsci X X Bacoli I.C. Plinio il vecchio - Gramsci X Atripalda I.C. 'De Amicis - Masi' Vairano Patenora I.C. 'Garibaldi- Montalcini' I.C. 'Ilaria Alpi' - Scuola Secondaria di Primo Grado MONTESARCHIO X X 'Ugo Foscolo' Scisciano I.C. 'Omodeo - Beethoven' X Scisciano I.C. 'Omodeo - Beethoven' X Scisciano I.C. 'Omodeo - Beethoven' X Scisciano I.C.'Omodeo-Beethoven'- plesso centrale- Scisciano I.C.'Omodeo-Beethoven'- plesso succursale- San San Vitaliano Vitaliano Sant'Anastasia I.C:'F.d'Assisi-N.Amore' Benevento I.I.S. GALILEI VETRONE X Sant'Agata de' Goti I.I.S. 'A.M. de' Liguori' NAPOLI IC 2 Moscati Maglione NAPOLI IC 2 Moscati Maglione MONTECORVINO PUGLIANO IC MONTECORVINO PUGLIANO X MONTECORVINO PUGLIANO IC MONTECORVINO PUGLIANO X MONTECORVINO PUGLIANO (SA) IC Montecorvino Pugliano MONTECORVINO PUGLIANO (SA) IC Montecorvino Pugliano CASALNUOVO DI NAPOLI ICS 'ENRICO DE NICOLA' X CAPACCIO PAESTUM IIS IPSAR PIRANESI X TELESE TERME IIS TELESI@ X X Sant'Agata de' Goti IIS 'A.M. de' Liguori' Napoli IISS 'A.Serra' Baronissi Istituto Comprensivo AUTONOMIA 82 Casoria Istituto Comprensivo Nino Cortese Acerno Istituto Comprensivo Statale 'Romualdo Trifone' X Montecorvino Rovella Istituto Comprensivo Statale 'Romualdo Trifone' X Istituto Comprensivo Statale'Ilaria Alpi' Scuola Montesarchio X Primaria Plesso Varoni Montesarchio Airola Istituto istruzione Superiore 'Alessandro Lombardi' Montesarchio istituto istruzione superiore 'E. -
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. -
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 -
Map 44 Latium-Campania Compiled by N
Map 44 Latium-Campania Compiled by N. Purcell, 1997 Introduction The landscape of central Italy has not been intrinsically stable. The steep slopes of the mountains have been deforested–several times in many cases–with consequent erosion; frane or avalanches remove large tracts of regolith, and doubly obliterate the archaeological record. In the valley-bottoms active streams have deposited and eroded successive layers of fill, sealing and destroying the evidence of settlement in many relatively favored niches. The more extensive lowlands have also seen substantial depositions of alluvial and colluvial material; the coasts have been exposed to erosion, aggradation and occasional tectonic deformation, or–spectacularly in the Bay of Naples– alternating collapse and re-elevation (“bradyseism”) at a staggeringly rapid pace. Earthquakes everywhere have accelerated the rate of change; vulcanicity in Campania has several times transformed substantial tracts of landscape beyond recognition–and reconstruction (thus no attempt is made here to re-create the contours of any of the sometimes very different forerunners of today’s Mt. Vesuvius). To this instability must be added the effect of intensive and continuous intervention by humanity. Episodes of depopulation in the Italian peninsula have arguably been neither prolonged nor pronounced within the timespan of the map and beyond. Even so, over the centuries the settlement pattern has been more than usually mutable, which has tended to obscure or damage the archaeological record. More archaeological evidence has emerged as modern urbanization spreads; but even more has been destroyed. What is available to the historical cartographer varies in quality from area to area in surprising ways. -
Rete Di Monitoraggio
ALLEGATO A REGIONE CAMPANIA RETE DI MONITORAGGIO ACQUE DI BALNEAZIONE - ANNO 2021 22/03/2021 (d.lgs.116/08 - DM 30.10.2010 mod.DM 19.04.2018) COORDINATE COORDINATE INIZIO COORDINATE FINE LUNGHEZZA CLASSIFICAZIONE Acqua di PUNTO DI TRATTO ACQUA DI TRATTO ACQUA DI ACQUA DI balneazione ID_AREA_BAL COMUNE ACQUA DI BALNEAZIONE 2021 PRELIEVO BALNEAZIONE BALNEAZIONE BALNEAZIONE (CODICE) (D.Lgs.116/08) Lat. N Long. E Lat. N Long. E Lat. N Long. E (metri) 3064 IT015061027002 CASTEL VOLTURNO 41,06410 13,90690 Pineta Nuova 41,06943 13,90522 41,06025 13,90960 1103 Eccellente 3065 IT015061027003 CASTEL VOLTURNO 41,05510 13,91110 Pescopagano 41,06025 13,90960 41,05229 13,91281 934 Eccellente 3066 IT015061027004 CASTEL VOLTURNO 41,04630 13,91480 Le Morelle 41,05229 13,91281 41,04367 13,91638 1015 Eccellente 3067 IT015061027005 CASTEL VOLTURNO 41,03940 13,91690 Lavapiatti 41,04367 13,91638 41,03821 13,91848 741 Eccellente 3068 IT015061027006 CASTEL VOLTURNO 41,03186 13,91862 Nord Foce Fiume Volturno 41,03821 13,91848 41,02932 13,92159 1180 Eccellente 3070 IT015061027007 CASTEL VOLTURNO 41,01401 13,93228 I Variconi 41,01886 13,93159 41,01202 13,93674 903 Eccellente 3071 IT015061027008 CASTEL VOLTURNO 41,00626 13,94142 Pineta Grande Nord 41,01202 13,93674 41,00591 13,94569 1109 Eccellente 3072 IT015061027009 CASTEL VOLTURNO 41,00060 13,94950 Pineta Grande 41,00591 13,94569 40,99987 13,95241 1072 Buona 3073 IT015061027010 CASTEL VOLTURNO 40,99530 13,95640 Pineta Grande sud 40,99987 13,95241 40,99233 13,96026 1145 Sufficiente 3076 IT015061027013 CASTEL VOLTURNO