Misenum: the Harbour and the City
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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. -
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 ................................................... -
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. -
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. -
Campi Flegrei Caldera, Somma–Vesuvius Volcano, and Ischia Island) from 20 Years of Continuous GPS Observations (2000–2019)
remote sensing Technical Note The Ground Deformation History of the Neapolitan Volcanic Area (Campi Flegrei Caldera, Somma–Vesuvius Volcano, and Ischia Island) from 20 Years of Continuous GPS Observations (2000–2019) Prospero De Martino 1,2,* , Mario Dolce 1, Giuseppe Brandi 1, Giovanni Scarpato 1 and Umberto Tammaro 1 1 Istituto Nazionale di Geofisica e Vulcanologia, Sezione di Napoli Osservatorio Vesuviano, via Diocleziano 328, 80124 Napoli, Italy; [email protected] (M.D.); [email protected] (G.B.); [email protected] (G.S.); [email protected] (U.T.) 2 Istituto per il Rilevamento Elettromagnetico dell’Ambiente, Consiglio Nazionale delle Ricerche, via Diocleziano 328, 80124 Napoli, Italy * Correspondence: [email protected] Abstract: The Neapolitan volcanic area includes three active and high-risk volcanoes: Campi Flegrei caldera, Somma–Vesuvius, and Ischia island. The Campi Flegrei volcanic area is a typical exam- ple of a resurgent caldera, characterized by intense uplift periods followed by subsidence phases (bradyseism). After about 21 years of subsidence following the 1982–1984 unrest, a new inflation period started in 2005 and, with increasing rates over time, is ongoing. The overall uplift from 2005 to December 2019 is about 65 cm. This paper provides the history of the recent Campi Flegrei caldera Citation: De Martino, P.; Dolce, M.; unrest and an overview of the ground deformation patterns of the Somma–Vesuvius and Ischia vol- Brandi, G.; Scarpato, G.; Tammaro, U. canoes from continuous GPS observations. In the 2000–2019 time span, the GPS time series allowed The Ground Deformation History of the continuous and accurate tracking of ground and seafloor deformation of the whole volcanic area. -
Università Di Pisa
Università di Pisa Tesi di Laurea Specialistica La fascia costiera campana da Cuma alla piana del Fiume Sarno: dinamiche paleoambientali e porti antichi Relatore Prof.essa Nella Maria Pasquinucci Candidato Stefano Marinelli ANNO ACCADEMICO 2010-2011 La Campania è la regione più bella non solo d'Italia, ma di tutto il mondo. Non c'è niente di più dolce del suo clima: basti dire che la primavera vi sboccia due volte. Non c'è niente di più fertile del suo suolo: si dice che là gareggino Cerere e Bacco. Niente di più ospitale del suo mare: vi si trovano i famosi porti di Gaeta e di Miseno, di Baia dalle tepide fonti, il Lucrino e l'Averno, quasi luoghi di riposo del mare. Qui ci sono monti cinti di vigneti, il Gauro, il Falerno, il Massico e, più bello di tutti, il Vesuvio, che rivaleggia col fuoco dell'Etna. Ci sono città volte al mare: Formia, Cuma, Pozzuoli, Napoli, Ercolano, Pompei e la stessa loro capitale Capua, un tempo annoverata fra le tre più grandi città (del mondo) con Roma e Cartagine. (Floro, Campania Felix) Indice Introduzione 1 1 Inquadramento dell'area di studio: il golfo di Napoli 5 1.1 Il territorio dei Campi Flegrei . 7 1.1.1 I laghi costieri . 11 1.2 Il territorio dell'antica Neapolis . 13 1.2.1 Settore occidentale . 15 1.2.2 Settore orientale . 16 1.3 Il settore meridionale del golfo di Napoli . 18 2 Dinamiche paleoambientali nella fascia costiera campana in età storica 22 2.1 Evoluzione del paesaggio costiero dei Campi Flegrei . -
Baia. Una Ciudad, O Los Restos De Lo Que Fue, a Veintitrés Ki- Lómetros De Nápoles Y 8 Metros Bajo El Nivel Del Mar
Baia. Una ciudad, o los restos de lo que fue, a veintitrés ki- lómetros de Nápoles y 8 metros bajo el nivel del mar. Aquí comienza el trabajo, un viaje por la antigüedad a través de las ruinas de Baia. El tema de este trabajo se centra en las ruinas de la ciudad subacuática de Baia, conocida antiguamente como Puteoli, una ciudad de vacaciones de la antigua Roma para las clases altas de la sociedad, absorbida por el mar hace más de dos mil años. Esta ciudad albergó grandes autores como Cicerón, Virgilio o Nerón, y en ella aún se pueden encontrar estructu- ras de las villas, calles e incluso templos como el de Venus, además de estatuas o mosaicos perfectamente conservados bajo el agua. Actualmente, a pesar de contar con numerosas investigacio- nes sobre el yacimiento a nivel fotográfico y de conservación, no se encuentran cartografías detalladas del mismo que nos hagan recorrer los restos de la ciudad, más allá de los planos turísticos de museo u otros con poca definición. Por ello, este trabajo pretende entender la evolución de la ciudad de Baia a través de plantas, secciones y dibujos a mano de su emplaza- miento, además del análisis del territorio donde se sitúa. Todo ello se analiza desde los ocho lugares de inmersión existentes actualmente, alrededor de los cuales se desarrolla el trabajo. BAIA 8 CARTOGRAFÍAS SUBACUÁTICAS Autora: CARMEN LLORENTE ANAYA Tutor: ENRIQUE COLOMÉS MONTAÑÉS ABSTRACT Baia. Una ciudad, o los restos de lo que fue, a veintitrés kilómetros de Nápoles y 8 metros bajo el nivel del mar. -
De Feo Giovanni
Università degli Studi di Salerno Dipartimento di Ingegneria Industriale Gli antichi acquedotti romani e alcune meraviglie dell’ Aqua Augusta di Serino Giovanni De Feo www.greenopoli.it UNIVERSITY OF SALERNO - ITALY www.unisa.it Department of Civil Engineering www.unisa.diciv.it Groundwater Recharge in an Endoreic Basin with Reclaimed Municipal Wastewater Giovanni De Feo Wastewater Reclamation & Reuse for Sustainability Nov. 8-11.2005 / Ramada Plaza, Jeju, Korea La Piana del Dragone Volturara Irpina (Av) Dr. Andreas N. Angelakis Honorary Member of IWA Fellow IWA Past President of EUREAU Chairperson of IWA-WWAC SG on Water and Wastewater in Ancient Civilizations Iraklion, Hellas. Ottaviano De Biase Poeta, storico locale, “marinaio di montagna” UNIVERSITY OF SALERNO - ITALY www.unisa.it Department of Civil Engineering www.unisa.diciv.it Historical Development of the Augustan Aqueduct in Southern Italy: Twenty Centuries of Works from SERINO to NAPLES Giovanni DE FEO Via Ferrari, 14 83028 SERINO (AV) EU, FAO, UNESCO, EUREAU, Assoc. of Greek Municipalities IWA Specialty Conference: 1 st International Symposium on Water and Wastewater Technologies in Ancient Civilizations October 28-30, 2006 - Heraklion (Iraklio), Crete, Greece Specialist Group on Water and Wastewater in Ancient Civilizations http://img2.wikia.nocookie.net/__cb20090502052213/timemachine/images/4/45/The_Time_Machine.jpg Università degli Studi di Salerno Dipartimento di Ingegneria Civile www.unisa.it www.unisa.diciv.it Sviluppo Storico dell’Acquedotto Augusteo in Campania: Venti Secoli di Lavori tra SERINO e NAPOLI Giovanni DE FEO A.N.M.I. Associazione Nazionale Marinai d’Italia per la Campania Presenta il volume L’Acqua del Serino - Sorgenti e Acquedotti di Ottaviano De Biase CIRCOLO UFFICIALI DELLA MARINA MILITARE DI NAPOLI Sabato 11 novembre, ore 17.30 Perché i Romani costruivano acquedotti? ° In generale, non per fornire acqua potabile e per motivi igienici: per rifornire le terme (Hodge, 2002) o per scopi militari . -
Plinian Pumice Fall Deposit of the Campanian Ignimbrite Eruption Ž/Phlegraean Fields, Italy
Journal of Volcanology and Geothermal Research 91Ž. 1999 179±198 www.elsevier.comrlocaterjvolgeores Plinian pumice fall deposit of the Campanian Ignimbrite eruption ž/Phlegraean Fields, Italy M. Rosi a,), L. Vezzoli b, A. Castelmenzano b, G. Grieco b a UniÕersitaÁ degli Studi di Pisa, Dipartimento di Scienze della Terra, Õia S. Maria 53, 56126 Pisa, Italy b UniÕersitaÁ degli Studi di Milano, Dipartimento di Scienze della Terra, Õia Mangiagalli 34, 20133 Milan, Italy Abstract A plinian pumice fall deposit associated with the Campanian Ignimbrite eruptionŽ. 36 ka, Phlegraean Fields caldera, Italy occurs at the base of the distal grey ignimbrite in 15 localities spread over an area exceeding 1500 km2 between Benevento and the Sorrentina peninsula. In the thickest stratigraphic section at VosconeŽ. 130 cm , 45 km east of the Phlegraean caldera centreŽ. Pozzuoli , the deposit consists of two units: the lower fall unit Ž. LFU is well sorted, exhibits reverse size grading and is composed of equidimensional light-grey pumice clasts with very subordinate accidental lithics; the upper fall unitŽ. UFU is from well to poorly sorted, crudely stratified, richer in lithics and composed of both equidimensional and prolate pumice clasts. The two fall units show slightly different dispersal axis: N908 for the LFU and N958 for the UFU. Volumes calculated with the method of PyleŽ. 1989 are about 8 km33 for the LFU and 7 km for the UFU. The maximum height of the eruptive columns are estimated, using the model of the maximum lithic clasts dispersal, at 44 km for the LFU and 40 km for the UFU, classifying both fall units as ultraplinian in character. -
Pompeii & Naples
POMPEII & NAPLES BAY: ANCIENT ROMAN WATER SUPPLIES & WATER USE REPORT OF FIELD OBSERVATIONS ‐ SEPTEMBER 2016 Wayne Lorenz i PREFACE The Wright Paleohydrological Institute (WPI) has been researching the Aqua Augusta, the ancient Roman aqueduct that served the Naples Bay region of Italy, including the ancient City of Pompeii, and water use in the city. A few facts regarding the aqueduct and related water systems provide some background to this report. First, ancient Pompeii can justifiably be identified as the most famous archaeological site in the world (Berry, 2007), likely due to its preservation under about 3 to 12 meters (10 to 40 feet) of volcanic ash after the eruption of Mount Vesuvius in A.D. 79. It was here that the modern study of “archaeology” began when the city started to be unearthed over 250 years ago. It is interesting to note that Pompeii is about 75 percent excavated and has revealed many unique details of Roman culture and technology. The archaeological areas of Pompeii, (as well as Herculaneum and Torre Annunziata) were listed as UNESCO World Heritage sites in 1997. The historic center of Naples is also a UNESCO site. The engineering and construction of the Aqua Augusta (also known as the Serino Aqueduct) provided a fresh water supply to communities and fostered economic development in the Naples Bay region during the first century A.D. The aqueduct supplied Pompeii and at least 9 other distinct communities, plus multiple villas, in the Bay of Naples through a system of ten side branches. This seems to have been the most complex single aqueduct ever built by the Romans (Keenan-Jones, 2010). -
The Geography of Augustus Between Persistence and Evolutionary Dynamics the Phlegraean Fields Between the Augustan Reform and Current Functional Reorganization1
Unofficial English version provided by the author of the Italian paper published in: BOLLETTINO DELLA SOCIETÀ GEOGRAFICA ITALIANA ROMA - Serie XIII, vol. IX (2016), pp. 253-267 SIMONE BOZZATO – GIACOMO BANDIERA THE GEOGRAPHY OF AUGUSTUS BETWEEN PERSISTENCE AND EVOLUTIONARY DYNAMICS THE PHLEGRAEAN FIELDS BETWEEN THE AUGUSTAN REFORM AND CURRENT FUNCTIONAL REORGANIZATION1 1. General framework. – At the end of the Republican era, thus on the eve of the territorial reorganization issued by Augustus, Italy was divided into more than four hundred local communities, which were self-governed with a high degree of autonomy and with their own magistrates, senates, and political assemblies. The magistrates were vested with jurisdictional powers, even if somewhat limited regarding the nature and value of disputes; the senates dealt with administrative and judicial issues; the local magistrates were elected by the comitia who were authorized to introduce certain restricted legislation. The unifying mantle of granting Roman citizenship to all the inhabitants of what we today call Italy had blurred any differences and softened any diversities, and all municipalities were obviously subject to laws and to Roman law. Rome was the center of power, the place where the constitutional bodies of the State, the magistrates, the Senate and comitia were located and where their meetings were held; the arena in which «national» political life was carried out. Laws and common law were the founding values of a unitary frame within which each individual authority maintained mediated relations with the central power (Laffi, 2007). The Augustan territorial reorganization, which may be seen as based on a flexible pragmatism from the point of view of what would be a substantive approach, was engaged in this status quo. -
M. Guidarelli1, A. Zille, A. Saraò1, M. Natale2, C. Nunziata2 and G.F. Panza1,3
Available at: http://www.ictp.it/~pub_off IC/2006/145 United Nations Educational, Scientific and Cultural Organization and International Atomic Energy Agency THE ABDUS SALAM INTERNATIONAL CENTRE FOR THEORETICAL PHYSICS SHEAR-WAVE VELOCITY MODELS AND SEISMIC SOURCES IN CAMPANIAN VOLCANIC AREAS: VESUVIUS AND PHLEGRAEAN FIELDS M. Guidarelli1, A. Zille, A. Saraò1, M. Natale2, C. Nunziata2 and G.F. Panza1,3 1 Dipartimento di Scienze della Terra, Università degli Studi di Trieste, Trieste, Italy 2 Dipartimento di Geofisica e Vulcanologia, Università di Napoli “Federico II”, Napoli, Italy 3 The Abdus Salam International Centre for Theoretical Physics, Trieste, Italy MIRAMARE – TRIESTE December 2006 Abstract This chapter summarizes a comparative study of shear-wave velocity models and seismic sources in the Campanian volcanic areas of Vesuvius and Phlegraean Fields. These velocity models were obtained through the nonlinear inversion of surface- wave tomography data, using as a priori constraints the relevant information available in the literature. Local group velocity data were obtained by means of the frequency-time analysis for the time period between 0.3 and 2 s and were combined with the group velocity data for the time period between 10 and 35 s from the regional events located in the Italian peninsula and bordering areas and two station phase velocity data corresponding to the time period between 25andl00s.In order to invert Ray lei gh wave dispersion curves, we applied the nonlinear inversion method called hedgehog and retrieved average models for the first 30-35 km of the lithosphere, with the lower part of the upper mantle being kept fixed on the basis of existing regional models.