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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. -
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. -
Nonindigenous Species Along the Apulian Coast, Italy
Chemistry and Ecology Vol. 26, Supplement, June 2010, 121–142 Nonindigenous species along the Apulian coast, Italy Cinzia Gravilia*, Genuario Belmontea, Ester Cecereb, Francesco Denittoa, Adriana Giangrandea, Paolo Guidettia, Caterina Longoc, Francesco Mastrototaroc, Salvatore Moscatelloa, Antonella Petrocellib, Stefano Pirainoa, Antonio Terlizzia and Ferdinando Boeroa aDipartimento di Scienze e Tecnologie Biologiche ed Ambientali, Università del Salento, Lecce, Italy; bIstituto Ambiente Marino Costiero, CNR, U.O.S. Taranto, Taranto, Italy; cDipartimento di Biologia Animale ed Ambientale, Università di Bari, Bari, Italy (Received 17 May 2009; final version received 14 December 2009) Thirty-eight nonindigenous marine species (NIS) (macroalgae, sponges, hydrozoans, molluscs, polychaetes, crustaceans, ascidiaceans and fish), are reported from the Apulian coast of Italy. Shipping, aquaculture and migration through the Suez Canal are the main pathways of introduction of the NIS. In Apulian waters, 21% of NIS are occasional, 18% are invasive and 61% are well-established. It is highly probable that more NIS will arrive from warm-water regions, because Mediterranean waters are warming. Furthermore, some of the successful NIS must have the ability to become dormant in order to survive adverse conditions, either seasonal or during long journeys in ballast waters. The identification of NIS depends greatly on the available taxonomic expertise; hence the paucity of taxonomists hinders our knowl- edge of NIS in our seas. We propose the creation and maintenance of a network of observatories across the Mediterranean to monitor the changes that take place along its coasts. Keywords: nonindigenous species (NIS); transport vectors; Apulian coast; Mediterranean Sea Downloaded By: [Gravili, Cinzia] At: 10:25 20 May 2010 1. -
Is the Gulf of Taranto an Historic Bay?*
Ronzitti: Gulf of Taranto IS THE GULF OF TARANTO AN HISTORIC BAY?* Natalino Ronzitti** I. INTRODUCTION Italy's shores bordering the Ionian Sea, particularly the seg ment joining Cape Spartivento to Cape Santa Maria di Leuca, form a coastline which is deeply indented and cut into. The Gulf of Taranto is the major indentation along the Ionian coast. The line joining the two points of the entrance of the Gulf (Alice Point Cape Santa Maria di Leuca) is approximately sixty nautical miles in length. At its mid-point, the line joining Alice Point to Cape Santa Maria di Leuca is approximately sixty-three nautical miles from the innermost low-water line of the Gulf of Taranto coast. The Gulf of Taranto is a juridical bay because it meets the semi circular test set up by Article 7(2) of the 1958 Geneva Convention on the Territorial Sea and the Contiguous Zone. 1 Indeed, the waters embodied by the Gulf cover an area larger than that of the semi circle whose diameter is the line Alice Point-Cape Santa Maria di Leuca (the line joining the mouth of the Gulf). On April 26, 1977, Italy enacted a Decree causing straight baselines to be drawn along the coastline of the Italian Peninsula.2 A straight baseline, about sixty nautical miles long, was drawn along the entrance of the Gulf of Taranto between Cape Santa Maria di Leuca and Alice Point. The 1977 Decree justified the drawing of such a line by proclaiming the Gulf of Taranto an historic bay.3 The Decree, however, did not specify the grounds upon which the Gulf of Taranto was declared an historic bay. -
FASTMIT Project Activities in the Apulia Platform: Evidence of an Active Fault System in the Salento Offshore (Ionian Sea) F.E
GNGTS 2017 SESSIONE 1.2 FASTMIT PROJECT ACTIVITIES IN THE APULIA PLATFORM: EVIDENCE OF AN ACTIVE FAULT SYSTEM IN THE SALENTO OFFSHORE (IONIAN SEA) F.E. Maesano1, V. Volpi2, R. Basili1, M.M. Tiberti1, M. Zecchin2, S. Ceramicola2, G. Rossi2 1 Istituto Nazionale di Geofisica e Vulcanologia, Roma, Italy 2 Istituto Nazionale di Oceanografia e Geofisica Sperimentale (OGS), Trieste, Italy The FASTMIT Project (FAglie Sismogeniche e Tsunamigeniche nei Mari Italiani) aims to widening and systematizing the knowledge on seismogenic and potentially tsunamigenic faults in the Italian marine areas, thereby taking the pledge to address compelling issues related to geohazards of coastal areas and offshore infrastructures. FASTMIT study areas straddle the Europe-Nubia plate boundary, with focus on the Adriatic Sea, the Gulf of Taranto, the Sicily Channel and the Southern Tyrrhenian Sea. Here we present the preliminary results in the Gulf of Taranto. This area has been recently studied in the framework of various national and international projects (e.g.: EC HERMES, MAGIC, RITMARE, CARG, DPC-INGV-S1), which highlighted its geological complexities. In this area, the Apulia Platform is inflected under the Calabrian Accretionary Wedge as a result of the subduction of the Ionian oceanic crust and the subsequent collision with the Apulia continental margin. The Apulia Platform units have been recognized under the allochthonous units of the accretionary wedge in all the Gulf of Taranto and in the offshore of Crotone where they are affected by transpressional structures (Maesano et al., 2017; Volpi et al., 2017), whereas in the foreland areas (Salento offshore) they are affected by normal faulting. -
Romanisation in the Brindisino, Southern Italy: a Preliminary Report Douwe Yntema
BaBesch 70 (1995) Romanisation in the Brindisino, southern Italy: a preliminary report Douwe Yntema I. INTRODUCTION Romanisation is a highly complicated matter in southern Italy. Here, there was no culture dialogue Romanisation is a widely and often indiscrimi- involving two parties only. In the period preceding nately used term. The process expressed by the the Roman incorporation (4th century B.C.) this word involves at least two parties: one of these is area was inhabited by several different groups: rel- the Roman world and the other party or parties is ative latecomers were the Greek-speaking people or are one or more non-Roman societies. These who had emigrated from present-day Greece and are the basic ingredients which are present in each the west coast of Asia Minor to Italy in the 8th, 7th definition, be it explicit or implicit, of that term. and 6th centuries; they lived mainly in the coastal Many scholars have given their views on what strip on the Gulf of Taranto. Other (‘native') they think it should mean. Perhaps the most satis- groups had lived in southern Italy since the Bronze factory definition was formulated by Martin Age. Some groups in present-day Calabria and Milett. In his view, Romanisation is not just Campania displayed initially close links with the another word to indicate Roman influence: ‘it is urnfield cultures of Central Italy. Comparable a process of dialectical change rather than the groups, living mainly in present-day Apulia and influence of one … culture upon others' (Millett Basilicata and having closely similar material cul- 1990). -
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UNIVERSITÀ DEGLI STUDI DI NAPOLI “FEDERICO II” PhD thesis “Marine organisms model species for the assessment of biological, environmental and economic impacts on marine aquaculture in Campania” Coordinatore Candidato Tutor Prof. Dott. ssa Dott. Giuseppe Cringoli Sara Fioretti Francesco Paolo Patti Prof. Aniello Anastasio “First, think. Second, believe. Third, dream. And finally, dare. If you can dream it, you can do it” Walt Disney Index Abbreviations list ......................................................................................13 Figures list .................................................................................................15 Tables list ...................................................................................................17 Abstract .....................................................................................................19 Introduction ..............................................................................................23 I Aquaculture in Campania: from the origin to the current times ..........25 II Aquaculture today: global and European trend ..................................27 III Aquaculture in Italy ...........................................................................30 IV Aquaculture in Campania ..................................................................31 V Mussel farms: breeding systems .........................................................33 VI Mussel farms threats and future perspectives for the Campanian industries ................................................................................................35 -
The Amendolara Ridge, Ionian Sea, Italy
An active oblique-contractional belt at the transition between the Southern Apennines and Calabrian Arc: the Amendolara Ridge, Ionian Sea, Italy. Luigi Ferranti (*, a), Pierfrancesco Burrato (**), Fabrizio Pepe (***), Enrico Santoro (*, °), Maria Enrica Mazzella (*, °°), Danilo Morelli (****), Salvatore Passaro (*****), Gianfranco Vannucci (******) (*) Dipartimento di Scienze della Terra, dell’Ambiente e delle Risorse, Università degli Studi di Napoli Federico II, Napoli, Italy. (**) Istituto Nazionale di Geofisica e Vulcanologia, Roma, Italy. (***) Dipartimento di Scienze della Terra e del Mare, Università di Palermo, Italy. (****) Dipartimento di Scienze Geologiche, Ambientali e Marine, Università di Trieste, Italy (*****) Istituto per l’Ambiente Marino Costiero, Consiglio Nazionale delle Ricerche, Napoli, Italy (******) Istituto Nazionale di Geofisica e Vulcanologia, Bologna, Italy. (°) presently at Robertson, CGG Company, Wales. (°°) presently at INTGEOMOD, Perugia, Italy. (a) Corresponding author: L. Ferranti, DiSTAR - Dipartimento di Scienze della Terra, dell'Ambiente e delle Risorse, Università di Napoli “Federico II,” Largo S. Marcellino 10, IT-80138 Naples, Italy. ([email protected]) This article has been accepted for publication and undergone full peer review but has not been through the copyediting, typesetting, pagination and proofreading process which may lead to differences between this version and the Version of Record. Please cite this article as doi: 10.1002/2014TC003624 ©2014 American Geophysical Union. All rights -
Decapoda Brachyoura) in the Mediterranean Sea M
THALASSIA JUGOSLAVICA 8 (1) 105—117 (1972) 105 Conference Paper Decapoda Crustacea in the Gulf of Taranto and the Gulf of Catania with a discussion of a new species of Dromidae (Decapoda Brachyoura) in the Mediterranean Sea M. A. Pastore Istituto Sperimentale Talassografico Taranto, via Roma 3, 74100 Taranto, Italy Two sources give information about Jonian Decapoda. One, by Costa1 is a catalogue of 51 Decapoda found in the Taranto area. Also in Costa2, two other species are mentioned which make a total number of 53. The other source, by Forest', is a list of 67 Decapoda found in the Porto Cesareo area. The list of the species is enlarged by a new find in the Gulf of Taranto and the Gulf of Catania. Dromidiopsis spinirostris (Miers, 1881) is also a new Record for the Mediterranean Sea. At the moment, 119 species of Decapoda in the Jonian Sea are re corded, 25 of which are not recorded above. In this work we have examined 74 species: 6 Peneidaea, 8 Caridea, 7 Macrura reptantia, 11 Anomura and 42 Brachiura. INTRODUCTION The materials studied in this work were collected under various circum stances and at different times and places from 1969 until today. All of them are from the Jonian sea. Most of these species are common or very common in the western Medi terranean. But there are some species which are mentioned here for the first time. There is very little literature for the Jonian sea. We have found only five works which deal with the area. From the past century Rizza4 describes material from the Gulf of Catania and Costa1 describes material from the Gulf of Taranto. -
Marine Stratigraphy of Active Volcanic Areas in the Campania Offshore: Correlation Between the Seismic Units of the Gulf of Pozzuoli and Ischia Island G
GNGTS 2016 SESSIONE 3.2 MARINE STRATIGRAPHY OF ACTIVE VOLCANIC AREAS IN THE CAMPANIA OFFSHORE: CORRELATION BETWEEN THE SEISMIC UNITS OF THE GULF OF POZZUOLI AND ISCHIA ISLAND G. Aiello CNR-IAMC Sede di Napoli, Naples, Italy Introduction. The marine stratigraphy of active volcanic areas located in the Campania offshore is herein shown and discussed based on high resolution seismic data (Sparker seismic source). Selected examples located in the Gulf of Pozzuoli and in the Ischia offshore will be shown. New and innovative geological and hazard maps of volcanic terrains have been presented, dealing with the definition of mapped units during the field survey, highlighting that a geological map represents a warehouse in which to store the data existing on past eruptions and on inter-eruptive phenomena, having significant implications on the volcanic hazard assessment (Lucchi et al., 2010; Tibaldi, 2010; Bonomo and Ricci, 2010; Palladino et al., 2010; Viereck-Goette et al., 2010; Martì et al., 2010; Gertisser et al., 2010; Milia, 2010; Perrotta et al., 2010; De Vita et al., 2010; De Beni and Groppelli, 2010; Cortes et al., 2010; Vargas-Franco et al., 2010; Sheridan et al., 2010). Marine stratigraphy of active volcanic areas in the Campania offshore has been previously discussed, focusing on examples located in the Gulf of Pozzuoli and Ischia island (Aiello et al., 2012a, 2012b). The techniques of sequence stratigraphy have 534 GNGTS 2016 SESSIONE 3.2 been successfully applied in seismo-stratigraphic interpretation of high resolution seismic data (Fig. 1) to produce reliable geoseismic sections showing the stratigraphic relationships among volcanic bodies and interstratified marine deposits, mostly pertaining to the Late Quaternary depositional sequence (De Lange et al., 1989; Amorosi et al., 2008; Riboulot et al., 2012; Oyedele and Duprè, 2014; Aiello and Marsella, 2015). -
Map 45 Tarentum Compiled by I.E.M
Map 45 Tarentum Compiled by I.E.M. Edlund-Berry and A.M. Small, 1997 Introduction The landforms of South Italy have changed in many respects since the classical period. On both the Tyrrhenian and Adriatic coasts the sea level has risen in relation to the landmass, submerging the Oenotrides islands which once provided anchorage off the west coast at Velia, and drowning Roman coastal installations on the Adriatic (Michaelides 1992, 21). As elsewhere in the peninsula, the increase in human population has led to deforestation of the hills, with consequent erosion of the slopes and sedimentation in the valley bottoms (Boenzi 1989; Campbell 1994; Barker 1995, 62-83). Increased silting in the lower courses of the rivers created marshy conditions in the coastal plains, which were only drained and rendered safe from malaria in the mid-twentieth century. The alluvial deposits have pushed out the coastline along the Ionian Gulf and the Gulf of Paestum, so that the remains of the ancient ports there now lie a considerable distance inland. Deforestation has also led to flash flooding, which in turn has caused rivers to change their courses. Such change is vividly illustrated by the Via Traiana, which crossed the Cerbalus and Carapelle (ancient name unknown) rivers by bridges that now straddle dry land. Other changes have been brought about by more deliberate human intervention. Several inland lakes have been drained since Roman times to provide arable land or relieve malaria. We have reconstructed these on the map where the evidence is reasonably clear, as it is at Forum Popili on the R. -
The Phlegrean Fields
Generale_INGL 25-03-2008 13:26 Pagina 40 The Phlegrean Fields 40 41 The Phlegrean Fields is a place of profound and The Phlegrean Fields (from the Greek Flegraios, ancient fascination. Here history, legend, myth and or “burning”) is an enormous volcanic area that i mystery melt into a fickle landscape. Rich with extends to the west of the Gulf of Naples from the history and art, the Phlegrean Fields are also hill of Posillipo to Cuma, and includes the islands extraordinarily beautiful, with the signs of volcanic of Nisida, Procida, Vivara and Ischia. activity clearly evident. The volcanic nature of the zone is immediately The area was an obligatory stop on the Grand Tour. obvious in the widespread presence of tuff, pumice, Azienda Autonoma The myths sung by Homer and Virgil, the Greek geysers of scorching steam and the craters that form di Cura Soggiorno culture that spread onto the rest of the peninsula, the natural amphitheatres. Some craters have become e Turismo di Pozzuoli via Campi Flegrei 3 record of the times in which the Roman aristocracy lakes like Averno, Lucrino, Fusaro and Miseno. tel. 081 5261481/5262419 built sumptuous villas: all of it helped to increase Active vulcanic phenomena are visibile close-up, www.infocampiflegrei.it the fascination of an area where extraordinary like in the famous Solfatara with its lake of lava, and Pozzuoli Tourist natural beauty and the wonderous opera of man the thermal springs of Agnano. In order to safeguard Information Office create an incomparable scenery. Archaeology lovers the delicate environmental equilibrium, the area piazza Matteotti l/a will find so much to see: impressive ruins, was made into the Phlegrean Fields Regional Park tel.