DOCSLIB.ORG

Geology of the Southern Apennines

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text
Geology of the Southern Apennines Boll.Soc.Geol.It. (Ital.J.Geosci.), Spec. Issue No. 7 (2007), pp. 75-119, 14 figs., CROP-04 (ed. by A. Mazzotti, E. Patacca and P. Scandone) Geology of the Southern Apennines E. PATACCA (*) & P. SCANDONE (*) ABSTRACT – breve descrizione delle tappe più significative dell’evoluzione cinematica del sistema catena-avanfossa-avampaese dal Miocene in- This paper aims to provide a concise description of the geology feriore alla fine del Pleistocene inferiore. of the Southern Apennines especially useful for readers having scarce familiarity with this complex region. The text is divided into La carta geologica strutturale allegata dovrebbe aiutare il lettore four parts: a conservare il quadro regionale d’assieme, volutamente semplifica- to, durante la lettura della nota. Qualora il lettore volesse approfon- – Brief introduction to the geology of the Southern Apennines dire le sue conoscenze sulle problematiche dell’Appennino meridio- in which the general outlines of the thrust belt-foredeep-foreland nale, è stata messa a disposizione, unità per unità, una bibliografia system are given together with a general description of the internal selezionata. Attraverso di essa il lettore potrà navigare all’interno structural architecture of the mountain chain; delle numerose controversie e contraddizioni interne che rendono – Summary of the paleogeographic models existing in the geo- variegata la letteratura geologica italiana logical literature and discussion of the basic criteria used for the palinspastic restoration of the Apennine depositional domains pro- posed in this paper; TERMINI CHIAVE: Italia, Appennino Centrale, Appennino – Synthetic description of the Apennine tectonic units and of Meridionale, unità tettoniche, depositi discordanti sulla the Neogene-Quaternary thrust-sheet-top deposits cropping out in catena. the study area and discussion on the available structural and strati- graphic information constraining the time-space reconstruction of the tectonic deformation; – Short illustration of the principal steps describing the kine- 1. FOREWORD matic evolution of the thrust belt-foredeep-foreland system from the early Miocene to the end of the early Pleistocene. This paper aims to provide a concise description of The enclosed simplified geological-structural map will help the the geology of the Southern Apennines especially useful reader to keep in mind without difficulties the key points of the regional framework. Selected references on the single tectonic unit for readers having scarce familiarity with this complex or thrust-sheet-top deposit have been provided at the end of each region. The work is divided into four parts: paragraph, with the aim of assisting the reader who wanted to tackle the Apennine geological problems by navigating through the – Brief introduction to the geology of the Southern numerous controversies and internal inconsistencies of the current Apennines in which the general outlines of the thrust literature. belt-foredeep-foreland system are given together with a general description of the internal structural architecture KEY WORDS: Italy, Central Apennines, Southern Apennines, of the mountain chain; tectonic units, thrust-sheet-top deposits. – Summary of the paleogeographic models existing in the geological literature and discussion of the basic cri- teria used for the palinspastic restoration of the Apennine RIASSUNTO depositional domains proposed in this paper; – Synthetic description of the Apennine tectonic Geologia dell’Appennino Meridionale. units and of the Neogene-Quaternary thrust-sheet-top Questo lavoro ha lo scopo di fornire una succinta descrizione deposits present in the study area and discussion on the della geologia dell’Appennino meridionale rivolta sopratutto ad un available stratigraphic and structural information con- lettore che abbia scarsa dimestichezza con l’area. Il lavoro è diviso in straining the time-space reconstruction of the tectonic quattro parti: deformation; – breve introduzione alla geologia dell’Appennino Meridionale – Description of the principal steps describing the nella quale viene fornito un quadro generale relativo agli elementi di kinematic evolution of the thrust belt-foredeep-foreland primo ordine del sistema catena-avanfossa-avampaese e alla struttu- ra interna della catena; system from the early Miocene to the early Pleistocene. – rassegna dei modelli paleogeografici esistenti in letteratura e discussione dei criteri utilizzati per la ricostruzione palinspastica Where possible, the surface geological data have been che viene qui proposta; integrated with the subsurface information coming from – descrizione sintetica delle unità tettoniche che formano la ca- extensive petroleum exploration in the area. tena Sud-Appenninica e dei depositi che le ricoprono in discordanza; The enclosed simplified geological-structural map will discussione sulle evidenze strutturali e sui dati stratigrafici disponi- bili per vincolare la ricostruzione spazio-temporale della deforma- help the reader to keep in mind without difficulties the zione tettonica; key points of the regional framework. Selected references on the single tectonic unit or thrust-sheet-top deposit have been provided at the end of each paragraph, with the aim of assisting the reader who wanted to tackle the (*) Dipartimento di Scienze della Terra dell’Università di Pisa - Apennine geological problems by navigating through the Via Santa Maria, 53 - 56100 Pisa, Italy - [email protected] - numerous controversies and internal inconsistencies of [email protected] the current literature. 76 E. PATACCA & P. SCANDONE Fig. 1 GEOLOGY OF THE SOUTHERN APENNINES 77 2. GEOLOGICAL FRAMEWORK OF THE SOUTHERN APENNINES provided in other pages of this volume (see PATACCA & SCANDONE, Constraints on the interpretation of the CROP- The area object of this paper is located in the north- 04 seismic line derived from Plio-Pleistocene foredeep and ern part of the Southern Apenninic Arc, a segment of the thrust-sheet-top deposits); mountain chain that extends from the Southern Abruzzi- 4) The Adriatic-Apulia foreland, constituted of Meso- Alto Molise region to Sicily through the Calabrian Arc zoic-Tertiary carbonates and Triassic evaporites overlying (see fig. 1). Four first-order geological elements may be a thick pile of mixed carbonate-siliciclastic Paleozoic distinguished in this region (see PATACCA et alii, 1990 and deposits the top of which has been reached at a depth of references therein): 6112 m be the Puglia 1 well. A Precambrian (Baikalian- Panafrican) crystalline basement has been hypothesized 1) The Tyrrhenian area, characterized by oceanic under the whole Adriatic-Apulia foreland (VAI, 1994, crust and thinned continental crust, representing a back- 2001). arc extensional feature developed at the rear of the Apen- nine system in late- and post-Tortonian times. Intermedi- The enclosed simplified geological-structural map ate and deep-focus earthquakes depict a relic lithospheric shows the areal distribution of the tectonic units in the slab dipping towards the NE beneath the Aeolian calc- Southern Apennines and their mutual geometric relation- alkaline arc (ANDERSON & JACKSON, 1987; GIARDINI & ships. Our definition of «tectonic unit» roughly corre- VELONÀ, 1991); sponds to the definition of «structural-stratigraphic unit» 2) The Southern Apennine mountain chain, formed of IPPOLITO et alii (1975). A tectonic units is represented by a deep-seated carbonate duplex system («Inner Apulia by a single thrust sheet or, more frequently, by a group of Platform» of the geological literature, see MOSTARDINI & thrust sheets constituted of stratigraphic successions MERLINI, 1986) tectonically overlain by a thick pile of referable to the same paleogeographic realm, which have NE-verging rootless nappes derived from basin and plat- undergone a specific tectonic evolution different from the form domains (MOSTARDINI & MERLINI, 1986; CELLO et tectonic evolution recorded in the overlying and underly- alii, 1987, 1989; CASERO et alii, 1988, 1991; PATACCA & ing thrust sheets. Every tectonic unit is separated from SCANDONE, 1989, 2001; PATACCA et alii, 1992a,b; ROURE the underlying and overlying ones by first-order thrust et alii, 1991; MATTAVELLI et alii, 1993; ROURE & SASSI, surfaces (e.g. Triassic-Cretaceous deep-water deposits of 1995; LA BELLA et alii, 1996; LENTINI et alii, 1996, 2002; the Lagonegro Units tectonically sandwiched between the CORRADO et alii, 1997, 1998a,b; SPERANZA et alii, 1998: Triassic-Miocene platform carbonates of the Alburno-Cer- MONACO et alii, 1998; CELLO & MAZZOLI, 1999; DI BUCCI vati plus Monti della Maddalena Units (hangingwall) and et alii, 1999; SCROCCA & TOZZI, 1999; MENARDI NOGUERA the lower Pliocene siliciclastic flysch deposits stratigraph- & REA, 2000; IMPROTA et alii, 2000; MAZZOLI et alii, 2000, ically covering the Mesozoic-Tertiary carbonates of the 2001). The buried duplex system is composed of shallow- Apulia Platform (footwall). Thrust surfaces delimitating water and subordinate deeper-water Mesozoic-Tertiary tectonic units are usually represented, in the Southern carbonates stratigraphically covered by Pliocene terrige- Apennines, by long thrust flats displaying very low cutoff nous deposits. The Mesozoic carbonates, representing the angles at the footwall. The only exception is represented main target of oil research in the Southern Apennines, by the Sannio Unit, the basal contact of which with the have been extensively explored and carefully mapped over underlying Lagonegro Units corresponds
Load more

Recommended publications
  • Urban Planning in the Greek Colonies in Sicily and Magna Graecia
    Urban Planning in the Greek Colonies in Sicily and Magna Graecia (8th – 6th centuries BCE) An honors thesis for the Department of Classics Olivia E. Hayden Tufts University, 2013 Abstract: Although ancient Greeks were traversing the western Mediterranean as early as the Mycenaean Period, the end of the “Dark Age” saw a surge of Greek colonial activity throughout the Mediterranean. Contemporary cities of the Greek homeland were in the process of growing from small, irregularly planned settlements into organized urban spaces. By contrast, the colonies founded overseas in the 8th and 6th centuries BCE lacked any pre-existing structures or spatial organization, allowing the inhabitants to closely approximate their conceptual ideals. For this reason the Greek colonies in Sicily and Magna Graecia, known for their extensive use of gridded urban planning, exemplified the overarching trajectory of urban planning in this period. Over the course of the 8th to 6th centuries BCE the Greek cities in Sicily and Magna Graecia developed many common features, including the zoning of domestic, religious, and political space and the implementation of a gridded street plan in the domestic sector. Each city, however, had its own peculiarities and experimental design elements. I will argue that the interplay between standardization and idiosyncrasy in each city developed as a result of vying for recognition within this tight-knit network of affluent Sicilian and South Italian cities. This competition both stimulated the widespread adoption of popular ideas and encouraged the continuous initiation of new trends. ii Table of Contents: Abstract. …………………….………………………………………………………………….... ii Table of Contents …………………………………….………………………………….…….... iii 1. Introduction …………………………………………………………………………..……….. 1 2.
    [Show full text]
  • PIANO DI MONITORAGGIO DEL LUPO (Canis Lupus) NEL PARCO NATURALE REGIONALE DEI MONTI SIMBRUINI
    PARCO NATURALE REGIONALE DEI MONTI SIMBRUINI PIANO DI MONITORAGGIO DEL LUPO (Canis lupus) NEL PARCO NATURALE REGIONALE DEI MONTI SIMBRUINI 2008-2009 Ilaria GUJ - Servizio Monitoraggio e Sorveglianza 1. INTRODUZIONE 3 2. CENNI ALLA SITUAZIONE PREGRESSA 4 2.1 Presenza del lupo dagli anni ’80 ai primi anni 2000. 4 2.2 Presenza del lupo dal 2003 al 2008 4 2.3 Predazioni sulla fauna selvatica 5 2.4 Bracconaggio. 6 2.5 Danni al patrimonio zootecnico 6 2.6 Reperti conservati presso l’Ente 7 3. OBIETTIVI DEL PIANO DI MONITORAGGIO 8 4. METODOLOGIE DI CAMPO 8 4.1 Wolf-Howling 8 4.2 Snowtracking 10 4.3 Rilevamento simultaneo su neve 11 4.4 Analisi dei dati relativi alle richieste di danno da fauna selvatica sul bestiame domestico 12 4.5 Utilizzo opportunistico di trappole fotografiche 13 5. MONITORAGGIO GENETICO 13 5.1 Introduzione 13 5.2 Strategia di campionamento 14 5.3 Raccolta campioni fecali 14 5.4 Altri campioni biologici 14 5.5 Criteri di scelta del laboratorio 14 6. SCHEMA GENERALE DEL PERSONALE NECESSARIO 15 BIBLIOGRAFIA 16 ALLEGATI 17 2 1. INTRODUZIONE Il “Piano di monitoraggio del lupo” è uno dei prodotti previsti dal “Progetto Lupo” nell’ambito delle attività previste dalla Convenzione fra la Provincia di Roma, il Parco Naturale Regionale dei Monti Simbruini e il Dipartimento BAU dell’Università di Roma La Sapienza (Determinazione R.U. N° 6504 del 29/10/07 del Servizio Ambiente della Provincia di Roma). La presenza del lupo nel Parco Naturale Regionale dei Monti Simbruini è stabile fin dagli anni ’70 e probabilmente la specie non si è mai estinta in questo comprensorio, a differenza di quanto accaduto nella maggior parte del territorio italiano.
    [Show full text]
  • Bernalda - Metaponto Scalo Quadro Delle Corse: ANDATA
    Linea: 344 - Matera - Bernalda - Metaponto Scalo Quadro delle Corse: ANDATA ORARIO VALIDO DAL 01/10/2019 ATTUALMENTE IN VIGORE Frequenza Scolastica Scolastica Scolastica Non Scol Scol Feriale Note - 1 2 - 3 - Matera - Piazzale Matteotti 06:45 13:30 13:30 14:10 14:30 18:10 Matera- Ospedale Maria SS delle Grazie 06:48 13:33 13:33 14:13 14:33 18:13 Matera - Via Levi - 13:35 13:35 - 14:35 - Innesto SP 10/SS 7 07:00 13:45 13:45 14:25 14:45 18:25 Innesto SS. 7/SS 380 07:15 14:00 14:00 14:40 15:00 18:40 Bernalda Bivio 07:25 14:10 14:10 14:50 15:10 18:50 Bernalda C.so Umberto 07:35 - - - - - Bernalda P.zza Plebiscito - 14:20 14:20 15:00 15:20 19:00 Metaponto Borgo / SC 07:50 - - - - - Note: 1) Partenza ore 13:15 da Istituti scolastici C.da Rondinelle per Piazzale Matteotti 2) Partenza Via Mattei Istituti scolastici ore 13:20 - Piazzale Matteotti - Uscita Matera Sud 3) Partenza Via Mattei Istituti scolastici ore 14:20 - Piazzale Matteotti - Uscita Matera Sud N.B. Da Matera per Bernalda, nel periodo non scolastico, c'è la possibilità di prendere il bus delle 6:20 da Piazzale Matteotti per Policoro (Linea 354) ed effettuare cambio autobus sulla SS 175 con Bus in coincidenza proveniente da Montescaglio (Linea 337) e diretto a Bernalda - Policoro, con arrivo a Bernalda in P.zza Plebiscito alle ore 6:55 N.B. Prestare attenzione alle partenze in quanto le suddette corse possono essere espletate oltre che dalla Sita Sud, anche da consorziati Cotrab (Società Chiruzzi) Andata pagina 1 di 3 Linea: 344 - Matera - Bernalda - Metaponto Scalo Quadro delle Corse: RITORNO ORARIO VALIDO DAL 01/10/2019 ATTUALMENTE IN VIGORE Frequenza Feriale Scolastica Scolastica Scolastica Feriale Note 1 2 3 - 4 Metaponto Borgo / SC - - - 14:00 - Bernalda P.zza Plebiscito 07:00 07:00 07:00 - 17:00 Bernalda C.so Umberto - - - 14:15 - Bernalda Bivio 07:10 07:10 07:10 14:25 17:10 Innesto SS.
    [Show full text]
  • Geochronology of Volcanic Rocks from Latium (Italy)
    R£:-Imcu-...:n UELLA !'oclt;TA 1TALl .... N.... DI MlNER.-\LOG1A E l'ETROLOGIA, 1985, Vu!. 40, pp. 73·106 Geochronology of volcanic rocks from Latium (Italy) MARIO FORNASERl Istituto di Geochirnica dell'Universita, Citta Universit:nia, Piazza Aldo Moro, 0018.5 ROffia Centro di Studio per la Geocronologia e la Geochimica delle Formazioni Recenti del CN.R. ABSTRACT. - The age determination data for A few reliable age measurements arc available volcanic rocks from Latium (haly) are reviewed. for the Sabatini volcanoes, rather uniformely scat· This paper reports the geochronological data obtained tert-d between 607 and 85 ka. The "tufo rosso a chefly by the Ar-K t~hnique, but also by Rb-Sr, scorie nere,. from the sabatian region, which is ""'rh, "C and fission tI"1lcks methods. the analogue of the ignimbrite C from Vico has a The Latium region comprises rocks belonging to firmly established age of 442 + 7 ka. This formation the acidic volcanic groups of Tolfa, Ceriti and Man. can be considered an impor-tant marker not only ziana districlS and to Mt. Cimino group, having for the tephrochronology but also, more generally, strong magmatic affinity with the Tuscan magmatic for the Quaternary deposits in Latium. province and the rocks of the Roman Comagmatic Taking into account all data in the literature Region. lbe last one encompasses the Vulsinian, the oldest known product of the Alban Hills show Vicoan, Sabatinian volcanoes, the Alban Hills and an age of 706 ka, but more recent measurements rhe volcanoes of the Valle del Sacco, often referred indicate for these pt<xluclS a mol'C recent age to as Mts.
    [Show full text]
  • Medici Convenzionati Con La ASM Elencati Per Ambiti Di Scelta
    DIPARTIMENTO CURE PRIMARIE S.S. Organizzazione Assistenza Primaria MMG, PLS, CA Medici Convenzionati con la ASM Elencati per Ambiti di Scelta Ambito : Accettura - Aliano - Cirigliano - Gorgoglione - San Mauro Forte - Stigliano 80 DEFINA/DOMENICA Accettura VIA IV NOVEMBRE 63 bis 63 bis 9930 SARUBBI/ANTONELLA STIGLIANO Corso Vittorio Emanuele II 45 308 SANTOMASSIMO/LUIGINA MIRIAM Aliano VIA DELLA VITTORIA 4 8794 MORMANDO/ANTONIO Cirigliano VIA FONTANA 8 8794 MORMANDO/ANTONIO Gorgoglione via DE Gasperi 30 3 BELMONTE/ROCCO San Mauro Forte VIA FRATELLI CATALANO 5 4374 MANDILE/FRANCESCO San Mauro Forte CORSO UMBERTO I 14 4242 CASTRONUOVO/ANTONIO Stigliano CORSO UMBERTO 57 8474 DIGILIO/MARGHERITA CARMELA Stigliano Corso Umberto I° 29 9382 DIRUGGIERO/MARGHERITA Stigliano Via Zanardelli 58 Ambito : Bernalda 9292 CALBI/MARISA Bernalda VIALE EUROPA - METAPONTO 10 9114 CARELLA/GIOVANNA Bernalda VIA DEL CONCILIO VATICANO II 35 8523 CLEMENTELLI/GREGORIO Bernalda CORSO UMBERTO 113 7468 GRIECO/ANGELA MARIA Bernalda VIALE BERLINGUER 15 7708 MATERI/ANNA MARIA Bernalda PIAZZA PLEBISCITO 4 9283 PADULA/PIETRO SALVATORE Bernalda VIA MONTESCAGLIOSO 28 9698 QUINTO/FRANCESCA IMMACOLATA Bernalda Via Nuova Camarda 24 4366 TATARANNO/RAFFAELE Bernalda CORSO UMBERTO 113 327 TOMASELLI/ISABELLA Bernalda CORSO UMBERTO 113 9918 VACCARO/ALMERINDO Bernalda CORSO UMBERTO 113 8659 VITTI/MARIA ANTONIETTA Bernalda VIA TRIESTE 14 Ambito : Calciano - Garaguso - Oliveto Lucano - Tricarico MEDICO INCARICATO Calciano DISTRETTO DI CALCIANO S.N.C. MEDICO INCARICATO Oliveto Lucano
    [Show full text]
  • Campania – Curiosando Nel Parco Del Matese
    SCHEDA PROGETTO PER L’IMPIEGO DI VOLONTARI IN SERVIZIO CIVILE IN ITALIA Unpli SCN cod. Accr. UNSC NZ01922 Ufficio per il Servizio Civile Nazionale Via Roma,21 - 83020 Contrada (Av) ENTE 1) Ente proponente il progetto: UNPLI NAZIONALE 2) Codice di accreditamento: EZ01922 3) Albo e classe di iscrizione: NAZIONALE 1 1 CARATTERISTICHE PROGETTO 4) Titolo del progetto: CURIOSANDO NEL PARCO DEL MATESE 5) Settore ed area di intervento del progetto con relativa codifica (vedi allegato 3): SETTORE: EDUCAZIONE E PROMOZIONE CULTURALE E-10 INTERVENTI DI ANIMAZIONE NEL TERRITORIO 6) Descrizione dell’area di intervento e del contesto territoriale entro il quale si realizza il progetto con riferimento a situazioni definite, rappresentate mediante indicatori misurabili; identificazione dei destinatari e dei beneficiari del progetto: PRESENTAZIONE DELL’ASSOCIAZIONE Questo progetto prevede un lavoro integrato tra le Pro Loco sedi di servizio civile della provincia di Caserta afferenti all’UNPLI, ente proponente del progetto. L’UNPLI è iscritta nel registro nazionale delle Associazioni di Promozione Sociale - legge 7 dicembre 2000, n.383, all’Albo nazionale del Servizio Civile Nazionale - Legge 6 marzo 2001, n. 64. ed è inoltre riconosciuta dalla Commissione Nazionale italiana per l’UNESCO quale Associazione che persegue con forte impegno, la promozione, la tutela e la valorizzazione del patrimonio culturale immateriale. Dell’Unione Pro Loco d’Italia oggi è ampiamente riconosciuto e valorizzato il ruolo sociale da parte del Ministero della Solidarietà Sociale, del Ministero dei Beni Culturali, da quello degli Interni e dalla Presidenza del Consiglio, con i quali intrattiene continui e fruttuosi rapporti di collaborazione. L’UNPLI conta oggi circa 600.000 soci suddivisi in più di 6.000 Pro Loco iscritte in tutta Italia, delle quali 101 registrate al 2017 nella sola provincia di Caserta.
    [Show full text]
  • Rankings Municipality of San Polo Matese
    9/27/2021 Maps, analysis and statistics about the resident population Demographic balance, population and familiy trends, age classes and average age, civil status and foreigners Skip Navigation Links ITALIA / Molise / Province of Campobasso / San Polo Matese Powered by Page 1 L'azienda Contatti Login Urbistat on Linkedin Adminstat logo DEMOGRAPHY ECONOMY RANKINGS SEARCH ITALIA Municipalities Powered by Page 2 Acquaviva Stroll up beside >> L'azienda Contatti Login Urbistat on Linkedin Collecroce Guglionesi Adminstat logo DEMOGRAPHY ECONOMY RANKINGS SEARCH Baranello JelsiITALIA Bojano Larino Bonefro Limosano Busso Lucito Campobasso Lupara Campochiaro Macchia Valfortore Campodipietra Mafalda Campolieto Matrice Campomarino Mirabello Casacalenda Sannitico Casalciprano Molise Castelbottaccio Monacilioni Castellino del Montagano Biferno Montecilfone Castelmauro Montefalcone Castropignano nel Sannio Cercemaggiore Montelongo Cercepiccola Montemitro Civitacampomarano Montenero di Colle d'Anchise Bisaccia Colletorto Montorio nei Duronia Frentani Ferrazzano Morrone del Fossalto Sannio Gambatesa Oratino Gildone Palata Guardialfiera Petacciato Guardiaregia Petrella Tifernina Pietracatella Pietracupa Portocannone Provvidenti Riccia Ripabottoni Powered by Page 3 Ripalimosani L'azienda Contatti Login Urbistat on Linkedin Provinces Roccavivara Adminstat logo DEMOGRAPHY ECONOMY RANKINGS SEARCH Rotello CAMPOBASSOITALIA Salcito ISERNIA San Biase San Felice del Molise San Giacomo degli Schiavoni San Giovanni in Galdo San Giuliano del Sannio San Giuliano di
    [Show full text]
  • The Unification of Italy
    New Dorp High School Social Studies Department AP Global Mr. Hubbs & Mrs. Zoleo The Unification of Italy While nationalism destroyed empires, it also built nations. Italy was one of the countries to form from the territories of the crumbling empires. After the Congress of Vienna in 1815, Austria ruled the Italian provinces of Venetia and Lombardy in the north, and several small states. In the south, the Spanish Bourbon family ruled the Kingdom of the Two Sicilies. Nevertheless, between 1815 and 1848, increasing numbers of Italians were no longer content to live under foreign rulers. Amid growing discontent, two leaders appeared—one was idealistic, the other practical. They had different personalities and pursued different goals. But each contributed to the Unification of Italy. The Movement for Unity Begins In 1832, an idealistic 26-year-old Italian named Guiseppe Mazzini organized a nationalist group called, Young Italy. Similarly, youth were the leaders and custodians of the nineteenth century nationalist movements. The Napoleonic Wars were lead principally by younger men. Napoleon was 35 years of age when crowned Emperor. As nationalism spread across Europe the pattern continued. People over 40 were excluded from Mazzini's organization. During the violent year of 1848, revolts broke out in eight states on the Italian Peninsula. Mazzini briefly headed a republican government in Rome. He believed that nation-states were the best hope for social justice, democracy, and peace in Europe. However, the 1848 rebellions failed in Italy as they did elsewhere in Europe. The foreign rulers of the Italian states drove Mazzini and other nationalist leaders into exile.
    [Show full text]
  • University of Groningen Hellenistic Rural Settlement and the City of Thurii, the Survey Evidence (Sibaritide, Southern Italy) A
    CORE Metadata, citation and similar papers at core.ac.uk Provided by University of Groningen University of Groningen Hellenistic Rural Settlement and the City of Thurii, the survey evidence (Sibaritide, southern Italy) Attema, Peter; Oome, Neeltje Published in: Palaeohistoria DOI: 10.21827/5beab05419ccd IMPORTANT NOTE: You are advised to consult the publisher's version (publisher's PDF) if you wish to cite from it. Please check the document version below. Document Version Publisher's PDF, also known as Version of record Publication date: 2018 Link to publication in University of Groningen/UMCG research database Citation for published version (APA): Attema, P., & Oome, N. (2018). Hellenistic Rural Settlement and the City of Thurii, the survey evidence (Sibaritide, southern Italy). Palaeohistoria, 59/60, 135-166. https://doi.org/10.21827/5beab05419ccd Copyright Other than for strictly personal use, it is not permitted to download or to forward/distribute the text or part of it without the consent of the author(s) and/or copyright holder(s), unless the work is under an open content license (like Creative Commons). Take-down policy If you believe that this document breaches copyright please contact us providing details, and we will remove access to the work immediately and investigate your claim. Downloaded from the University of Groningen/UMCG research database (Pure): http://www.rug.nl/research/portal. For technical reasons the number of authors shown on this cover page is limited to 10 maximum. Download date: 13-11-2019 PALAEOHISTORIA ACTA ET COMMUNICATIONES INSTITUTI ARCHAEOLOGICI UNIVERSITATIS GRONINGANAE 59/60 (2017/2018) University of Groningen / Groningen Institute of Archaeology & Barkhuis Groningen 2018 Editorial staff P.A.J.
    [Show full text]
  • Coastal Ocean Forecasting with an Unstructured Grid Model in the Southern Adriatic and Northern Ionian Seas
    Nat. Hazards Earth Syst. Sci., 17, 45–59, 2017 www.nat-hazards-earth-syst-sci.net/17/45/2017/ doi:10.5194/nhess-17-45-2017 © Author(s) 2017. CC Attribution 3.0 License. Coastal ocean forecasting with an unstructured grid model in the southern Adriatic and northern Ionian seas Ivan Federico1, Nadia Pinardi1,2,3, Giovanni Coppini1, Paolo Oddo2,a, Rita Lecci1, and Michele Mossa4 1Centro Euro-Mediterraneo sui Cambiamenti Climatici – Ocean Predictions and Applications, via Augusto Imperatore 16, 73100 Lecce, Italy 2Istituto Nazionale di Geofisica e Vulcanologia, Via Donato Creti 12, 40100 Bologna, Italy 3Universitá degli Studi di Bologna, viale Berti-Pichat, 40126 Bologna, Italy 4Dipartimento di Ingegneria Civile, Ambientale, del Territorio, Edile e di Chimica, Politecnico di Bari, Via E. Orabona 4, 70125 Bari, Italy anow at: NATO Science and Technology Organisation – Centre for Maritime Research and Experimentation, Viale San Bartolomeo 400, 19126 La Spezia, Italy Correspondence to: Ivan Federico ([email protected]) Received: 13 May 2016 – Published in Nat. Hazards Earth Syst. Sci. Discuss.: 25 May 2016 Accepted: 6 December 2016 – Published: 11 January 2017 Abstract. SANIFS (Southern Adriatic Northern Ionian ternative datasets at different horizontal resolution (12.5 and coastal Forecasting System) is a coastal-ocean operational 6.5 km). system based on the unstructured grid finite-element three- The SANIFS forecasts at a lead time of 1 day were com- dimensional hydrodynamic SHYFEM model, providing pared with the MFS forecasts, highlighting that SANIFS is short-term forecasts. The operational chain is based on a able to retain the large-scale dynamics of MFS.
    [Show full text]
  • The 2013–2018 Matese and Beneventano Seismic Sequences (Central–Southern Apennines): New Constraints on the Hypocentral Depth Determination
    geosciences Article The 2013–2018 Matese and Beneventano Seismic Sequences (Central–Southern Apennines): New Constraints on the Hypocentral Depth Determination Brando Trionfera 1, Alberto Frepoli 2,*, Gaetano De Luca 2, Pasquale De Gori 2 and Carlo Doglioni 1,2 1 Dipartimento Scienze della Terra, Università La Sapienza, 00185 Roma, Italy; [email protected] (B.T.); [email protected] (C.D.) 2 Istituto Nazionale di Geofisica e Vulcanologia, Osservatorio Nazionale Terremoti, 00185 Roma, Italy; [email protected] (G.D.L.); [email protected] (P.D.G.) * Correspondence: [email protected] Received: 19 November 2019; Accepted: 24 December 2019; Published: 30 December 2019 Abstract: The Matese and Beneventano areas coincide with the transition from the central to the southern Apennines and are characterized by both SW- and NE-dipping normal faulting seismogenic structures, responsible for the large historical earthquakes. We studied the Matese and Beneventano seismicity by means of high-precision locations of earthquakes spanning from 29 December 2013 to 4 September 2018. Events were located by using all of the available data from temporary and permanent stations in the area and a 1D computed velocity model, inverting the dataset with the Velest code. For events M > 2.8 we used P- and S-waves arrival times of the strong motion stations located in the study area. A constant value of 1.83 for Vp/Vs was computed with a modified Wadati method. The dataset consists of 2378 earthquakes, 18,715 P- and 12,295 S-wave arrival times. We computed 55 new fault plane solutions. The mechanisms show predominantly normal fault movements, with T-axis trends oriented NE–SW.
    [Show full text]
  • Progetto CARG Per Il Servizio Geologico D’Italia - ISPRA: F
    I S P R A Istituto Superiore per la Protezione e la Ricerca Ambientale SERVIZIO GEOLOGICO D’ITALIA Organo Cartografi co dello Stato (legge n°68 del 2.2.1960) NOTE ILLUSTRATIVE della CARTA GEOLOGICA D’ITALIA alla scala 1:50.000 foglio 450 SANT’ANGELO DEI LOMBARDI A cura di: T. S. Pescatore1†, F. Pinto1 Con contributi di: P. Galli2 (Sismicità e Strutture Sismogeniche) S. I. Giano3 (Geologia del Quaternario e Geomorfologia) R. Quarantiello1 (Geologia Applicata) M. Schiattarella3 (Tettonica e Morfotettonica) PROGETTORedazione scientifica: M.L. Putignano4 1 Dipartimento di Scienze per la Biologia, Geologia e l’Ambiente, Università degli Studi del Sannio - Benevento 2 Dipartimento di Protezione Civile Nazionale - Roma 3 Dipartimento Scienze Geologiche, Università degli Studi della Basilicata - Potenza 4 Istituto di Geologia Ambientali e Geoingegneria - IGAG - CNR - RomaCARG CNR Ente realizzatore: Consiglio Nazionale delle Ricerche NoteIllustrative F450_S.Angelo dei Lomabardi_17_01_2020_cc.indd 1 17/01/2020 16:20:53 Direttore del Servizio Geologico d’Italia - ISPRA: C. Campobasso Responsabile del Progetto CARG per il Servizio Geologico d’Italia - ISPRA: F. Galluzzo Responsabile del Progetto CARG per il CNR: R. Polino (IGG), fino al 2009, P. Messina (IGAG) Gestione operativa del Progetto CARG per il Servizio Geologico d’Italia - ISPRA: M.T. Lettieri per il Consiglo Nazionale delle Ricerche - CNR: P. Messina (IGAG) PER IL SERVIZIO GEOLOGICO D’ITALIA - ISPRA: Revisione scientifica: R. Di Stefano (†), A. Fiorentino, F. Papasodaro, P. Perini Coordinamento cartografico: D. Tacchia (coord.), S. Grossi Revisione informatizzazione dei dati geologici: L. Battaglini, R. Carta, A. Fiorentino (ASC) Coordinamento editoriale: D. Tacchia (coord.), S. Grossi PER IL CONSIGLIO NAZIONALE DELLE RICERCHE: Funz.
    [Show full text]