1 Descrizione Del Territorio Della Provincia Di Viterbo
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Download Download
EQA – Environmental quality / Qualité de l’Environnement / Qualità ambientale, 24 (2017) 39-45 PRELIMINARY EVIDENCES OF A PALEOSOL IN THE LIVING LANDSCAPE OF CIVITA DI BAGNOREGIO (ITALY) Sara Marinari (1)*, Maria Cristina Moscatelli (1) , Flavia Fiordelmondo (1) , Rosita Marabottini (1) , Giovanni Maria Di Buduo (2) , Gilmo Vianello (3) (1) Dipartimento per l’innovazione dei sistemi Biologici, Agroalimentari e Forestali, Università degli Studi della Tuscia, Viterbo (2) Museo Geologico e delle Frane, Civita di Bagnoregio, Viterbo (3) Dipartimento di Scienze Agrarie, Alma Mater Studiorum Università di Bologna Corresponding author Email: [email protected] Abstract A paleosol has been identified in an area of great natural interest for its geomorphologic and naturalistic aspects between the municipalities of Bagnoregio and Castiglione in Teverina (Viterbo, Italy). This investigation represents the preliminary steps of a study aimed to know the specific environmental features and dynamics prior to the eruptions of the "nenfri" of the Paleovulsini complex. The physico-chemical characteristics and some horizons morphological details such as the presence of roots fingerprint, the polyhedric angular and columnar structure suggest incipient weathering and pedogenesis. Moreover, the presence of nodules and the high salinity of deep horizons suggest the incorporation of pyroclastic material into a hydromorphic environment at the time of the eruptions, putting forward the hypothesis of a paleo-marsh under an arid paleoclimate. Keywords: paleosol, pyroclastic material, microbiological analysis, Civita di Bagnoregio Introduction A paleosol has been identified in an area of great natural interest for its geomorphologic and naturalistic aspects between the municipalities of Bagnoregio and Castiglione in Teverina (northern Lazio, bordering Umbria). Particular attention is given to landslides and erosive events repetition that affect both the cliff on which Civita rises and the adjacent "Valle dei Calanchi" (Fig. -
4 International Workshop on Collapse Calderas September 23-29, 2012
4th International Workshop on Collapse Calderas September 23-29, 2012, Vulsini Calderas, Italy Second Circular - http://www.gvb-csic.es/CCC.htm Organizers: Valerio Acocella; Roma Tre, Roma, Italy; [email protected] Adelina Geyer; CSIC, Barcelona, Spain; [email protected] Danilo M. Palladino; La Sapienza, Roma, Italy; [email protected] Scientific Committee: Valerio Acocella, Univ. Roma Tre, Italy. Gerardo J. Aguirre-Díaz; UNAM, Queretaro, Mexico. Jim Cole; Univ. Canterbury, Christchurch, New Zealand. Adelina Geyer; CSIC, Barcelona, Spain. Agust Gudmundsson; Univ. Royal Holloway, London, England. Peter W. Lipman; USGS, Menlo Park, USA. Joan Martí; CSIC, Barcelona, Spain. Geshi Nobuo; Geological Survey, Ibaraki, Japan. Stephen Self; Open University, UK/US-NRC. Roberto Sulpizio; Univ. Bari, Italy. Danilo M. Palladino; Univ. La Sapienza Roma, Italy. 1 2 What is the Workshop on Collapse Calderas? The IAVCEI Collapse Calderas Commission (CCC; http://www.gvb-csic.es/CCC.htm) was created in 2008 to have a wider and deeper understanding on calderas. It includes caldera geology, geodesy and geophysics, modelling, magma chamber processes, volcanic hazard and risk management, economic benefits and environmental research. CCC promotes interdisciplinary interaction to help solve the many questions regarding the formation, evolution and affect on society of collapse calderas. Previous meetings were held at Tenerife, Canarias, (2005), Mexican Volcanic Belt (2008) and Reunion (2010). Venue The 4th Workshop on Collapse Calderas is scheduled for September 23-29, 2012, at Hotel Royal in Bolsena, Central Italy. Bolsena is a medieval village on the edge of Bolsena Caldera, that is the most distinctive feature of the Vulsini Calderas District, 100 km north of Rome. -
The Routes of Taste
THE ROUTES OF TASTE Journey to discover food and wine products in Rome with the Contribution THE ROUTES OF TASTE Journey to discover food and wine products in Rome with the Contribution The routes of taste ______________________________________ The project “Il Camino del Cibo” was realized with the contribution of the Rome Chamber of Commerce A special thanks for the collaboration to: Hotel Eden Hotel Rome Cavalieri, a Waldorf Astoria Hotel Hotel St. Regis Rome Hotel Hassler This guide was completed in December 2020 The routes of taste Index Introduction 7 Typical traditional food products and quality marks 9 A. Fruit and vegetables, legumes and cereals 10 B. Fish, seafood and derivatives 18 C. Meat and cold cuts 19 D. Dairy products and cheeses 27 E. Fresh pasta, pastry and bakery products 32 F. Olive oil 46 G. Animal products 48 H. Soft drinks, spirits and liqueurs 48 I. Wine 49 Selection of the best traditional food producers 59 Food itineraries and recipes 71 Food itineraries 72 Recipes 78 Glossary 84 Sources 86 with the Contribution The routes of taste The routes of taste - Introduction Introduction Strengthening the ability to promote local production abroad from a system and network point of view can constitute the backbone of a territorial marketing plan that starts from its production potential, involving all the players in the supply chain. It is therefore a question of developing an "ecosystem" made up of hospitality, services, products, experiences, a “unicum” in which the global market can express great interest, increasingly adding to the paradigms of the past the new ones made possible by digitization. -
Volcanic Rocks from Central Italy: an Oxygen Isotopic Microanalytical and Geochemical Study
Volcanic Rocks from Central Italy: An Oxygen Isotopic Microanalytical and Geochemical Study Dissertation zur Erlangung des Doktorgrades der Mathematisch-Naturwissenschaftlichen Fakultäten der Georg-August-Universität zu Göttingen vorgelegt von Peter Barnekow aus Bremen Göttingen 2000 D 7 Referent: Prof. Dr. J. Hoefs Korreferent: Prof. Dr. S.F. Foley Tag der mündlichen Prüfung: 30. Oktober 2000 Table of Contents Table of Contents ,QWURGXFWLRQ BBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBB 1.1 General Charakteristics of the Tertiary to Quarternary Italian Magmatic Rocks .........1 1.2 Magmatic Provinces in Italy.........................................................................................2 1.3 Overview of the Different Genetic Models ..................................................................3 1.4 Investigated Area and Petrogenetic Subdivision ..........................................................6 1.5 Oxygen Isotopes ...........................................................................................................7 6DPSOH'HVFULSWLRQ BBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBBB 2.1 Sampling.......................................................................................................................9 2.2 Geological and Petrographical Description of the Samples .......................................10 2.2.1 Monti Vulsini – Roman Province Type Rocks...........................................................10 2.2.2 Orciatico and Montecatini Val di Cecina – Lamproites .............................................11 -
Tuscia Economica
Tuscia Economica Supplemento al Mensile informativo edito dalla Camera di Commercio di Viterbo Direttore responsabile Franco Rosati Autorizzazione del tribunale di Viterbo n. 2 del 27-3-1948 via Fratelli Rosselli 4, tel. 0761 2341, fax 0761 345755, www.vt.camcom.it numero 2, Luglio-Dicembre 2007 TUSCIA ECONOMICA periodico a cura della Camera di Commercio, Indice Industria, Artigianato e Agricoltura di Viterbo Direttore responsabile Dott. Franco Rosati Supplemento al n. 12/2007 1 Studio di impatto socio-economico Le opinioni espresse nei singoli articoli non im- sullo sviluppo dell’aeroporto pegnano la Direzione. È vietata la riproduzione anche parziale del te- di Viterbo pag. 05 sto e delle illustrazioni senza citarne la fonte. Per riproduzione a puntate è obbligo ripetere la 2 La CSR nelle Pmi: opportunità citazione. di marketing o realtà lontana? Un’indagine empirica pag. 11 Autorizzazione del Tribunale di Viterbo n. 2 del 27-3-1948 Stampato presso la Tipografia Agnesotti - Viterbo 3 Progetto Valle Faul. Storia del luogo, risanamento e conservazione del paesaggio pag. 25 4 Stili di vita, performance fisica e consumo di prodotti tipici locali nella popolazione anziana dell’Alta Tuscia pag. 39 5 Appendice Statistica pag. 49 Presidente: - PALOMBELLA Ferindo Vice Presidente: - PEPPONI Roberto Giunta Camerale - BOCCOLINI Franco - CORETTI Petronio - GIULIANI Marco - MESCHINI Adalberto - PELOSI Massimo - PEPARELLO Vincenzo - TARDANI Giacobbe Segretario Generale - ROSATI Franco Collegio dei Revisori dei Conti: - ROMEO Teresa (Presidente) - CIMA -
Volcano-Tectonic Deformation in the Monti Sabatini Volcanic District At
Volcano-tectonic deformation in the Monti Sabatini Volcanic District at the gates of Rome (central Italy): evidence from new geochronologic constraints on the Tiber River MIS 5 terraces F. Marra, F. Florindo, Brian R. Jicha, S. Nomade, D.M. Palladino, A. Pereira, G. Sottili, C. Tolomei To cite this version: F. Marra, F. Florindo, Brian R. Jicha, S. Nomade, D.M. Palladino, et al.. Volcano-tectonic deforma- tion in the Monti Sabatini Volcanic District at the gates of Rome (central Italy): evidence from new geochronologic constraints on the Tiber River MIS 5 terraces. Scientific Reports, Nature Publishing Group, 2019, 9 (1), 10.1038/s41598-019-47585-8. hal-02973727 HAL Id: hal-02973727 https://hal.archives-ouvertes.fr/hal-02973727 Submitted on 26 Oct 2020 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. www.nature.com/scientificreports OPEN Volcano-tectonic deformation in the Monti Sabatini Volcanic District at the gates of Rome (central Italy): Received: 13 February 2019 Accepted: 12 July 2019 evidence from new geochronologic Published: xx xx xxxx constraints on the Tiber River MIS 5 terraces F. Marra1, F. Florindo1, B. R. Jicha2, S. -
Formation Conditions of Leucite-Bearing Lavas in the Bolsena Complex (Vulsini, Italy): Research Data on Melt Inclusions in Minerals
Russian Geology and Geophysics © 2019, V.S. Sobolev IGM, Siberian Branch of the RAS Vol. 60, No. 2, pp. 119–132, 2019 DOI:10.15372/RGG2019009 Geologiya i Geofizika Formation Conditions of Leucite-Bearing Lavas in the Bolsena Complex (Vulsini, Italy): Research Data on Melt Inclusions in Minerals A.T. Isakovaa,, L.I. Paninaa, F. Stoppab a V.S. Sobolev Institute of Geology and Mineralogy, Siberian Branch of the Russian Academy of Sciences, pr. Akademika Koptyuga 3, Novosibirsk, 630090, Russia b Dipartimento di Scienze DiSPUTer, Universita degli Studi G. d’Annunzio, via dei Vestini 30, Chieti Scalo (CH), 66100, Italy Received 29 June 2017; received in revised form 9 November 2017; accepted 15 June 2018 Abstract—A melt inclusion study was carried out in the leucite-bearing tephriphonolite and phonolite lavas of the Bolsena complex in order to obtain direct data on the chemical composition of initial melts, their evolution, and their crystallization temperatures. It has been found that the initial melt for the considered rocks was of tephrite–basanite composition. Its crystallization began with the formation of clinopyroxene phenocrysts at 1205–1100 °C, then leucite and plagioclase crystallization took place at about 1120 °C and 1080–1060 °C, respectively. The initial tephrite–basanite melt was slightly enriched in volatile components (H2O, F, SO3, and Cl). During the crystalliza- tion of clinopyroxene, leucite, and plagioclase, the composition of the initial magma changed toward an increase in the contents of SiO2, Al2O3, and K2O and a decrease in the contents of FeO, MgO, and CaO, i.e., evolved toward phonolite. A similar evolution trend is typical of alkaline basic systems. -
Volume 16 Winter 2014
Volume 16 Winter 2014 Tomb 6423 At right, the Below is the A Digger’s View: lastra sealing chamber as The Tomb of the Hanging the chamber found at the The perspective of a field Aryballos, Tarquinia shown in situ. moment of archaeologist by Alessandro Mandolesi Above it is the opening, by Maria Rosa Lucidi another lastra on the back The University of Turin and the possibly reut- wall a little The discovery of the tomb of the Superintendency for the Archaeological ilzed spolia aryballos still “hanging aryballos" has aroused great Heritage of Southern Etruria have been interest among the public in both Italy taken from hangs on its investigating the Tumulus of the Queen and internationally. The integrity of the original nail. and the necropolis surrounding it, the the tumulus unviolated tomb is definitely one of the Doganaccia, since 2008. The excava- of the queen, (photographs reasons for the attention it has received. tions have brought forth many important which stands by Massimo The uniqueness is even more pro- and unexpected results, thanks to subse- nearby. Legni). nounced when one considers that since quent research, and the infor- the second half of the nine- mation relating to the differ- teenth century the English ent phases of its use has made traveler George Dennis it possible to clarify many blamed the inability to recov- obscure points about the great er the contexts from intact era of the monumental tumuli chamber tombs in Etruscan at Tarquinia. Tarquinia on repeated looting Archaeologists working since ancient times. The -
PIANO DI GESTIONE DEL Psic/ZPS “MONTI VULSINI” (IT 6010008)
Provincia di Viterbo PIANO DI GESTIONE DEL pSIC/ZPS “MONTI VULSINI” (IT 6010008) SSSTTTUUUDDDIIIOOO GGGEEENNNEEERRRAAALLLEEE Settembre 2004 Lynx Natura e Ambiente s.r.l. PIANO DI GESTIONE DEL PSIC/ZPS “MONTI VULSINI - IT 6010008” PARTE I – STUDIO GENERALE INDICE 1. PREMESSA..............................................................................................................5 2. INTRODUZIONE.......................................................................................................7 2.1. DESCRIZIONE GENERALE DEL SITO .........................................................................7 2.2. QUADRO DI RIFERIMENTO NORMATIVO ....................................................................7 2.3. METODOLOGIA .....................................................................................................9 2.3.1. Articolazione dello Studio Generale .................................................................................. 10 2.3.2. Articolazione del Piano di Gestione .................................................................................. 11 3. CARATTERIZZAZIONE TERRITORIALE ED ABIOTICA DEL SITO ....................14 3.1. LOCALIZZAZIONE DEL SITO...................................................................................14 3.2. VINCOLI NATURALISTICI ESISTENTI........................................................................14 3.3. GEOLOGIA .........................................................................................................14 3.3.1. Indice di franosità ............................................................................................................. -
Sulle Orme Di Goethe Nella Tuscia Vista Da Viaggiatori Tedeschi Fra Sei E Settecento
Sulle orme di Goethe nella Tuscia CLAUS RIESSNER vista da viaggiatori tedeschi fra Sei e Settecento. iamo informati fin nei mini- scritte da Roma quasi quotidia- Via Cassia fino a Firenze, dove i Smi dettagli sull'itinerario namente il suo stato d'animo dal due si fermarono quasi quindici seguito da Goethe durante il suo primo giorno del suo arrivo in giorni, per proseguire poi via viaggio in Italia (settembre 1786 città (la sera del 29 ottobre Bologna, Parma, Milano (con - giugno 1788) che lo portò 1786) fino al momento della sua altre brevi soste di pochi giorni), prima a Roma, successivamente partenza definitiva così doloro- per Coira e il Passo dello Spluga a Napoli e da lì via mare fino in samente sentita, egli è sorpren- fino al Lago di Costanza. Sicilia. Dagli appunti del diario dentemente scarso di parole Goethe non ha tenuto un dia- tenuto dal poeta e dalla redazio- circa la progettata via del suo rio durante il viaggio di ritorno ne finale della Italienische ritorno in patria. In una lettera (a prescindere da una serie di Reise, stampata per la prima del 2 aprile 1788 al duca di lettere e da sporadici appunti e volta negli anni 1816-18171 Weimar, Carl August, annuncia schizzi, prevalentemente d'argo- conosciamo inoltre il motivo per semplicemente la sua partenza mento botanico, raccolti in una cui ha deciso, dopo una sosta di per i prossimi quindici giorni, specie di taccuino), ma in ricom- poche ore a Firenze, di non pro- pregando di indirizzare a pensa ci resta la testimonianza seguire il suo viaggio sulla Via Firenze le lettere destinate a lui, di una quarantina di disegni, Cassia attraverso la Toscana, e nell'ultima lettera scritta a soprattutto di paesaggi, dai quali come usava fare la maggior Roma il 19 aprile dice che “1a possiamo tirare certe conclusio- parte dei viaggiatori stranieri a partenza è fissata al 22 o 23 ni riguardo a circostanze che quel tempo. -
Seismicity and Velocity Images of the Roman Magmatic Province
Chiarabba et al. SEISMICITY AND VELOCITY IMAGES OF THE ROMAN MAGMATIC PROVINCE Claudio Chiarabba Alessandro Amato and Adolfo Fiordelisi * Istituto Nazionale di Geofisica, * Ente Nazionale Energia Elettrica ABSTRACT 2. METHOD Seismic tomography provides velocity images of the crust Arrival times of body waves at a seismic network contain beneath Quaternary volcanoes and geothermal areas with a detail information about the velocity structure sampled by the seismic of 1-4 km. We describe the three-dimensional P-wave velocity ray paths. Local earthquake tomography yields the three- structure of the upper crust beneath the adjacent Amiata and dimensional velocity structure (defined as a discrete series of Vulsini Geothermal Regions, and beneath the Alban Hills parameters) by inverting P- and S-wave arrival times at a dense Volcano (Central Italy), obtained by inverting local earthquake local array (Thurber, 1983). We used the method developed by arrival times. In the three study areas, we find high-velocity Thurber ( 1983) and successively modified by Eberhart-Phillips anomalies in the upper km of the crust revealing the presence (1986). The crustal model is defined specifying the velocity of uplifted limestone units (metamorphosed at depth). The 3-D values at the nodes of a three-dimensional grid (in our case, grid geometry of the limestone units (the main geothermal reservoir in spacing is 4 km horizontally for the Amiata-Vulsini region, and 2 the region) is clearly defined by the three-dimensional velocity km for the Alban Hills). This technique consists of a pattern. Negative anomalies at 1 and 3 km depth identify Plio- simultaneous inversion of data to obtain both velocity parameters Quaternary depressed structures, filled with low velocity clayey and earthquake location. -
Ampelographic and DNA Characterization of Local Grapevine Accessions of the Tuscia Area (Latium, Italy)
Research Note Ampelographic and DNA Characterization of Local Grapevine Accessions of the Tuscia Area (Latium, Italy) Massimo Muganu , l * Gerald Dangl,2 Maui Aradhya,3 Manuela Frediani,4 Angela Scossa, 1 and Ed Stover' Abstract: The presence of local vines in the Tuscia area (Latium region, Italy) was documented by historical sources. Ampelographic and molecular characterization (35 morphological descriptors and 16 microsatellite loci) was carried out on accessions belonging to the most frequently mentioned local vines. SSR markers have enabled us to distinguish cases of local synonymy and microsatellite profiles have permitted comparison with previously reported profiles indicating synonymy and divergence with vines in other collections. Ampelograpliic traits showed that some accessions of the same genotype differ in minor characteristics that can have a role in clonal evaluation. Key words: Vitis vinifera, germplasm, SSRs, grape quality The Latium region, situated in the center of Italy. has graphic studies described several vines that contained the a varied grape germplasm and a winemaking tradition name Greco (Bullettino ampelografico 1881). In the Mid- that predates the Roman civilization. In the Tuscia area dle Ages, greco was an adjective that referred to sweet of Latium (province of Viterbo), seeds of the cultivated and long-lived wine, with high alcohol, and well-known grape Vitis vinijera saliva date to the 10th century ac, in Tuseia (Lanconelli 1994). In the 19th century, Pagadeb- testifying to the antiquity of grape consumption and pro- ito (also called Rornanesco and Scassadehito in Tuscia) duction (Delpino 2005). Wines produced in the Tuscia was one of the most cultivated varieties in the area, very area were popular and well-known during the Middle productive, and yielding wine in quantity (Cinelli 1884).