Presentazione Bolsena Living Lakes Calvario
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3.1 – Presenza Di Aree a Rischio Idrogeologico in Attuazione Della
3.1 – Presenza di aree a rischio idrogeologico In attuazione della Legge 183/89 è stato emanato il D.L. n. 180 dell’11 giugno 1998 (Decreto Sarno) con la finalità di individuare le aree a più elevato rischio idrogeologico e di adottare idonee misure di salvaguardia e prevenzione. La difesa del suolo diviene in tal modo, se pur sulla base della emotività scatenata dalla tragedia di Sarno, una attività preventiva e non, come in precedenza, riparativa di danni ormai avvenuti sul territorio. Lo stesso decreto fu convertito con modificazioni dalla legge n. 267 del 3 agosto 1998 e promulgato il D.P.C.M 29 settembre 1998 per la individuazione dei criteri relativi agli adempimenti da compiere in merito alla perimetrazione delle aree esposte a diversi livelli di rischio. Esso traccia, inoltre, la fase di programmazione della mitigazione del rischio attraverso elaborazioni, anche grafiche tali da individuare le tipologie di interventi da realizzare per mitigare o rimuovere lo stato di rischio. In attesa di un riordino successivo all’entrata in vigore del nuovo Decreto legislativo 152/2006 si riportano le strategie di intervento fino ad oggi attuate per quanto riguarda la difesa del suolo. Esse si inquadrano nell’ambito della pianificazione di bacino che le 5 Autorità di bacino competenti sul territorio regionale (Tevere, Liri-Garigliano, Fiora, Tronto, Bacini regionali) elaborano ed approvano. Lo strumento pianificatorio attualmente approvato e vigente su tutto il territorio regionale è il Piano Straordinario per l’Assetto Idrogeologico (PSAI). Le Autorità di Bacino che interessano il territorio provinciale sono tre, di seguito si riportano i dati salienti (Tab. -
'Truth': Representations of Intercultural 'Translations'
eScholarship California Italian Studies Title Sleights of Hand: Black Skin and Curzio Malaparte's La pelle Permalink https://escholarship.org/uc/item/0xr9d2gm Journal California Italian Studies, 3(1) Author Escolar, Marisa Publication Date 2012 DOI 10.5070/C331012084 Peer reviewed eScholarship.org Powered by the California Digital Library University of California Sleights of Hand: Black Fingers and Curzio Malaparte’s La pelle Marisa Escolar La pelle [1949], written towards the end of Curzio Malaparte’s rather colorful political career,1 has long been used as a litmus test for its author, helping critics confirm their belief in a range of divergent and often contradictory interpretations. At one end of the spectrum is the view that he was an unscrupulous “chameleon” who distorted the reality of the Allies’ Liberation of Italy to suit his own interests.2 At the other is the claim that he was a true artist whose representations of the horrors of war absorb historical details into what is a consummately literary work.3 In other words, La pelle has been read either as a vulgar deformation or a poetic transcendence of the historical moment it purports to represent.4 And yet Malaparte’s narrative of the myriad social transformations following the Armistice actually combines concrete historical events (the Allies’ arrival in Naples and in Rome, the eruption of Vesuvius on March 22, 1944, and the battle of 1 Malaparte, born Kurt Erich Suckert, joined the Partito Nazionale Fascista in September 1922 and resigned in January, 1931 just before moving to France. Upon his return to Italy in October 1931, he was expelled from the party (despite having already left it) and sentenced to political exile on Lipari for five years of which he served less than two (Martellini Opere scelte xcii-xciv). -
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. -
Path to Rome Walk May 8 to 20, 2018
Path to Rome Walk May 8 to 20, 2018 “A delight—great food and wine, beautiful countryside, lovely hotels and congenial fellow travelers with whom to enjoy it all.” —Alison Anderson, Italian Lakes Walk, 2016 RAVEL a portion of the Via Francigena, the pilgrimage route that linked T Canterbury to Rome in the Middle Ages, following its route north of Rome through olive groves, vineyards and ancient cypress trees. Discover the pleasures of Central Italy’s lesser-known cities, such as Buonconvento, Bolsena, Caprarola and Calcata. With professor of humanities Elaine Treharne as our faculty leader and Peter Watson as our guide, we refresh our minds, bodies and souls on our walks, during which we stop to picnic on hearty agrarian cuisine and enjoy the peace and quiet that are hallmarks of these beautiful rural settings. At the end of our meanderings, descend from the hills of Rome via Viale Angelico to arrive at St. Peter’s Basilica, the seat of Catholicism and home to a vast store of art treasures, including the Sistine Chapel. Join us! Faculty Leader Professor Elaine Treharne joined the Stanford faculty in 2012 in the School of Humanities and Sciences as a Professor of English. She is also the director of the Center for Spatial and Textual Analysis. Her main research focuses on early medieval manuscripts, Old and Middle English religious poetry and prose, and the history of handwriting. Included in that research is her current project, which looks at the materiality of textual objects, together with the patterns that emerge in the long history of text technologies, from the earliest times (circa 70,000 B.C.E.) to the present day. -
First Premarital Screening of Thalassaemia Carriers in Intermediate Schools in Latium
Journal ofMedical Genetics, 1978, 15, 202-207J Med Genet: first published as 10.1136/jmg.15.3.202 on 1 June 1978. Downloaded from First premarital screening of thalassaemia carriers in intermediate schools in Latium E. SILVESTRONI, I. BIANCO, B. GRAZIANI, C. CARBONI, AND S. U. D'ARCA From the 'Centro di Studi-della Microcitemia di Roma% Istituto d'Igiene dell'Universitd di Roma, Italia SUMMARY In the 1975 to 1976 school year, under the auspices of the Health Authorities of the Latium Region, the Rome Microcythaemia Centre carried out for the first time a partial screening survey of thalassaemia carriers among the students of the compulsory intermediate school in Latium. This work was the beginning of a new preventive school health service aimed at the prophylaxis of Cooley's disease. In 23 places investigated in Latium, 17 724 students were examined, 13 354 of whom were in Rome and 4370 elsewhere. The mean percentage of co-operation was 70% and the mean percentage of thalassaemia 2.42%. Thalassaemic students were invited to attend the centre for a check-up along with their families: about half had already come in by the end of June 1976. All students examined, whether normal or thalassaemic, have received written results of the tests. The screening survey aroused notable interest and obtained wide approval both at school and at home. The news of being thalassaemia carriers, even if not welcome, was never the cause of family tragedy. copyright. Under the auspices of and with financial support from Informed consent having been obtained, a team of the Health Authorities of the Latium Region, the doctors took 1 ml venous blood from each student in Rome Microcythaemia Centre initiated and carried out the school dispensary. -
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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. -
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. -
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.