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Aa Aa Unione Montana Valle Varaita
REGIONE PIEMONTE BU7 18/02/2021 Unione Montana Valle Varaita - Frassino (CN) Statuto Allegato UNIONE MONTANA VALLE VARAITA STATUTO UNIONE MONTANA DEI COMUNI DELLA VALLE VARAITA STATUTO Sommario TITOLO I ‐ ELEMENTI COSTITUTIVI ........................................................................................................................................................................3 Art. 1 ‐ Principi fondamentali ................................................................................................................................................................................3 Art. 2 – Denominazione e Sede..............................................................................................................................................................................3 Art. 3 – Finalità.............................................................................................................................................................................................................3 Art. 4 – Disposizioni per l’esercizio in forma associata delle funzioni e dei servizi........................................................................4 Art. 5 – Durata dell’Unione montana ..................................................................................................................................................................4 Art. 6 ‐ Scioglimento dell'Unione montana e recesso ..................................................................................................................................4 -
The Sand Lizard, Lacerta Ag/Lis, in Italy: Preliminary
SHORT NOTES 101 REFERENCES HERPETOLOGICAL JOURNAL, Vol. 2, pp. 101-103 (1992) Anonymous ( 1987). The flying death ofRa jputana - systematics of dan THE SAND LIZARD, LACERTA AG/LIS, gerously venomous snakes. In Report of the British Museum (Natural History), 1984- 1985. London: British Museum (Natural IN ITALY: PRELIMINARY DATA ON History). DISTRIBUTION AND HABITAT Harding, K. A., & Welch, K. R. G. ( 1980). Venomous snakes of the CHARACTERISTICS World. A checklist. Oxford: Pergamon Press. MASSIMO CAPULA AND LUCA LUISELLI Leviton, A. E. ( 1980). Museum acronyms -second edition. Herpetologica/ Review 11, 93- 102. Dipartimento di Biologia Animate e del/ ' Uomo, Universitii "la Sapienza " di Roma, Via Borelli 50, 00161 Roma, Italy Looareesuwan, S., Viravan, C. & Warrell, D. A. ( 1988). Factors contrib uting to fatal snake bite in the tropics: analysis of 46 cases in (Accepted 30. 1.91) Thailand. Transactions of the Royal Societ.v o.lTropical Medicine and Hygiene 82, 930-934. Lacerta agilis Linnaeus is a lacertid lizard whose wide range extends from NE Iberia and W France to central Asia through Myint-Lwin, Phillips, R. E., Tun-Pe, Warrell, D. A., Tin-Nu-Swe & Maung-Maung-Lay. ( 1985). Bites by Russell's viper (Vipera most of Europe. This species is rare or absent fromthe European russelli siamensis) in Burma: Haemostatic, vascular, and renal regions characterized by a Mediterranean climate, such as most disturbances and response to treatment. The lancet 2, 1259- of the Iberian Peninsula, the Italian Peninsula and S Balkans 1264. (Arnold & Burton, 1978; Jablokov, Baranow & Rozanow, 1980; Bischoff, 1984, 1988). The occurrence of the sand lizard Thorpe, R. -
Cottian Alps Geoparc
COTTIAN ALPS GEOPARC Discover more than a hundred geological sites which recount the different stages of the history of the Alps. Visit plenty of museums and mining sites (copper, silver, iron, coal, talc...) which tell the story of the exploitation of mineral resources by mankind since prehistory. http://cottianalps-geoparc.eu COTTIAN ALPS GEOPARC The geological history of the Alps The French-Italian Geoparc of the Cottian Alps illustrates the different periods of the region’s geological history, from the end of the Primary Era (more than 300 million years ago) up to the present day: - a single conti nent (Pangaea) - the creation and development of the alpine ocean - the convergence of European and African plates, the end of the ocean - the collision of the two plates and the creation of the Alps. Today the Alpine range is still alive. Seismic activity and uplift show active tectonic movements among plates. The progressive destruction of mountain relief by different erosional processes is anot her illustration of it. The Cottian Alps The Cottian Alps were an ancient imperial Roman province. Cottius, the Celto-Ligurian king who was allied to Rome, gave them his name. This part of the French-Italian Alps lies between the Graian Alps (to the north) and the Maritime Alps (to the south). To visit the Geoparc... Discover the sites and museums of the Geoparc by car, on foot or on a mountain bike, on your own or with a local guide. A general map and some useful information are available free of charge from the tourism offices and can be downloaded from the Geoparc website. -
Slope Instability and Flood Events in the Sangone Valley, Northwest Italian Alps
77 STUDIA GEOMORPHOLOGICA CARPATHO-BALCANICA Vol. XLIV, 2010: 77–112 PL ISSSN 0081-6434 LANDFORM EVOLUTION IN MOUNTAIN AREAS 1 1 1 MARCELLA BIDDOCCU , LAURA TURCONI , DOMENICO TROPEANO , 2 SUNIL KUMAR DE (TORINO) SLOPE INSTABILITY AND FLOOD EVENTS IN THE SANGONE VALLEY, NORTHWEST ITALIAN ALPS Abstract. Slope instability and streamflow processes in the mountainous part of the SanGone river basin have been investiGated in conjunction with their influence on relief remodellinG. ThrouGh histor- ical records, the most critical sites durinG extreme rainfalls have been evidenced, concerned natural parameters and their effects (impact on man-made structures) reiterated over space and time. The key issue of the work is the simulation of a volume of detrital materials, which miGht be set in motion by a debris flow. Two modellinG approaches have been tested and obtained results have been evaluated usinG Debris © (GEOSOFT s.a.s.) software. Simulation of debris flow in a small sub-catchment (Tauneri stream) was carried out and the thickness of sediment “packaGe” that could be removed was calculated in order to assess the debris flow hazard. The Turconi & Tropeano formula (2000) was applied to all the partitions of the SanGone basin in order to predict the whole sediment volume which miGht be delivered 3 to the main stream durinG an extreme event and the result beinG 117 m /hectare. Key words : landslip, torrential flood, debris flow, predictive model INTRODUCTION The Alpine valleys, throughout centuries, are in search of an equilibrium between anthropogenic activity and natural processes; interventions due to ameliorating productivity, accommodation and safety conditions for Man and environment often were done overlapping or contrasting the slowly-operating exogenous agents. -
Bumble Bees of the Susa Valley (Hymenoptera Apidae)
Bulletin of Insectology 63 (1): 137-152, 2010 ISSN 1721-8861 Bumble bees of the Susa Valley (Hymenoptera Apidae) Aulo MANINO, Augusto PATETTA, Giulia BOGLIETTI, Marco PORPORATO Di.Va.P.R.A. - Entomologia e Zoologia applicate all’Ambiente “Carlo Vidano”, Università di Torino, Grugliasco, Italy Abstract A survey of bumble bees (Bombus Latreille) of the Susa Valley was conducted at 124 locations between 340 and 3,130 m a.s.l. representative of the whole territory, which lies within the Cottian Central Alps, the Northern Cottian Alps, and the South-eastern Graian Alps. Altogether 1,102 specimens were collected and determined (180 queens, 227 males, and 695 workers) belonging to 30 species - two of which are represented by two subspecies - which account for 70% of those known in Italy, demonstrating the particular value of the area examined with regard to environmental quality and biodiversity. Bombus soroeensis (F.), Bombus me- somelas Gerstaecker, Bombus ruderarius (Mueller), Bombus monticola Smith, Bombus pratorum (L.), Bombus lucorum (L.), Bombus terrestris (L.), and Bombus lapidarius (L.) can be considered predominant, each one representing more than 5% of the collected specimens, 12 species are rather common (1-5% of specimens) and the remaining nine rare (less than 1%). A list of col- lected specimens with collection localities and dates is provided. To illustrate more clearly the altitudinal distribution of the dif- ferent species, the capture locations were grouped by altitude. 83.5% of the samples is also provided with data on the plant on which they were collected, comprising a total of 52 plant genera within 20 plant families. -
Fold Interference Pattern at the Top of Basement Domes and Apparent Vertical Extrusion of HP Rocks
Fold interference pattern at the top of basement domes and apparent vertical extrusion of HP rocks (Ambin and South Vanoise massifs, Western Alps) Jérôme Ganne, Jean-Michel Bertrand, Serge Fudral To cite this version: Jérôme Ganne, Jean-Michel Bertrand, Serge Fudral. Fold interference pattern at the top of basement domes and apparent vertical extrusion of HP rocks (Ambin and South Vanoise massifs, Western Alps). Journal of Structural Geology, Elsevier, 2005, 27 (3), pp.553-570. 10.1016/j.jsg.2004.11.004. hal- 00079351 HAL Id: hal-00079351 https://hal.archives-ouvertes.fr/hal-00079351 Submitted on 21 Jan 2018 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. Fold interference pattern at the top of basement domes and apparent vertical extrusion of HP rocks (Ambin and South Vanoise massifs, Western Alps) J. Gannea,*, J.-M. Bertrandb, S. Fudralc aAustralian Crustal Research Centre, School of Geiosciences, Monash University, PO Box 28E, Melbourne, Victoria 3800, Australia bLaboratoire de Ge´odynamique des Chaıˆnes Alpines, CNRS UMR 5025, Universite´ de Savoie, F 73376 le Bourget du Lac ce´dex, France cEDYTEM, CNRS, Universite´ de Savoie, Domaine Universitaire, F-73376, France The Ambin and South Vanoise Brianc¸onnais basement domes, located within the HP metamorphic zone, were chosen for a reappraisal of the early tectonic evolution of the Internal Alps in their western segment. -
Ferrocarpholite from Colle Ciarbonet (Cottian Alps)
90o SHORT COMMUNICATIONS MINERALOGICAL MAGAZINE, DECEMBER I976, VOL. 40, PP. 900-2 Ferrocarpholite from Colle Ciarbonet (Cottian Alps) DURING a petrographical investigation of the uranium-bearing high-pressure meta- morphic rocks of the Acceglio Zone, E. Zanettin (i96o) cursorily described the first occurrence of carpholite in the Western Alps at Colle Ciarbonet. The mineral occurs in calcite-quartz knobs and lenses to be found in the sheared zones of a horizon of Permian muscovite-chlorite phyllitic schists that underwent metamorphism at high pressure resulting in the scattered formation of lawsonite. Carpholite forms strongly elongated, fibrous prisms, bright green in colour, macroscopically indistinguishable from an actinolitic amphibole. It was identified through the following optical pro- perties: colourless in thin section, medium birefringent with negative optic sign, 2V~ 7 o~ 7 : [ooI] 2 ~ maximum index of refraction less than I"635. Carpholite s.s., the Mn-rich variety of the carpholite group of minerals (Mn,Mg, Fe") AI2[(OH)4]Si20~], has never been described in Italy whereas ferrocarpholite appears to be common in Calabria, southern Italy, sometimes in occurrences similar to that of Colle Ciarbonet (de Roever et al., I967, I97I). In view of the possible significance of ferrocarpholite as the alleged equivalent of the chloritoid+quartz-- water assemblage at high pressure (de Roever and Kieft, i97i), as well as of the incompleteness of another alpine description (Goff6 et al., I973), it seemed worth while to carry out a thorough investigation of the Colle Ciarbonet occurrence, so as to verify whether carpholite actually is present in the western Alps as well as to give new data on the distribution of a mineral the significance of which in metamorphism is far from being entirely understood. -
An Overview of Glacier Lakes in the Western Italian Alps from 1927 To
Geogr. Fis. Dinam. Quat. DOI 10.4461/GFDQ.2016.39.19 39 (2016). 203-214, 9 figg., 3 tabb. CRISTINA VIANI (*), MARCO GIARDINO (*,**), CH RISTIAN GLHUG E (***), LUIGI PEROTTI (*,**) & GIO VANNI MORTARA (**) AN OVERVIEW OF GLACIER LAKES IN THE WESTERN ITALIAN ALPS FROM 1927 TO 2014 BASED ON MULTIPLE DATA SOURCES (HISTORICAL MAPS, ORTHOPHOTOS AND REPORTS OF THE GLACIOLOGICAL SURVEYS) ABSTRT AC : VIANI C., GIARDINO M., HUGLG E C., PEROTTI L. & MOR- Alps (Monte Rosa Group). Moreover, in a dedicated database, we collect- TARA G., An overview of glacier lakes in the Western Italian Alps form ed information (descriptions, photos, maps) about glacier lakes from the 1927 to 2014 based on multiple data sources (historical maps, orthophotos reports of the annual glaciological surveys published by the Italian Gla- and reports of the glaciological surveys). (IT ISSN 0391-9839, 2016) ciological Committee (CGI) since 1928. Finally, we reported two cases of glacier lakes at the Tzére Glacier (Monte Rosa Group, Pennine Alps) Since the end of the Little Ice Age (LIA, ca. 1850 AD) a general and at the Ban Glacier (Monte Leone-Blinnenhorn Chain, Lepontine and progressive retreat of glaciers started in the European Alps, causing Alps), in order to demonstrate the importance of integrating data from a important environmental changes in this high mountain region. The ap- diversity of sources (historical maps, orthophotos and reports of the gla- pearance of glacier lakes is one of the most evident environmental effects ciological surveys) for better detailed reconstructions of the condition of in the Alps as well as in newly deglaciated areas worldwide. -
The Permian Formation in the Alps of Piémont, Dauphiné, and Savoy
Dr. Du Biche Preller—Permian in the Alps. 7 as at Bourg d'Oisans, has been noted by other writers. Here, too, the mineral so abundant in the green veins of Penmaenmawr, which Schaub has determined as prehnite,1 is at times seen to be intimately associated with the axinite. It has a lower refractive index and higher birefringence than the latter, and where cleavage-traces are developed it extinguishes parallel thereto (001). A genetic relation- ship between the two minerals appears to be indicated. In all the cases which I have seen recorded hitherto the gaseous boron-bearing emanations leading to the production of axinite have followed the intrusion of a granite magma. At Penmaenmawr the magma was of intermediate calc-alkalic character. It is assumed that here, too, the hot gases charged with boron-compounds reacted on the original lime-bearing minerals of the veins, releasing the silica and forming new combinations with the lime and other constituents, and that thus the secondary mineralization of the axinite veins was essentially effected. In the Cornish greenstones the production of axinite is usually accompanied by " one or more of the following minerals, pyroxene, epidote, hornblende, garnet, quartz, and felspar, while zoisite, zincblende, sphene, and fluor-spar are sometimes present ".J With the exception of quartz, a soda-lime felspar, and a little epidote, none of these minerals has been observed in the axinite veins of Penmaenmawr. The green and other veins, which are so abundant at Penmaenmawr and have been previously described, as mentioned above, consist predominantly of micropegmatite and orthoclase, with, subordinate plagioclase, augite, ilmenite, biotite, and apatite. -
The Passages of the Alps in IJI8
1915 THE PASSAGES OF TEE ALPS IN 1518 681 The Passages of the Alps in IJI8 IT seems well to reprint below the text of an exceedingly raxe little French book by Jacques Signot, which' bears the following long descriptive title : Downloaded from La totale et vraie description de tous lea passaiges, lieux et destroictz, par lesquelz on pent passer et entrer des Gaules es Ytalies. Et signam- ment par oi passerent Hannibal, Julius Cesar, et les trea chrestiens, magnanimes, et tres puissans roys de France, Charlemaigne, Charles viii, Louys xii, et le tres illustre roy Francois a present regnant premier de ce nom. http://ehr.oxfordjournals.org/ This is the first of several short treatises—the others refer to cardinals, patriarchs, archbishops, and bishops—written by a certain Jacques Signot, of whom nothing is known save that (as he tells us himself in his text, under the fifth pass) he himself accompanied Charles VIII to Naples in 1494-5. It is the earliest known systematic account of the passes of the Alps (though including only those from France to Italy), was often utilized at University of Iowa Libraries/Serials Acquisitions on July 14, 2015 and summarized by later writers, and for very many years formed the chief source of the knowledge of the passes between France and Italy. I owe most of the following bibliographical details to my friend Monsieur Henry Duhamel of Grenoble. The first edition was published in 1507 at Paris by Eustache de Brie (small 8vo, 28 leaves) as an appendix to the Crbnique de Qennes avec la totale description de Untie Ytattie; two later undated editions are known, one printed at Paris in small 8vo (48 leaves), and the other in 4to, by Michel Le Noir. -
Bozza RIVISTA Atto Costitutivo Unione Montana Valle Varaita
Bozza atto costitutivo allegato alla deliberazione del consiglio comunale n° del Il Sindaco Il Segretario comunale Registro Repertorio n. ATTO COSTITUTIVO DELL’UNIONE MONTANA DI COMUNI DELLA VALLE VARAITATRA I COMUNI DI BELLINO, BROSSASCO, COSTIGLIOLE SALUZZO, FRASSINO, ISASCA, MELLE, VALMALA, VENASCA. L’anno Duemila_____ (____ ), il giorno _______ del mese di ________ , con la presente scrittura privata, valida ad ogni effetto di legge: TRA il Comune di Bellino, rappresentato dal Sindaco pro-tempore, Sig. __________________ nato a ______________, il quale interviene ed agisce nel presente atto nella sua qualità di legale rappresentante del Comune di ______________________, autorizzato in forza della deliberazione del Consiglio comunale n. del , esecutiva; il Comune di Brossasco, rappresentato dal Sindaco pro-tempore, Sig. __________________ nato a ______________, il quale interviene ed agisce nel presente atto nella sua qualità di legale rappresentante del Comune di ______________________, autorizzato in forza della deliberazione del Consiglio comunale n. del , esecutiva; il Comune di Costigliole Saluzzo, rappresentato dal Sindaco pro-tempore, Sig. __________________ nato a ______________, il quale interviene ed agisce nel presente atto nella sua qualità di legale rappresentante del Comune di Frassino , autorizzato in forza della deliberazione del Consiglio comunale n. del , esecutiva; il Comune di Isasca, rappresentato dal Sindaco pro-tempore, Sig. __________________ nato a ______________, il quale interviene ed agisce nel presente atto nella sua qualità di legale rappresentante del Comune di ______________________, autorizzato in forza della deliberazione del Consiglio comunale n. del , esecutiva; il Comune di Melle, rappresentato dal Sindaco pro-tempore, Sig. __________________ nato a ______________, il quale interviene ed agisce nel presente atto nella sua qualità di legale rappresentante del Comune di ______________________, autorizzato in forza della deliberazione del Consiglio comunale n. -
Rapporto Preliminare Per Le Verifiche Di Assoggettabilita’ a Vas
COMUNE DI MONCALIERI CITTA’ METROPOLITANA DI TORINO PIANO URBANO DEL TRAFFICO VALUTAZIONE AMBIENTALE STRATEGICA progettazione Certificato UNI EN ISO 9001 direzione tecnica n° 24163/01/S emesso da associato TAU trasporti e ambiente urbano srl via Oslavia, 18/7 p.iva e c.f. 05500190961 20134 Milano t +39 02 26417244 [email protected] t +39 02 26417284 [email protected] f +39 02 73960215 www.t-au.com codifica elaborato commessa fase livello tipo prog rev nr scala 3701 PUT A RS 02 A 4 - oggetto RAPPORTO PRELIMINARE PER LE VERIFICHE DI ASSOGGETTABILITA’ A VAS rev data autore verifica approvazione A 19.01.2018 Valentina Zangirolami Marco Salvadori Giorgio Morini B C D La proprietà intellettuale di questo documento è riservata alla società Tau Trasporti e Ambiente Urbano s.r.l. ai sensi di legge. Il presente documento non può pertanto essere utilizzato per alcun scopo eccetto quello per il quale è stato realizzato e fornito senza l'autorizzazione scritta di Tau Trasporti e Ambiente Urbano s.r.l. né venire comunicato a terzi o riprodotto. La società proprietaria tutela i propri diritti a rigore di legge. COMUNE DI MONCALIERI PIANO URBANO DEL TRAFFICO VALUTAZIONE AMBIENTALE STRATEGICA Documento tecnico per la valutazione di assoggettabilità INDICE 1. PREMESSA ................................................................................................. 4 2. QUADRO NORMATIVO ............................................................................... 7 2.1. Normativa comunitaria .......................................................................