Commission Decision 2003/458/EC Amending Annexes I
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ISEO: Improving the lake Status from Eutrophy towards Oligotrophy University of Parma Nutrient loads, factors affecting their availability and response of submerged vegetation Main activities WP1: to estimate N and P potential loads of the different anthropic activities in the watershed to quantify nutrients (P, N and Si) loads to lake Iseo, evaluate how their magnitude and bioavailability are affected by hydrological conditions to check (and improve) the accuracy of P determination by the in situ auto analyzer WP2: to quantify nutrients (P, N and Si) concentrations in waters discharged by sewer overflows to evaluate the functioning of the littoral areas as a buffer of the external nutrients loads to map the extension and composition of submerged macrophytes meadows and their nutrients content and how they change in relation to external pressures Net anthropogenic P and N input to watersheds: a comparison 350 4000 300 3000 250 -1 -1 y y -2 -2 200 2000 150 kg P km kg 100 N km kg 1000 50 0 0 f. toce f. toce f. sarca f. mera f. mera f. sarca f. caffaro f. caffaro f. oglio imm f. ticino imm f. adda imm f. oglio imm f. adda immf. ticino imm f. chiese imm f. chiese imm Net anthropogenic phosphorus Net anthropogenic nitrogen input input = 562 t P y-1, = 6325 t N y-1 (areal load of 314 kg P km-2 y-1) (areal load of 3526 kg N km-2 y-1) average Po river watershed: 800 kg average Po river watershed: 8000 N km-2 y-1 kg N km-2 y-1 all fluxes are tons/y input = 562 t P y-1 P-fert P-feed P-food P-det 32 328 149 18 3 185 103 237 512 255 126 350 145 Main -
Voltzia Recubariensis from the Uppermost Angolo Limestone of the Bagolino Succession (Southern Alps of Eastern Lombardy, Italy)
Geo.Alp, Vol. 10 2013 61 - 70 Voltzia recubariensis from the uppermost Angolo Limestone of the Bagolino succession (Southern Alps of Eastern Lombardy, Italy) Peter Brack1 & Evelyn Kustatscher2 1ETH Zurich, Departement Erdwissenschaften, Sonneggstrasse 5, CH-8092 Zurich, Switzerland, e-mail: [email protected] 2 Naturmuseum Südtirol, Bindergasse 1, 39100 Bozen, Italy and Departement für Geo- und Umweltwissenschaften, Paläontologie und Geobiologie, Ludwig-Maximilians-Universität München, e-mail: [email protected]; Abstract Bagolino is the Global Stratotype Section and point for the base of the Ladinian Stage, well known for its ammonoids, bivalves and conodonts, while plant remains have so far not been described. Recently a conifer shoot of Voltzia recubariensis was found in the Anisian Angolo Limestone of the Rio Riccomassimo section east of Bagolino. This discovery opened a taxonomic discussion. A detailed literature research confirmed the validity of the name Voltzia recubariensis against V. agordica. The plant remain confirms also the presence of emerged land near Bagolino during the Anisian, probably to the south. It confirms also that V. recubariensis was one of the most common taxa of the Anisian of the Southern Alps and suggests that the flora of the western border area of the Tethys ocean must have been quite uniform. 1. Introduction The Anisian stratigraphic successions of eastern (Brack et al., 2005). Only few ammonoid-bearing Lombardy and Giudicarie rank among the clas- horizons are known also from older Anisian stra- sic localities since the early research on the Al- ta, i.e. from the uppermost part of the Angolo Li- pine Middle Triassic (Lepsius, 1878; Bittner, 1881; mestone (Monnet et al., 2008). -
BROCHURE INFORMATIVA COMUNE DI IDRO 0.Pdf
COMUNECOMUNE DIDI IDRO IDROIDRO Idro is ... a world waiting to be discovered In Auto come raggiungerci: Dall’Austria: Autostrada: Innsbruck - Brennero (Ita) - Bolzano - Trento (uscire dall’autostrada a Trento Nord) - Tione (seguendo per Riva fino a Le Sarche) - Lago Idro è... TRENTO km 70 MILANO km 150 d’Idro (in direzione Brescia) - Anfo - Idro. Idro un mondo da scoprire VENEZIA km 220 BRESCIA km 60 Dalla Svizzera: Autostrada: Gottardo - Bellinzona - Lugano - Chiasso (Ita) - Como MADONNA BRENNERO - Milano - Brescia (uscita dell’autostrada a Brescia Est) - Lago d’Idro (seguire le in- BOLZANO è...un mondo da scoprire DI CAMPIGLIO dicazioni per Lago di Garda - Lago d’Idro - Valle Sabbia - Madonna di Campiglio). Idro ist ... eine Welt zum entdecken Da Bologna: Autostrada: Verona - Desenzano (uscita dell’autostrada) - Salò - Tor- TRENTO is...a world waiting to be discovered mini - Lago d’Idro (seguire le indicazioni per Lago d’Idro - Valle Sabbia - Madonna di Campiglio). ist...eine Welt zum entdecken RIVA IDRO ROVERETO In Treno: Stazione di Brescia (60 km). In Autobus Lago d’Idro Da Brescia ferma a Idro (Idro-Bagolino-Madonna di Campiglio le destinazioni). TORMINI Da Trento ferma a Tione e a Baitoni-Lago d’Idro-Ponte Caffaro, cambiare per Idro MILANO (Vestone - Brescia le destinazioni). BRESCIA Lago di Garda In Aereo Aeroporti di Villafranca 95 km(Verona), Montichiari 55 km (Brescia), Orio al Serio DESENZANO VENEZIA VERONA 105 km (Bergamo) MODENA By car Mit dem Auto From Austria: Motorway: Innsbruck - Brennero (Ita) - Bolzano - Trento (exit the motorway at Von Österreich: Autobahn: Innsbruck – Brenner (Italien) – Bozen – Trient (Autobahnausfahrt Trento Nord) - Tione (head in the direction of Riva until Le Sarche) - Lago d’Idro (in the direction Trento Nord) – Tione (Richtung Riva bis Le Sarche) – Lago d’Idro (Richtung Brescia) – Anfo – Idro. -
The Geomorphosites in Lombardy
Il Quaternario Italian Journal of Quaternary Sciences 18(1), 2005 - Volume Speciale, 39-61 THE GEOMORPHOSITES IN LOMBARDY Luisa Pellegrini, Paolo Boni, Pierluigi Vercesi, Alberto Carton, Lamberto Laureti & Francesco Zucca with contribution of Stefania De Vita Dipartimento di Scienze della Terra, Università di Pavia, Via Ferrata 1, 27100 Pavia – e-mail: [email protected] ABSTRACT: L. Pellegrini et al., The Geomorphosites in Lombardy. (IT ISSN 0394-3356, 2005). Lombardy is a region of Northern Italy with a territory whose structure includes, from the physical-geographical point of view, a very important portion of the Alps and the adjacent Po plain with a little part of the Northern Apennines. This situation is due to the complexity of the landscape with its great diversity of historical and human aspects, frequently studied and described, but also the same physical elements which are, owing to their interest, worthy of conservation as part of the cultural heritage. As in many other Italian regions and provinces, also in Lombardy the exigence of describing and making available sites and peculiari- ties of the landscape arose, together with the suggestion of specific naturalistic tours, by means of relative guidebooks, monographs and so on. The Authors of the present work (as a part of the national research programme on ‘Geosites and Italian Landscape’) made a census of geomorphosites in Lombardy in order to their improvement, conservation and availability, both on the tourist and the scientific level. From the operating point of view, because of the high heterogeneity of the Lombard physical landscapes, it has been necessary to dif- ferentiate three main areas: Alps, Po plain and Apennines. -
Canyoning (AIC), Che Promuove La Diffusione Del Torrentismo, Un’Attività Sportiva finalizzata Alla Percorrenza in Sicurezza Dei Canyon
canAYoning u n v i aB g g i o nella storia n e i c o l o r i Sn e i s a p o r i IB comunità montana AGENZIA TERRITORIALE PER IL TURISMO di valle sabbia Comune di Idro ValleA DELLASabbia VALLE SABBIA E LAGO D’IDRO INTRODUZIONE RADUNO INTERNAZIONALE DI TORRENTISMO A IDRO Cos’è un canyon? La maggior parte delle persone i canyon li chiama anche orridi, quasi a voler sottolineare con questo termine i sentimenti di paura e di repulsione che normalmente sorgono nell’affacciarsi sul bordo di uno di quei profondi solchi scavati dalla forza dell’acqua. C’è però una minoranza che al termine “orrido” preferisce il più scientifico “forra”, ed è irresistibilmente attratta dal calarvisi dentro per transitare, assieme all’acqua, nel contesto di una natura che come in pochi altri luoghi può ancora definirsi selvaggia. Semantica a parte i canyon rappresentano ambienti di grande fascino. La pensano così almeno quelle centinaia di persone iscritte all’Associazione Italiana Canyoning (AIC), che promuove la diffusione del torrentismo, un’attività sportiva finalizzata alla percorrenza in sicurezza dei canyon. Forre spettacolari si concentrano in gran numero attorno al lago di Garda e al lago d’Idro: la loro percorrenza è diventata in questi ultimi anni un elemento di valorizzazione turistica capace di coinvolgere nella stagione estiva, attraverso le escursioni guidate dagli accompagnatori specializzati, migliaia di persone entusiaste. Sulla scia di questo interesse è nata così nell’AIC l’idea di organizzare a Idro dal 30 luglio al 6 agosto 2006, con il patrocinio dell’Agenzia Territoriale per il Turismo Valle Sabbia e Lago d’Idro, il 4° raduno internazionale di torrentismo. -
Première Édition
Première édition Les 4 lauréats du concours Eco-trophée du Parc naturel régional de la Brenne ont été dévoilés lors de la cérémonie de remise des prix qui s’est tenue à la Maison du Parc (Rosnay), jeudi 18 novembre. Près de 100 personnes étaient présentes (entreprises et associations candidates, élus et partenaires de l’opération). Une première édition qui se clôture sous le signe de la réussite. Pour rappel, 41 dossiers ont été déposés dans les 3 catégories : - Respect de l’environnement : actions en faveur de l’environnement dans différents domaines que peuvent être les déchets, l’eau, l’air, les énergies, la sauvegarde de la biodiversité… - Renforcement du lien social : actions favorisant le lien social dans l’établissement : formation des salariés, accompagnement d’apprentis, de stagiaires, recrutement de personnes en difficultés d’insertion, sécurité et santé du personnel… - Harmonie territoriale : actions liées à la reconnaissance et au développement de son territoire : approvisionnements locaux, sauvegarde de ressources et de savoir-faire locaux, service rendu à la population… Un prix a été décerné par catégorie, auquel s’ajoute le prix coup de cœur du jury. Les résultats Catégorie « Respect de l’environnement » 16 dossiers étaient présentés Le prix a été attribué à l’exploitation agricole, l’EARL du Bois d’Angles. Chefs d’exploitation Xavier JACQUET et Benjamin MEREAU Commune Lurais Activité Production de céréales et élevage de canards gras et canards prêts à engraisser Date de reprise 1er septembre 2006 Réalisation présentée Traitement des eaux usées en milieu agricole à l’Eco-trophée Xavier Jacquet et Benjamin Mereau ont aménagé en 2009 une aire de lavage pour le matériel de gavage et le matériel agricole. -
Pré Diagnostic Hydromorphologiqué Dés Massés D'éau Du Bassin Dé L
Pré diagnostic hydromorphologiqué dés massés d’éau du bassin dé l’Anglin Syndicat Intercommunal d’Aménagement du bassin de l’Anglin Août 2014 Avec la collaboration de : Table des matières GLOSSAIRE ............................................................................................................................................................................. 2 CONTEXTE .............................................................................................................................................................................. 4 EXPLICATIONS SUR L’OUTIL SYRAH-CE ............................................................................................................................. 5 METHODES ............................................................................................................................................................................. 6 PRESENTATION SUCCINCTE DU BASSIN ................................................................................................................................ 6 I. HYDROLOGIE : QUANTITE ET DYNAMIQUE .............................................................................................................. 12 I.1 Anglin ............................................................................................................................................................... 12 I.2 Le Salleron .................................................................................................................................................... -
List of Rivers of Italy
Sl. No Name Draining Into Comments Half in Italy, half in Switzerland - After entering Switzerland, the Spöl drains into 1 Acqua Granda Black Sea the Inn, which meets the Danube in Germany. 2 Acquacheta Adriatic Sea 3 Acquafraggia Lake Como 4 Adda Tributaries of the Po (Left-hand tributaries) 5 Adda Lake Como 6 Adige Adriatic Sea 7 Agogna Tributaries of the Po (Left-hand tributaries) 8 Agri Ionian Sea 9 Ahr Tributaries of the Adige 10 Albano Lake Como 11 Alcantara Sicily 12 Alento Adriatic Sea 13 Alento Tyrrhenian Sea 14 Allaro Ionian Sea 15 Allia Tributaries of the Tiber 16 Alvo Ionian Sea 17 Amendolea Ionian Sea 18 Amusa Ionian Sea 19 Anapo Sicily 20 Aniene Tributaries of the Tiber 21 Antholzer Bach Tributaries of the Adige 22 Anza Lake Maggiore 23 Arda Tributaries of the Po (Right-hand tributaries) 24 Argentina The Ligurian Sea 25 Arno Tyrrhenian Sea 26 Arrone Tyrrhenian Sea 27 Arroscia The Ligurian Sea 28 Aso Adriatic Sea 29 Aterno-Pescara Adriatic Sea 30 Ausa Adriatic Sea 31 Ausa Adriatic Sea 32 Avisio Tributaries of the Adige 33 Bacchiglione Adriatic Sea 34 Baganza Tributaries of the Po (Right-hand tributaries) 35 Barbaira The Ligurian Sea 36 Basentello Ionian Sea 37 Basento Ionian Sea 38 Belbo Tributaries of the Po (Right-hand tributaries) 39 Belice Sicily 40 Bevera (Bévéra) The Ligurian Sea 41 Bidente-Ronco Adriatic Sea 42 Biferno Adriatic Sea 43 Bilioso Ionian Sea 44 Bisagno The Ligurian Sea 45 Biscubio Adriatic Sea 46 Bisenzio Tyrrhenian Sea 47 Boesio Lake Maggiore 48 Bogna Lake Maggiore 49 Bonamico Ionian Sea 50 Borbera Tributaries -
The Application of Environmental Flow Regulations to Small Hydropower Plants in Alpine Areas
View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by Archivio istituzionale della ricerca - Università di Brescia IWLHS, 20-22/02/2013, Aachen - Bung & Pagliara (eds) - © 2013 Bundesanstalt für Wasserbau ISBN 978-3-939230-04-5 The Application of Environmental Flow Regulations to Small Hydropower Plants in Alpine Areas L. Milanesi, M. Pilotti & G. Valerio Department of Civil Engineering, Architecture, Land, Environment and Mathematics (DICATAM), Università degli Studi di Brescia – Via Branze, 43, Brescia, Italy ABSTRACT: within a framework of conflicting needs and under water scarcity scenarios, environmental issues are assuming more and more relevance in water cycle management. An important role in this context is played by the minimum discharge release downstream of diversion structures, the so-called “environmental flow”, aiming at assuring acceptable ecological conditions along natural watercourses. In this paper the regulation criteria adopted in several European alpine countries will be briefly discussed. The implementation of environmental flow regulations to small hydropower plants in the province of Brescia (Northern Italy), which is one of the most relevant Italian district in terms of number of hydropower plants, installed capacity and energy production, will be presented. In particular, the prevailing environmental flow release devices and their main technical characteristics, operating features and design criteria are briefly discussed. The introduction of environmental flow legislation entails both benefits and disadvantages which are often difficult to quantify. This paper gives a contribution to this costs-benefits analysis, by estimating the loss of energy producibility for a small alpine hydropower plant, related to the enforcement of environmental flow regulations and to the design criteria of the release devices. -
Date Epoux Père Mère Ex
Date Epoux Père Mère Ex.conjoint Origine __________________________________________________________________________________________________________________________________ 07/02/1750 AUMASSON François 17/02/1656 DELANOT Jean 17/12/1708 GABILLON Antoine 03/02/1704 JOYEUX Pierre 03/02/1704 LONGIN André 06/06/1712 MIAUD Silvain 29/01/1704 PENNETIER Georges 02/03/1677 PINARDON Jean 15/02/1707 TREBILLON Léonard 22/02/1705 Catherine GIRAUD Jacques 17/02/1656 Marguerite RULAUD Léonard 02/02/1655 Pierre MOREAU Mathurine 19/08/1834 ALABEDOUCHE François +Benoît +PERROT Marie +X2 DAVID Marie ST BENOIT/SAULT DUCOURET Jeanne +Silvain +PINARDON Jeanne ST SÉBASTIEN 19/08/1834 ALABEDOUCHE Jean Baptiste François +BOUTAUD Marie Anne AZERABLES BRUNAUD Geneviève +Jean DEBROSSE Marie MOUHET 31/03/1845 ALABEDOUCHE Marie Louise François +BOUTAUD Marie Anne AZERABLES ALASSAUNIERE Silvain +Silvain PÉRINET Silvine +PINARD Silvine ST SÉBASTIEN 09/02/1751 ALAGAISSE Catherine François PENNETIER Aimée DELANEAU Philippe Henri DAILLET Marie 22/01/1828 ALAGAISSE Catherine MOUHET MAILLASSON Philippe Jean GABILLON Catherine MOUHET 08/03/1734 ALAGAISSE Etienne Silvain PEIGNOT Marie GIRAUD Marie Jacques ALAGAISSE Catherine 17/02/1763 ALAGAISSE Etienne François PENNETIER Aimée JAMOT Marie Jean DUCOURET Marie 27/02/1775 ALAGAISSE Etienne JAMOT Marie BONNET Thérèse François CHETIFEU Louise 22/02/1729 ALAGAISSE François Jean DUCOURET Françoise PENNETIER Renée 07/02/1730 ALAGAISSE Jacques Jean PHILIPPON Anne MAILLOCHON Madeleine Pierre ARNAUD Jeanne 07/11/1854 ALAGAISSE Jean +Jean -
SENTIER DE GRANDE RANDONNEE DE PAYS DE LA BRENNE De
SENTIER DE GRANDE RANDONNEE DE PAYS DE LA BRENNE De Saint-Benoît à Angles, deux des plus beaux villages de France 4 jours / 3 nuits 96 km Le cours champêtre de l'Anglin guide cet itinéraire entre deux des plus beaux villages de France : d'abord dans un paysage de bois et de bocage puis sur les plateaux des falaises calcaires qui bordent sa vallée, riche d'orchidées au printemps. L’itinéraire est jalonné pendant tout le parcours en jaune et rouge. Cartographie IGN 1/25000 : 2027 Est, 2028 Est, 2027 Ouest, 1927 Est,1926 Est et 1926 Ouest. Les possibilités de ravitaillement sont mentionnées à la fin du pas à pas de chaque journée. L'itinéraire traversant peu de villages dotés de commerces, soyez vigilant aux recommandations. Nous espérons que ce parcours répondra à vos attentes. Si vous avez des remarques à faire sur l’itinéraire, n’hésitez pas à les communiquer à l’Office de tourisme de Bélâbre qui transmettra au service tourisme du Parc naturel régional de la Brenne. Jour 1 : Saint-Benoit-du-Sault – Chaillac 21 km Départ de la cité médiévale de Saint-Benoît-du-Sault devant l’Office de Tourisme (1). A partir de ce point, deux solutions sont proposées : suivre le balisage du GR de Pays et entamer rapidement le parcours de la première journée (option 1) ou passer dans la vieille ville avant de rejoindre le circuit (option 2). Option 1 : dos à l'Office de tourisme, traverser en diagonale la place en direction de l’hôtel des 300 couverts. Emprunter le chemin du Lavoir qui serpente entre de hauts murs. -
(GSSP) of the Ladinian Stage (Middle Triassic) at Bagolino (Southern Alps, Northern Italy) and Its Implications for the Triassic Time Scale
Articles 233 by Peter Brack1, Hans Rieber2, Alda Nicora3, and Roland Mundil4 The Global boundary Stratotype Section and Point (GSSP) of the Ladinian Stage (Middle Triassic) at Bagolino (Southern Alps, Northern Italy) and its implications for the Triassic time scale 1 Departement Erdwissenschaften, ETH-Zentrum, CH-8092 Zürich, Switzerland. 2 Paläontologisches Institut, Universität Zürich, CH-8006 Zürich, Switzerland. 3 Dipartimento di Scienze della Terra, Università di Milano, Via Mangiagalli 34, I-20133 Milano, Italy. 4 Berkeley Geochronology Center, 2455 Ridge Road, Berkeley, CA 94709, USA. The Global boundary Stratotype Section and Point (GSSP) for the base of the Ladinian Stage (Middle Tri- Historical context of the Ladinian Stage assic) is defined in the Caffaro river bed (45°49’09.5’’N, The first formal recognition of a stratigraphic interval comprising what 10°28’15.5’’E), south of the village of Bagolino is now called Ladinian orginates from the subdivisions of the Triassic (Province of Brescia, northern Italy), at the base of a System proposed by E.v. Mojsisovics. Ammonoids served as the main biostratigraphic tool for these divisions. By 1874 and with later modi- 15–20-cm-thick limestone bed overlying a distinct fications (e.g., 1882), Mojsisovics used the name “Norian” for a strati- groove (“Chiesense groove”) of limestone nodules in a graphic interval including, at its base, the South Alpine Buchenstein Beds and siliceous limestones of Bakony (Hungary). Because Moj- shaly matrix, located about 5 m above the base of the sisovics erroneously equated this interval with parts of the ammonoid- Buchenstein Formation. The lower surface of the thick rich Hallstatt-limestones, he used the term “Norian” as the stage name, limestone bed has the lowest occurrence of the which refers to the Norian Alps around Hallstatt near Salzburg (Aus- tria).