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Dossier Cime Bianche Ayas, Estate-Inverno 2015
Dossier Cime Bianche Ayas, Estate-Inverno 2015 A cura del gruppo di lavoro “Ripartire dalle Cime Bianche” Contatti: [email protected] Per ulteriori informazioni sulle Cime Bianche, sul loro Vallone e sulla Val d’Ayas: - www.varasc.it - www.ayastrekking.it - www.andarpersassi.it - www.comune.ayas.ao.it/sito-ufficiale-comune/it/turismo/home-page-turismo.aspx - www.vivavda.it/it/aree/monte-rosa-valle-d-aosta CIME BIANCHE: UN VALLONE DI GRANDE BELLEZZA (AYAS, VALLE D’AOSTA) VENITE A CONOSCERLO - AIUTATECI A DIFENDERLO Il Vallone delle Cime Bianche, o di Courtoud, è situato intera- Percorrendo il vallone, preferibilmente con percorso ad anello, mente nel Comune di Ayas e si estende per una lunghezza di lo sguardo non cessa di stupirsi per la meravigliosa varietà ed circa 10 chilometri, delimitando a ovest il versante meridionale integrità dei paesaggi di alta quota che incontra a 360°. del massiccio del Monte Rosa. Giunti al Colle Superiore delle Cime Bianche, che mette in col- legamento con la Valtournenche, è sorprendente il colpo d’oc- Solcato per l’intera lunghezza dal Torrente Courtoud, il versan- chio sul Cervino. te orografico destro è sovrastato dai ripidi versanti che sorreggo- no il terrazzo orografico d’alta quota che dalla base del Grand Il Vallone delle Cime Bianche riveste inoltre una notevole im- Tournalin e del Monte Croce conduce al Monte Roisettaz. portanza storica, culturale e archeologica, essendo stata un’antica via di migrazione della popolazione Walser e di scam- Il versante orografico sinistro, denominato anche Comba d’A- bi commerciali, ospitando testimonianze della lavorazione della ventine, è un susseguirsi di ampi pianori erbosi e torbiere che pietra ollare e della cottura della calce, oltre al famoso Ru Cour- toud che da circa 600 anni porta le acque irrigue sui versanti intersecano le vallette tributarie di Tzere e Rollin, le cui acque aridi di Saint Vincent e Emarèse con un percorso di ben 25 chi- originano dagli omonimi ghiacciai. -
Valle D'aosta Checked
! AOSTA VALLEY: THE MOST LITTLE AMAZING GIFT Where Valle D’Aosta region is the smallest and least populated region in Italy. Weather Located at the northern tip of Italy is Valle d’Aosta (Aosta This northern region has a very Valley). It is a mountainous semi-autonomous region cold winter with a long snow bordered by Rhône-Alpes, France to the west, season and misty summer. Switzerland to the north and the region of Piedmont to the south and east. Aosta Valley has the highest peaks in the Alps: Cervino, Monte Rosa, Gran Paradiso and the king of them all, Mont Blanc, which at 15,781 feet is the highest mountain in Europe. Not only is Aosta Valley the smallest region in Italy, but with a population of about 126,933 people, it is also the least populous. Additionally, it is the only region without provinces. As the coldest region in Italy, with a bitter continental climate, the summers are cool, with an average temperature of 64-68 degrees, and very cold winters, averaging around 30 degrees, though slightly lower overall nearest the French border. Though Aosta Valley is known for its ski slopes of Cervinia, Courmayeur, and Pila, this region also offers plenty of cultural and traditional treasures. Despite being such a tiny region, Aosta Valley is bursting with opportunities to explore the off-the-beaten-path part www.helloitalytours.com !1 ! Food Specialities of Italy. Here you’ll find something for everyone, including a hundred castles, an array of Gothic sculptures, panoramic views, glamorous ski resorts, secluded hiking Fontina: A cow’s milk cheese, trails, sophisticated and rustic food, abundant wildlife, Fontina has a mild, somewhat Baroque village churches, and Europe’s largest casino. -
A Network-Based Approach for the Study of Criticalities in Ski-Resorts
International Snow Science Workshop Grenoble – Chamonix Mont-Blanc - 2013 A network-based approach for the study of criticalities in ski-resorts Valerio De Biagi1,2*, Barbara Frigo1,2 and Bernardino Chiaia1,2 1 Dept. of Structural, Geotechnical and Building Engineering, Politecnico di Torino, ITALY 2Mountain Risk Research Team – MRR Team, Verrès (AO) – Italy ABSTRACT: The correct management of ski-resorts requires wide knowledge in mountain hazards, as well as a large experience. Usually ski-resorts cover a surface that encompasses more than one side of a mountain (or more than one valley); for this reason, the meteorological conditions may vary locally and rapid decisions have to be taken in order to ensure the safety of the skiers. Any intervention on the structure of the resort may entail cascade events and other critical situations. For example, a temporary closure of a lift may create large queues in other parts of the ski-area. In the same way, a closure of a ski-slope might engender overcrowding in other ski runs. All these situations are potential sources of risk. We propose an approach to the study of criticalities in ski-resorts by means of transportation network approaches based on the ability of the skiers and the grade of the ski run. An example is made on the Antagnod branch of MonteRosaSki resort. The effects of a sudden interruption of part of it, i.e., ski- slope closure or lift temporary interruption, are simulated. KEYWORDS: Ski-resort management, Graph theory, Criticalities. others (2005) made a statistics of the average 1 INTRODUCTION speeds of skiers in three different ski resorts in the US. -
ORARI COURMAYEUR > AOSTA > TORINO
ORARI COURMAYEUR > AOSTA > TORINO LINEA ATTIVA DAL 14 GIUGNO 2021 frequenza / note GG GG 5 GG COURMAYEUR – P.le Monte Bianco 9.35 13.35 16.35 partenza LA THUILE 9.18 13.05 16.13 PRE-SAINT-DIDIER S.S.26 9.43 13.43 16.43 MORGEX S.S.26 9.50 13.50 16.50 LA SALLE S.S.26 9.53 13.53 16.53 RUNAZ S.S.26 10.00 14.00 17.00 ARVIER S.S.26 10.07 14.07 17.07 VILLENEUVE Entrata Est Capoluogo 10.14 14.14 17.14 SAINT-PIERRE Hotel Château 10.17 14.17 17.17 SARRE S.S.26 10.22 14.22 17.22 Aosta Autostazione arrivo 10.35 14.35 17.35 AOSTA – Autostazione 6.55 10.55 14.55 17.55 NUS S.S.26 7.10 11.10 15.10 18.10 partenze BREUIL-CERVINIA 6.25 10.25 13.05 17.15 partenza VALTOURNENCHE 6.45 10.45 13.25 17.35 partenza ANTEY-SAINT-ANDRE 7.05 11.05 13.45 17.55 CHÂTILLON Autostazione 7.25 11.25 15.25 18.25 VERRES Autostazione 7.35 11.35 15.35 18.35 PONT SAINT MARTIN - Via Circonvallazione 7.45 11.45 15.45 18.45 TORINO -C.so G.Cesare - IVECO 8.25 12.25 16.25 19.25 TORINO -C.so G.Cesare, 131 8.32 12.32 16.32 19.32 TORINO - C.so G.Cesare, 13 - Porta Palazzo 8.40 12.40 16.40 19.40 TORINO – P. -
Real-Time Detection of Natural Snow Avalanches by Infrasonic Array Network (IAN) on December 2012 in Valtournenche – Aosta Valley (IT)
International Snow Science Workshop Grenoble – Chamonix Mont-Blanc - 2013 Real-time detection of natural snow avalanches by Infrasonic Array Network (IAN) on December 2012 in Valtournenche – Aosta Valley (IT) Durand N.1, Ulivieri G.2, Marchetti E.2 , Frigo B.*, 1, Dellavedova P.1, Ripepe M.2, Segor V.3 1 Fondazione Montagna sicura - Montagne sûre, Courmayeur (AO) – Italy; 2 Dipartimento Scienze della Terra, University of Firenze, Firenze - Italy; 3 Struttura assetto idrogeologico dei bacini montani – Ufficio Neve e Valanghe, Regione Autonoma Valle d’Aosta, Quart (AO) - Italy; ABSTRACT: Since 2009 and within the Operational programme Italy-France (Alps ALCOTRA) – Pro- jects “DynAval” (2009-2012) and “Map3“ (2012-2014), infrasonic array technology is tested in Aosta Valley to real-time detect the natural and artificial avalanche activity in the Alpine areas. In winter 2012, an Infrasonic Array Network (IAN) operates around the Monte Rosa and Matterhorn areas, mon- itoring ~250 km2 of Valtournenche, Ayas and Gressoney Valleys. If single infrasonic array allows de- tecting small-to-medium size (~500 m3) powder avalanches in the 3-10 km distance range, providing relative location (direction of provenience and recording time) of the source, the IAN allows more pre- cise location (geographic position and time of occurrence), and the broadening of the area covered by the avalanche monitoring system. Information on identified events are broadcasted automatically in real-time (every 15 minutes), thus indicating potential sectors where avalanches might have occurred during the last 24 h or where to focus further avalanche control activity. The validation of the locations is done by comparing ground-truth (natural or artificial) avalanche events with the infrasonic meas- urements. -
Een Kleine Vallei Met Een Groots Verhaal
Een kleine vallei met een groots verhaal. Valle d’Aosta is de kleinste regio van Italië. Ze is omringd door de hoogste toppen van Europa en bestaat uit het centrale dal van de Dora Baltea, van- waar 13 kleinere zijdalen lopen die worden doorkruist door gletsjers en stro- men. Sinds de oudheid is het een belangrijk kruispunt van de westelijke Alpen. Op dit moment is het verbonden met Frankrijk via de Mont Blanc-tunnel en de Kleine Sint-Bernhardpas en met Zwitserland via de Grote Sint-Bernhardpas en -tunnel. De vallei was al in de prehistorie bewoond en werd bezet door de Salassi, een Gallo-Keltische bevolkingsgroep die na een lange strijd werd verdreven door de Romeinen in de 1ste eeuw v.Chr. De Romeinen vestigden zich in de regio en stichtten de stad Augusta Praetoria in 25 v.Chr. De vallei kwam later in handen van de Bourgondiërs, de Longobarden en de Karolin- gers tot ze de eigendom werd van het vorstenhuis Savoye. In 1191 verleende Thomas I van Savoye de “Carta delle Franchigie”, die het politieke en admi- nistratieve zelfbestuur erkende en van kracht bleef tot 1770. De vallei kende een vorm van autonomie met eigen wetten en werd bestuurd door de Staten Generaal, en vanaf 1536 door het Conseil des Commis, een soort bestuursraad die uit 24 leden bestond. Napoleon trok tijdens zijn campagne in Italië door de regio in 1800 en bracht de idealen van de revolutie met zich mee. Dit wekte sympathie en haat, bewondering en angst op en vormde de aanleiding voor legendes en verhalen die vandaag de dag nog steeds in de vallei worden verteld. -
Coccola Un Valdostano ELENCO STRUTTURE (Pdf
B&B e Affittacamere della Valle d’Aosta vogliono coccolare i Valdostani, e li invitano a scoprire un po’ di più la loro Regione, godendosi un soggiorno a prezzo scontato con cena presso i ristoranti convenzionati. Offerta valida dal 22 febbraio fino al 30 giugno 2021! www.coccolaunvaldostano.com SITO INTERNET ANIMALI LOCALITA’ NOME STRUTTURA N. TELEFONO RISTORANTI CONVENZIONATI SERVIZI E-MAIL AMMESSI www.bedbreakaosta.com Aosta B&B Al Nabuisson 339 6090332 Osteria da Nando SI aostacentro @hotmail.com www.lacasadelgrilloaosta.it Ristorante Hostaria del Calvino – Aosta Aosta B&B La Casa Del Grillo 348 9851918 SI Parcheggio gratuito, WiFi [email protected] Ristorante Osteria da Nando - Aosta www.maisondunoyer.com Aosta - Excenex Chambres d'hôtes Maison du Noyer 371 4834739 Cucina interna ? [email protected] www.lepetitlievre.com Aosta - Porossan B&B Le Petit Lièvre 335 5358682 Ristorante Osteria da Nando - Aosta ? [email protected] www.auchateaublanc.it Hotel Beau Sejour – Arvier Arvier B&B Au Chateau Blanc 347 8651747 SI [email protected] Osteria del Viandante - Arvier www.langolinodibonny.it Hotel Beau Sejour – Arvier Arvier B&B L’angolino di Bonny 338 2793576 ? [email protected] Osteria del Viandante - Arvier www.maisondelamontagne.net Arvier B&B Maison de la Montagne 333 2029837 ? [email protected] Ristorante Casa Coucca – Bard www.vecchiotorchio.com Bard B&B Vecchio Torchio 347 8743254 Ristorante Ad Gallias – Bard ? [email protected] Ristorante Caffè Bistrot - Bard www.micasaticasa.info -
0423662 Page 1 of 28 Annual Report for Period:12/2009
Annual Report: 0423662 Annual Report for Period:12/2009 - 11/2010 Submitted on: 11/17/2010 Principal Investigator: Williams, Mark W. Award ID: 0423662 Organization: U of Colorado Boulder Submitted By: Williams, Mark - Principal Investigator Title: Long Term Ecological Research: The Landscape Continuum Model: A Biogeochemical Paradigm for High Elevation Ecosystems Project Participants Senior Personnel Name: Williams, Mark Worked for more than 160 Hours: Yes Contribution to Project: Dr. Mark Williams is the current PI of the NWT LTER project and is project director. Provides overall project guidance and leadership. His research areas are in snow hydrology, surface-groundwater interactions, terrestrial-aquatic interactions, and biogeochemistry. Name: McKnight, Diane Worked for more than 160 Hours: Yes Contribution to Project: Dr. McKnight is a Co-I on the NWT LTER program. Her research focuses on limnology, aquatic ecology, reactive transport of metals and organic material in mountain streams and rivers. She is the NWT LTER lead on K-12 outreach activities. Name: Seastedt, Timothy Worked for more than 160 Hours: Yes Contribution to Project: Dr. Tim Seastedt is a Co-I on the NWT LTER program. He is the former lead PI of the NWT LTER program. He provides continuity in leadership as well as mentoring as M. Williams transitions to the lead PI position. His research interests focus on terrestrial ecosystem studies, including factors influencing primary productivity, soil carbon dynamics, decomposition and mineralization processes, and how these processes affect short- and long-term ecosystem-atmosphere interactions. Ongoing research collaborations involve cross-site comparisons of mechanisms controlling nutrient availability, carbon storage, and biotic productivity, invasive species, and ecosystem processes-biodiversity relationships. -
Châteaux De La Vallée D'aoste
CHÂTEAUX DE LA VALLÉE D AOSTE A journey through’ history, art and nature The castles From the twelfth century, the local of the lords constructed fortified buildings for defensive purposes, such as the castles Aosta Valley: of Graines, Châtel-Argent and Cly, which perfectly exemplify the oldest style a thrilling journey of castle architecture. through time However, from the fourteenth century onwards, the architectural features serving to defensive purposes were superseded by monolithic structures, such as those of the castles of Ussel and Verrès, which were then gradually embellished with decorative features, as can be observed at the famous A significant and rich cultural heritage Fénis Castle among others. made up of castles, strongholds The stylistic evolution of the fortressin and historic buildings welcomes to a fine manor house is evident in the those visiting the Aosta Valley castles of Aymavilles and Issogne, whereas or travelling through. the abodes of Sarre and Savoy Castle of Indeed, the many castles scattered Gressoney-Saint-Jean are testimonies to along the region’s central valley the presence of the Savoy dynasty in the are of outstanding Aosta Valley and the artistic taste in vogue beauty and cultural interest. in that court. Built in strategic places to defend ancient lands, these castles In the summer, the magic of this places with their variety of styles is even greater as the castles become and architectural features are spectacular scenery for emotionally a valuable testimony to the history charged musical events. Guests are treated of the Aosta Valley. to refined and exclusive evenings as the events feature artists of national and international caliber. -
Trip Factsheet: Off Piste Adventure Gressoney Gressoney One of The
Trip Factsheet: Off Piste Adventure Gressoney Gressoney One of the classic Italian villages in the Monte Rosa ski region, this pretty village situated at 1637m offers excellent access into the ski area. The ski area links Gressoney with Alagna and Champoluc and in total there are about 200km of pisted terrain. The off-piste options include everything from wide open powder fields, perfect for mastering your technique, to excellent treeskiing and steep, narrow couloirs. Add in the vertical drop of around 2000m from the top lift and the fact that during the week the slopes are often deserted and you’ll understand why this is one of our favourite ski areas. The hospitality and food in the region is typically Italian and you will enjoy plenty of fantastic local food and wine during your stay. Objectives of the trip To improve your off-piste skiing and your confidence by providing first class guiding from our pro Mountain Guides. To explore the best off piste skiing Gressoney has to offer. To provide practical mountain awareness training on the risks and hazards of backcountry skiing. Our top reasons to visit Gressoney Extensive off-piste terrain and a reputation for great freeriding Gressoney, together with Champoluc and Alagna make up the Monterosa ski area, the largest in Italy Charming Italian ambience One of the best heliskiing resorts in the Alps Minimal touristic development area means the slopes are often deserted especially during the week Easy access from Turin Airport make it a viable weekend or short break destination Travel to and from Gressoney You want to arrange to arrive in Gressoney by late afternoon on the first day. -
Determining the Drivers for Snow Gliding
Determining the drivers for snow gliding Reinhard Fromm1, Sonja Baumgärtner2, Georg Leitinger2, Erich Tasser3, Peter Höller1 1Federal Research and Training Centre for Forests, Natural Hazards and Landscape – BFW, Department of Natural Hazards, Innsbruck, 6020, Austria 5 2Institute2Department of Ecology, University of Innsbruck, Innsbruck, 6020, Austria 3Institute for Alpine Environment, Eurac research, Bozen, 39100, Italy Correspondence to: Reinhard Fromm ([email protected]) 10 Abstract. Snow gliding is a key factor for snow glide avalanche formation and soil erosion. This study considers atmospheric and snow variables, vegetation characteristics, and soil properties, and determines their relevance for snow gliding at a test site (Wildkogel, Upper Pinzgau, Austria) during winter 2014/15. The time-dependent data were collected at a high temporal resolution. In addition to conventional sensors a ‘snow melt analyzer’ was used. The analysis shows that the soil temperature 10 cm below the surface, the phytomass of mosses, the liquid water content in 15 the snowpack, and the static friction coefficient of the glide shoes had significant influence on snow gliding during the whole winter. In the first period (October to January) the soil moisture at the surface and 1.5cm below the surface and the length of the slope uphill the glide shoes affected the snow gliding, too. In the second period (February to May) the soil temperature at the surface, the soil moisture 10cm below the surface, and the slope angle had additional influence on snow gliding. The role of the vegetation in the snow glide process is determined by the influence on the static friction coefficient caused by 20 its composition and characteristics and that moss-rich and short-stemmed canopies seem to be more interconnected with the snowpack. -
EGU2018-4918, 2018 EGU General Assembly 2018 © Author(S) 2018
Geophysical Research Abstracts Vol. 20, EGU2018-4918, 2018 EGU General Assembly 2018 © Author(s) 2018. CC Attribution 4.0 license. Glacial Outburst flood risk assessment on the Chérillon Glacier (Valtournenche, Aosta Valley, Italy) Fabrizio Troilo (1), Elena Motta (1), Diego Franco (2), Alberto Godio (2), and Valerio Segor (3) (1) Safe Mountain Foundation, Glaciers and Permafrost Office, Italy ([email protected]), (2) DIATI, Politecnico di Torino, Torino, Italy, (3) Struttura assetto idrogeologico dei bacini montani, Regione Autonoma Valle d’Aosta An anomaly in the regular hydrology of the Chérillon Glacier (Aosta Valley –Italy) was reported to local authorities on the 24th of July 2017, describing the sudden disappearing of a glacial stream on the 23rd of July 2017. Investigation about the phenomena was needed to detect individuate the water retention inside or under the glacier that originated the glacial stream (Torrente Fossu), now dried. An eventual sudden increase in water run-off would flow, via the Torrente Fossu, through the densely populated area of Breuil-Cervinia: a first field survey was immediately carried out in order to observe in-situ conditions and eventual morphological evidences. No surface evidence of glacial collapse or water pocket formation was reported, but further investigations had to be planned to assess the presence of water pockets beneath the glacier surface. A first field survey was performed by collecting Ground Penetrating Radar (GPR) data along several profiles that covered all the North-East part of the glacier; this is the part of the glacier from which water would potentially flow towards the stream. The resulting radargrams detected a subglacial cavity with an estimated volume of some thousands of cubic meters; an accurate analysis of the cavity volume was not possible.