Glaciers of the Alps
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Adventure Travel Trip Itinerary
Adventure Travel Trip Itinerary Name of trip: Switzerland—Tour du Mont Blanc Dates of trip: August 20 - September 4, 2019 Leader: Debbie Markham Date Meals Day Day Activity (distances are approximate) Accommodation, Notes included Aug 20 Travel to Geneva, Switzerland (Tues) 1 Aug 21 Arrival in Geneva Overnight in Geneva at D (Wed) Please plan to arrive before 2 p.m. local time, to allow Hotel Tiffany. Double occupancy. enough time to get through customs, arrive at the hotel and soak up some much deserved down time prior to dinner. Transportation to the hotel from the airport is on your own. Trip leaders will provide suggestions for available transportation options. After checking in to the hotel, you are free to explore the city on your own. We will meet at 5 p.m. in the lobby of the hotel for a group meeting followed by a welcome dinner. 2 Aug 22 Shuttle to Chamonix Overnight in Chamonix at B, D (Thurs) After breakfast at the hotel, we will shuttle to Chamonix. Hotel Le Morgane, a 4-star Lunch and afternoon activities are on your own. You can boutique hotel with on-site pool explore the charming ski town of Chamonix and gaze at the and spa. Double occupancy. massive Mont Blanc as you savor gelato or take the cable car to Aiguille du Midi for a 360-degree view of the French, Swiss, and Italian Alps. The summit terrace is at 12,605 feet with a spectacular view of Mont Blanc on a clear day. We will meet up for a group dinner. -
French Alps & the Jura
© Lonely Planet 238 A R JU E H T & S P L French Alps & the Jura NCH A RE HIGHLIGHTS F Conquering the Alpe d’Huez (p261) Teetering on the edge of the Gorges da la Bourne (p242) Slowly approaching the hilltop, medieval-fortified village of Nozeroy (p255) Conquering the highest pedalled pass – Col du Galibier 2645m (p241) TERRAIN Extremely mountainous in the Alps, and mainly rolling hills in the Jura with some real lung-crushers from time to time. Telephone Code – 03 www.franche-comte.org www.rhonealpestourisme.com Awesome, inspiring, tranquil, serene – superlatives rarely do justice to the spectacular landscapes of the French Alps and the Jura. Soaring peaks tower above verdant, forested valleys, alive with wild flowers. Mountain streams rush down from dour massifs, carving out deep gorges on their way. Mont Blanc, Grandes Jorasses and Barre des Écrins for mountaineers. Val d’Isère, Chamonix and Les Trois Vallées for adrenaline junkies. Vanoise, Vercors and Jura for great outdoors fans. So many mythical names, so many expectations, and not a hint of flagging: the Alps’ pulling power has never been so strong. What is so enticing about the Alps and the Jura is their almost beguiling range of qualities: under Mont Blanc’s 4810m of raw wilderness lies the most spectacular outdoor playground for activities ranging from skiing to canyoning, but also a vast historical and architectural heritage, a unique place in French cuisine (cheese, more cheese!), and some very happening cities boasting world-class art. So much for the old cliché that you can’t have it all. -
Courmayeur Val Ferret Val Veny La Thuile Pré-Saint-Didier Morgex La
Sant’Orso fair Sankt Orso-Messe Matterhorn Tourist Courmayeur Mont Blanc Office Aosta roman and Val Ferret medieval town Monte Rosa Tourismusbüro Aosta römische und Val Veny mittelalterliche Stadt Astronomic observatory La Thuile Astronomische Observatorium Courmayeur Piazzale Monte Bianco, 13 Pré-Saint-Didier C E R V I N O 11013 Courmayeur AO Tel (+39) 0165 842060 Morgex M O N T E Fax (+39) 0165 842072 A N C O Breuil-Cervinia R O B I Col / Tunnel du S La Salle E A [email protected] T Tunnel du Grand-Saint-Bernard N O Mont-Blanc M Valtournenche Gressoney La Thuile La Trinité St-Rhémy-en-Bosses étroubles Via M. Collomb, 36 Ayas Courmayeur Valpelline 11016 La Thuile AO Gressoney-St-Jean Tel (+39) 0165 884179 Pré-Saint-Didier St-Barthélemy AOSTA Châtillon Brusson Fax (+39) 0165 885196 Sarre dalle flavio [email protected] • La Thuile Col du Fénis St-Vincent Petit-Saint-Bernard Pila VIC T A N guide società O • M L Verrès E D O Issogne C Cogne R A Valgrisenche P Bard Office Régional Champorcher Valsavarenche du Tourisme Rhêmes-Notre-Dame O DIS P A A AR Pont-St-Martin R N P Ufficio Regionale CO RA NAZIONALE G del Turismo Torino turistici operatori consorzi • Milano V.le Federico Chabod, 15 Genova G 11100 Aosta R A O Spas N P A R A D I S Therme 360° view over the whole chain of the Alps Gran Paradiso 360° Aussicht auf die gesamte Alpenkette Fénis (1), Issogne (2), Verrès (3), www.lovevda.it Traverse of Mont Sarre (4) castles and Blanc Bard Fortress (5) Überquerung des Schlösser Fénis (1), Issogne (2) Mont Blanc Verrès (3) und Bard -
Caractérisation De La Qualité De L'air À Saint-Gervais-Les-Bains En 2007
Juin 2008 Caractérisation de la Qualité de l’Air à Saint-Gervais-les-Bains en 2007 - Rapport Final - L’Air de l’Ain et des Pays de Savoie 430, Rue de la Belle Eau - Z.I des Landiers Nord - 73000 CHAMBERY Tél. 04.79.69.05.43 - Fax. 04.79.62.64.59 - . e-mail: [email protected] Caractérisation de la Qualité de l’Air à Saint-Gervais-les-Bains en 2007 SOMMAIRE INTRODUCTION 3 1. Contexte de l’étude 4 1.1 Description du secteur d’étude 4 1.2. Choix des polluants à mesurer 4 2. Mise en oeuvre de la campagne de mesures 6 2.1. Moyens de mesures 6 2.2. Localisation des sites de mesures 6 2.3. Période de mesures 7 3. Commentaires météorologiques 8 4. Indice ATMO sur la vallée de Chamonix et la vallée de l’Arve 9 5. Le trafic routier 11 5.1. Profils hebdomadaires 11 5.2. Profils journaliers 12 5.3. Conclusions concernant le trafic et la qualité de l’air sur la zone 13 6. Caractérisation de la qualité de l’air 14 6.1. Evolution temporelle 14 6.2. Profils hebdomadaires 15 6.3. Niveaux moyens observés 17 7. Corrélation avec les stations de mesures fixes 19 8. Contributions locales et régionales des oxydants 20 9. Situation en regard des normes en vigueur 21 9.1. Les normes concernant la santé humaine 22 CONCLUSIONS 23 2 Caractérisation de la Qualité de l’Air à Saint-Gervais-les-Bains en 2007 INTRODUCTION Dans le cadre du plan de la surveillance de la qualité de l’air en Rhône-Alpes, les zones rurales et plus particulièrement les zones d’altitude constituent un axe fort de la politique d’évaluation de la réglementation de l’Air de l’Ain et des Pays de Savoie (Air-APS). -
Present-Day Uplift of the European Alps Evaluating Mechanisms And
Earth-Science Reviews 190 (2019) 589–604 Contents lists available at ScienceDirect Earth-Science Reviews journal homepage: www.elsevier.com/locate/earscirev Invited review Present-day uplift of the European Alps: Evaluating mechanisms and models T of their relative contributions ⁎ Pietro Sternaia, ,1, Christian Sueb, Laurent Hussonc, Enrico Serpellonid, Thorsten W. Beckere, Sean D. Willettf, Claudio Faccennag, Andrea Di Giulioh, Giorgio Spadai, Laurent Jolivetj, Pierre Vallac,k, Carole Petitl, Jean-Mathieu Nocquetm, Andrea Walpersdorfc, Sébastien Castelltorta a Département de Sciences de la Terre, Université de Genève, Geneva, Switzerland b Chrono-Environnement, CNRS, Université de Bourgogne Franche-Comté, Besançon, France c Université Grenoble Alpes, CNRS, IRD, IFSTAR, ISTERRE, Université Savoie Mont Blanc, Grenoble 38000, France d Istituto Nazionale di Geofisica e Vulcanologia, Centro Nazionale Terremoti, Bologna, Italy e Institute for Geophysics, Department of Geological Sciences, Jackson School of Geosciences, The University Texas at Austin, Austin, TX, USA f Erdwissenschaften, Eidgenössische Technische Hochschule Zürich (ETH), Zurich, Switzerland g Dipartimento di Scienze, Università di Roma III, Rome, Italy h Dipartimento di Scienze della Terra e dell'Ambiente, Università di Pavia, Pavia, Italy i Università degli Studi di Urbino “Carlo Bo”, Urbino, Italy j Sorbonne Université, Paris, France k Institute of Geological Sciences, Oeschger Center for Climate Research, University of Bern, Switzerland l Geoazur, IRD, Observatoire de la Côte d'Azur, CNRS, Université de Nice Sophia-Antipolis, Valbonne, France m Institut de Physique du Globe de Paris, Paris, France ARTICLE INFO ABSTRACT Keywords: Recent measurements of surface vertical displacements of the European Alps show a correlation between vertical European Alps velocities and topographic features, with widespread uplift at rates of up to ~2–2.5 mm/a in the North-Western Vertical displacement rate and Central Alps, and ~1 mm/a across a continuous region from the Eastern to the South-Western Alps. -
Guide Hiver 2020-2021
BIENVENUE WELCOME GUIDE VALLÉE HIVER 2020-2021 WINTER VALLEY GUIDE SERVOZ - LES HOUCHES - CHAMONIX-MONT-BLANC - ARGENTIÈRE - VALLORCINE CARE FOR THE INDEX OCEAN* INDEX Infos Covid-19 / Covid information . .6-7 Bonnes pratiques / Good practice . .8-9 SERVOZ . 46-51 Activités plein-air / Open-air activities ����������������� 48-49 FORFAITS DE SKI / SKI PASS . .10-17 Culture & Détente / Culture & Relaxation ����������� 50-51 Chamonix Le Pass ��������������������������������������������������������������������� 10-11 Mont-Blanc Unlimited ������������������������������������������������������������� 12-13 LES HOUCHES . 52-71 ��������������������������������������������� Les Houches ��������������������������������������������������������������������������������� 14-15 Ski nordique & raquettes 54-55 Nordic skiing & snowshoeing DOMAINES SKIABLES / SKI AREAS �����������������������18-35 Activités plein-air / Open-air activities ����������������� 56-57 Domaine des Houches . 18-19 Activités avec les animaux ����������������������������������������� 58-59 Le Tourchet ����������������������������������������������������������������������������������� 20-21 Activities with animals Le Brévent - La Flégère . 22-25 Activités intérieures / Indoor activities ����������������� 60-61 Les Planards | Le Savoy ��������������������������������������������������������� 26-27 Guide des Enfants / Children’s Guide . 63-71 Les Grands Montets ����������������������������������������������������������������� 28-29 Famille Plus . 62-63 Les Chosalets | La Vormaine ����������������������������������������������� -
Preview Editions Seb Constant Classic Routes in the Ecrins
4 - INTRODUCTION - This guidebook cannot be considered a substitute for practical training. INTRODUCTION p. 2 II - DESCRIPTIONS TABLE OF CONTENTS p. 4 2-1 VALLOUISE p. 32 MAP OF THE SECTORS p. 5 - Access map p. 32 - Bans Valley p. 33 I - PRACTICAL INFORMATION - Sélé Valley p. 36 1-1 THE ÉCRINS MASSIF p. 6 - Glacier Noir Basin p. 48 - Access p. 6 - Glacier Blanc Basin p. 52 - Geography p. 7 2-2 HAUTE-ROMANCHE p. 76 1-2 A LONG HISTORY p. 8 - Access map p. 77 - Early exploration/In Coolidge’s footsteps p. 8 - Goléon Basin p. 78 - Recent changes and future trends p. 10 - Source of the Romanche p. 82 - Tabuchet Basin p. 90 1-3 MOUNTAIN HAZARDS p. 11 - Girose Basin p. 96 - Risk and the modern approach to safety p. 11 2-3 VÉNÉON p. 106 - A modern approach to safety p. 13 - Access map p. 107 - Selle Valley p. 108 1-4 DIFFICULTY RATINGS p. 14 - Soreiller Basin p. 114 - A complete reassessment p. 14 - Étançons Valley p. 122 - Technical difficulty p. 15 - Temple Écrins Basin p. 130 - Overall difficulty p. 15 - Pilatte Basin p. 134 - Lavey Valley p. 146 1-5 HOW TO USE THIS GUIDE p. 18 - Muzelle Valley p. 152 - Summit/altitude of the top of the route p. 18 - Route name / Route characteristics p. 18 2-4 VALJOUFFREY p. 154 - First ascent: climbers and date p. 19 - Access map p. 154 - Photos and page numbers p. 20 - Font Turbat Valley p. 156 - Approach / Route / Descent p. 20 2-5 VALGAUDEMAR p. -
The Destiny of Orogen-Parallel Streams in the Eastern Alps: the Salzach–Enns Drainage System
Earth Surf. Dynam., 8, 69–85, 2020 https://doi.org/10.5194/esurf-8-69-2020 © Author(s) 2020. This work is distributed under the Creative Commons Attribution 4.0 License. The destiny of orogen-parallel streams in the Eastern Alps: the Salzach–Enns drainage system Georg Trost1, Jörg Robl2, Stefan Hergarten3, and Franz Neubauer2 1Department of Geoinformatics, Paris Lodron University of Salzburg, 5020 Salzburg, Austria 2Department of Geography and Geology, Paris Lodron University of Salzburg, 5020 Salzburg, Austria 3Institute of Earth and Environmental Sciences, Albert Ludwig University of Freiburg, 79104 Freiburg, Germany Correspondence: Georg Trost ([email protected]) Received: 1 August 2019 – Discussion started: 7 August 2019 Revised: 7 November 2019 – Accepted: 3 January 2020 – Published: 28 January 2020 Abstract. The evolution of the drainage system in the Eastern Alps is inherently linked to different tectonic stages of the alpine orogeny. Crustal-scale faults imposed eastward-directed orogen-parallel flow on major rivers, whereas late orogenic surface uplift increased topographic gradients between the foreland and range and hence the vulnerability of such rivers to be captured. This leads to a situation in which major orogen-parallel alpine rivers such as the Salzach River and the Enns River are characterized by elongated east–west-oriented catchments south of the proposed capture points, whereby almost the entire drainage area is located west of the capture point. To determine the current stability of drainage divides and to predict the potential direction of divide migration, we analysed their geometry at catchment, headwater and hillslope scale covering timescales from millions of years to the millennial scale. -
A Hydrographic Approach to the Alps
• • 330 A HYDROGRAPHIC APPROACH TO THE ALPS A HYDROGRAPHIC APPROACH TO THE ALPS • • • PART III BY E. CODDINGTON SUB-SYSTEMS OF (ADRIATIC .W. NORTH SEA] BASIC SYSTEM ' • HIS is the only Basic System whose watershed does not penetrate beyond the Alps, so it is immaterial whether it be traced·from W. to E. as [Adriatic .w. North Sea], or from E. toW. as [North Sea . w. Adriatic]. The Basic Watershed, which also answers to the title [Po ~ w. Rhine], is short arid for purposes of practical convenience scarcely requires subdivision, but the distinction between the Aar basin (actually Reuss, and Limmat) and that of the Rhine itself, is of too great significance to be overlooked, to say nothing of the magnitude and importance of the Major Branch System involved. This gives two Basic Sections of very unequal dimensions, but the ., Alps being of natural origin cannot be expected to fall into more or less equal com partments. Two rather less unbalanced sections could be obtained by differentiating Ticino.- and Adda-drainage on the Po-side, but this would exhibit both hydrographic and Alpine inferiority. (1) BASIC SECTION SYSTEM (Po .W. AAR]. This System happens to be synonymous with (Po .w. Reuss] and with [Ticino .w. Reuss]. · The Watershed From .Wyttenwasserstock (E) the Basic Watershed runs generally E.N.E. to the Hiihnerstock, Passo Cavanna, Pizzo Luceridro, St. Gotthard Pass, and Pizzo Centrale; thence S.E. to the Giubing and Unteralp Pass, and finally E.N.E., to end in the otherwise not very notable Piz Alv .1 Offshoot in the Po ( Ticino) basin A spur runs W.S.W. -
A New Rock Glacier Inventory from the Lombardy Region, Central Alps, Italy
Università degli Studi di Milano – Bicocca Dipartimento di Scienze dell’Ambiente e del Territorio e di Scienze della Terra SPATIAL AND TEMPORAL VARIABILITY OF GLACIERS AND ROCK GLACIERS IN THE CENTRAL ITALIAN ALPS (LOMBARDY REGION) Supervisor: Prof. Giovanni Battista CROSTA Co-supervisor: Dott. Francesco BRARDINONI Candidato: Riccardo SCOTTI Dottorato in Scienze della Terra Ciclo XXV° Contents 1. Introduction ........................................................................................................................ 1 1.1 Motivation ..................................................................................................................... 1 1.2 Aims .............................................................................................................................. 6 2. A regional inventory of rock glaciers and protalus ramparts in the Central Italian Alps (Lombardy region) .................................................................................................... 8 2.1 Abstract ......................................................................................................................... 8 2.2 Introduction ................................................................................................................ 10 2.3 Study area ................................................................................................................... 11 2.4 Methods ....................................................................................................................... 16 -
Evaluating the Effects of the Geography of Italy Geography Of
Name: Date: Evaluating the Effects of the Geography of Italy Warm up writing space: Review: What are some geographical features that made settlement in ancient Greece difficult? Write as many as you can. Be able to explain why you picked them. _____________________________________________________________________________________________ _____________________________________________________________________________________________ _____________________________________________________________________________________________ _____________________________________________________________________________________________ _____________________________________________________________________________________________ Give One / Get One Directions: • You will get 1 card with important information about Rome’s or Italy’s geography. Read and understand your card. • Record what you learned as a pro or a con on your T chart. • With your card and your T chart, stand up and move around to other students. • Trade information with other students. Explain your card to them (“Give One”), and then hear what they have to say (“Get One.”) Record their new information to your T chart. • Repeat! Geography of Italy Pros J Cons L Give one / Get one cards (Teachers, preprint and cut a set of these cards for each class. If there are more than 15 students in a class, print out a few doubles. It’s okay for some children to get the same card.) The hills of Rome Fertile volcanic soil 40% Mountainous The city-state of Rome was originally Active volcanoes in Italy (ex: Mt. About 40% of the Italian peninsula is built on seven hills. Fortifications and Etna, Mt. Vesuvius) that create lava covered by mountains. important buildings were placed at and ash help to make some of the the tops of the hills. Eventually, a land on the peninsula more fertile. city-wall was built around the hills. Peninsula Mediterranean climate Tiber River Italy is a narrow peninsula—land Italy, especially the southern part of The Tiber River links Rome, which is surrounded by water on 3 sides. -
A Case Study in the Italian Alps
Discussion Paper | Discussion Paper | Discussion Paper | Discussion Paper | Nat. Hazards Earth Syst. Sci. Discuss., 2, 7329–7365, 2014 www.nat-hazards-earth-syst-sci-discuss.net/2/7329/2014/ doi:10.5194/nhessd-2-7329-2014 NHESSD © Author(s) 2014. CC Attribution 3.0 License. 2, 7329–7365, 2014 This discussion paper is/has been under review for the journal Natural Hazards and Earth A case study in the System Sciences (NHESS). Please refer to the corresponding final paper in NHESS if available. Italian Alps Geomorphological surveys and software S. Devoto et al. simulations for rock fall hazard Title Page assessment: a case study in the Italian Abstract Introduction Alps Conclusions References Tables Figures S. Devoto, C. Boccali, and F. Podda Dipartimento di Matematica e Geoscienze, Università degli Studi di Trieste, Via Weiss, 2, J I Trieste, 34128, Italy J I Received: 29 October 2014 – Accepted: 17 November 2014 – Published: 5 December 2014 Back Close Correspondence to: S. Devoto ([email protected]) Full Screen / Esc Published by Copernicus Publications on behalf of the European Geosciences Union. Printer-friendly Version Interactive Discussion 7329 Discussion Paper | Discussion Paper | Discussion Paper | Discussion Paper | Abstract NHESSD In northern Italy, fast-moving landslides represent a significant threat to the population and human facilities. In the eastern portion of the Italian Alps, rock falls are recurrent 2, 7329–7365, 2014 and are often responsible for casualties or severe damage to roads and buildings. The 5 above-cited type of landslide is frequent in mountain ranges, is characterised by strong A case study in the relief energy and is triggered by earthquakes or copious rainfall, which often exceed Italian Alps 2000 mm yr−1.