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Upper Tour Du Mont Blanc on the Glaciers
UPPER TOUR DU MONT BLANC ON THE GLACIERS 4-day glacier trek An original way of doing the Tour du Mont Blanc, away from the classic trail. A beautiful way to discover glacier walking. Ideal for those who want to go hiking in the high mountains, but also a great preparation to try to climb the summit of Mont Blanc ... Association de tourisme CiE DES GUIDES ST GERVAIS ORGANISATION affiliée à l’APRIAM immatriculation ATOUT France IM073.10.0023 Garant financier : GROUPAMA police 4000713451/0 – R.C.P : MMA IARD contrat n°103.056.234 Code APE 8230Z – Siret : 440.287.076.000.10. – TVA intracommunautaire : FR18440287076 OUTLINE The previous day Appointment at 6.30 pm at the guides' office. Day 1 Departure from Cugnon in Contamines Montjoie. Go up to the Tré la Tête refuge where we will take lunch. We will continue the ascent to the Conscrits Refuge at 2600m. Introduction to crampon walking on the Tré la Tête glacier. Walking time: 6 to 7 hours. Elevation gain: +1500m Day 2 We will descend on the glacier of Tré la Tête that we will cross to go up that of Tondu. Climb to the summit of the Sugar Loaf of Tondu 3169m. We will descend to the Col du Tondu then to Robert Blanc refuge 2750m. Walking time 5h. Difference in height: + 800m / - 600m Day 3 From the refuge, after a short descent, we will go back up to gain to the Glacier des glaciers. We will go up towards to the Aiguille des Glaciers. We will cross it to join the Col Supérieur de la Seigne at 3000m. -
Permanet Final Conference
PermaNET Permafrost Long-term Monitoring Network Final Conference 2nd Circular June 28, 2011 – July 1, 2011 Centre de Congrés, Chamonix Mont-Blanc, France The PermaNET project Permafrost is highly sensitive to climatic changes. Permafrost degradation and related natural hazards affect traffic routes, tourism areas, settlements and infrastructures. The main problem is a lacking strategy for the consideration of these newly observed specific impacts of climate change in risk prevention and territorial development. With the joint development of a common strategy for dealing with permafrost and related hazards under changing climatic conditions and the creation of an Alpine- wide monitoring network the project aims at preventing natural hazards, at contributing to sustainable territorial development and at the implementation of good governance practices. Results of the PermaNET project are an Alpine-wide permafrost monitoring network, a permafrost map for the entire Alpine Space guidelines for the consideration of permafrost in natural hazard and risk management guidelines for the consideration of permafrost in water resources management. These results will be presented at the final project conference. The Alpine Space permafrost monitoring network PermaNET collected metadata of the most important permafrost monitoring sites and compiled it into a standardized permafrost monitoring network. On key monitoring sites, new monitoring stations have been installed and instrumented. PermaNET provides recommendations for policy-makers for building up national monitoring networks on national and regional scale and a handbook for the installation and maintenance of an Alpine-wide permafrost monitoring network with standards for data acquisition. Alpine Space permafrost map PermaNET collected and compiled permafrost evidences into an inventory of permafrost evidences and elaborated an Alpine-wide map of the permafrost distribution. -
4000 M Peaks of the Alps Normal and Classic Routes
rock&ice 3 4000 m Peaks of the Alps Normal and classic routes idea Montagna editoria e alpinismo Rock&Ice l 4000m Peaks of the Alps l Contents CONTENTS FIVE • • 51a Normal Route to Punta Giordani 257 WEISSHORN AND MATTERHORN ALPS 175 • 52a Normal Route to the Vincent Pyramid 259 • Preface 5 12 Aiguille Blanche de Peuterey 101 35 Dent d’Hérens 180 • 52b Punta Giordani-Vincent Pyramid 261 • Introduction 6 • 12 North Face Right 102 • 35a Normal Route 181 Traverse • Geogrpahic location 14 13 Gran Pilier d’Angle 108 • 35b Tiefmatten Ridge (West Ridge) 183 53 Schwarzhorn/Corno Nero 265 • Technical notes 16 • 13 South Face and Peuterey Ridge 109 36 Matterhorn 185 54 Ludwigshöhe 265 14 Mont Blanc de Courmayeur 114 • 36a Hörnli Ridge (Hörnligrat) 186 55 Parrotspitze 265 ONE • MASSIF DES ÉCRINS 23 • 14 Eccles Couloir and Peuterey Ridge 115 • 36b Lion Ridge 192 • 53-55 Traverse of the Three Peaks 266 1 Barre des Écrins 26 15-19 Aiguilles du Diable 117 37 Dent Blanche 198 56 Signalkuppe 269 • 1a Normal Route 27 15 L’Isolée 117 • 37 Normal Route via the Wandflue Ridge 199 57 Zumsteinspitze 269 • 1b Coolidge Couloir 30 16 Pointe Carmen 117 38 Bishorn 202 • 56-57 Normal Route to the Signalkuppe 270 2 Dôme de Neige des Écrins 32 17 Pointe Médiane 117 • 38 Normal Route 203 and the Zumsteinspitze • 2 Normal Route 32 18 Pointe Chaubert 117 39 Weisshorn 206 58 Dufourspitze 274 19 Corne du Diable 117 • 39 Normal Route 207 59 Nordend 274 TWO • GRAN PARADISO MASSIF 35 • 15-19 Aiguilles du Diable Traverse 118 40 Ober Gabelhorn 212 • 58a Normal Route to the Dufourspitze -
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. -
The Eiger Myth Compiled by Marco Bomio
The Eiger Myth Compiled by Marco Bomio Compiled by Marco Bomio, 3818 Grindelwald 1 The Myth «If the wall can be done, then we will do it – or stay there!” This assertion by Edi Rainer and Willy Angerer proved tragically true for them both – they stayed there. The first attempt on the Eiger North Face in 1936 went down in history as the most infamous drama surrounding the North Face and those who tried to conquer it. Together with their German companions Andreas Hinterstoisser and Toni Kurz, the two Austrians perished in this wall notorious for its rockfalls and suddenly deteriorating weather. The gruesome image of Toni Kurz dangling in the rope went around the world. Two years later, Anderl Heckmair, Ludwig Vörg, Heinrich Harrer and Fritz Kasparek managed the first ascent of the 1800-metre-high face. 70 years later, local professional mountaineer Ueli Steck set a new record by climbing it in 2 hours and 47 minutes. 1.1 How the Eiger Myth was made In the public perception, its exposed north wall made the Eiger the embodiment of a perilous, difficult and unpredictable mountain. The persistence with which this image has been burnt into the collective memory is surprising yet explainable. The myth surrounding the Eiger North Face has its initial roots in the 1930s, a decade in which nine alpinists were killed in various attempts leading up to the successful first ascent in July 1938. From 1935 onwards, the climbing elite regarded the North Face as “the last problem in the Western Alps”. This fact alone drew the best climbers – mainly Germans, Austrians and Italians at the time – like a magnet to the Eiger. -
Aiguille D'entreves
AIGUILLE D’ENTREVES 3600m Accès par l’Italie et le téléphérique de la Pointe Helbronner. Marche d’approche sur glacier puis escalade sur une arête Objectif : rocheuse. Niveau requis: pour des personnes ayant une expérience de Mise en pratique l’escalade. des cours d’escalade sur une belle arête de granite Descriptif Niveau : Avec la traversée des Aiguilles d’Entrèves nous abordons la 1 pas de IV Pour course rocheuse en haute montagne et ses paysages toutes fantastiques. Après une approche glaciaire (1h) nous personnes ayant parcourons la très belle et très effilée arête de granit ocre une expérience (2h). Après la descente du sommet nous rejoignons notre trace de la Varappe d’approche que nous suivons jusqu’au téléphérique de la pointe Helbronner. Points forts : Cadre somptueux au cœur du Massif du Mont Blanc, des passages aériens et quelques pas de Varappe. Bureau des Guides de Megève Tel : 04 50 21 55 11 76 rue Ambroise Martin Email : [email protected] 74120 Megève Site internet : www.guides-megeve.com LA PETITE AIGUILLE VERTE Située dans un cadre fantastique: devant la face nord des Drus Objectif et le versant Nant Blanc de l’Aiguille Verte, la Petite Verte est une très bonne course d’initiation en terrain mixte. Petit sommet technique Accès par le téléphérique des Grands Montets ( 3295 m). Niveau Temps : la matinée ou l’après midi 4H. assez difficile Prévoir des lunettes de Descriptif soleil adapté à l’altitude De la station supérieure du téléphérique des Grands Montets on gagne le col des Grands Montets et on traverse le glacier. -
JAMES HART DYKE Whymper’S Mountains 150 Years on JAMES HART DYKE Whymper’S Mountains 150 Years On
JAMES HART DYKE Whymper’s Mountains 150 years on JAMES HART DYKE Whymper’s Mountains 150 years on 12 - 25 November 2015 Monday - Friday, 10am - 5pm at John Mitchell Fine Paintings 44 Old Bond Street, London W1S 4GB All paintings are for sale unless otherwise stated Please contact William Mitchell on 020 7493 7567 [email protected] JOHN MITCHELL FINE PAINTINGS EST 1931 2 Over thirty-one days in June This catalogue has been compiled to accompany an 3 and July 1865, Whymper and exhibition of over thirty oil paintings and sketches by his guides climbed five James Hart Dyke made to commemorate a remarkable mountains and crossed series of first ascents by the Victorian artist-turned- eleven passes. Four of those summits were first ascents mountaineer, Edward Whymper (1840-1911). including the Grandes One hundred and fifty years ago, in 1865, Whymper became the first person to climb the Jorasses and the Aiguille Matterhorn; a triumph that concluded an extraordinary career as the most courageous Verte, ascending just over and determined mountaineer of his generation. In fact, it has been widely suggested that 100,000 feet in the process. Whymper was a generation ahead of his peers in terms of what he accomplished in the mountains. And he had done it all by the time he was twenty-five years old. This summer the narrative landscapist, James Hart Dyke, spent his own ‘season’ in the Alps. For over two weeks in August he trekked and climbed, retracing where possible Whymper’s footsteps. Over a period of thirty-one days in June and July 1865, Whymper and his guides climbed five mountains and crossed eleven passes. -
Fondements Scientifiques En Vue De La Création D'une Zone De Protection
Asters - CEN Haute-Savoie 84 route du Viéran PRINGY 74370 ANNECY Tél. 04 50 66 47 51 www.cen-haute-savoie.org Fondements scientifiques En vue de la création d’une zone de protection d’habitat naturel du Mont-Blanc - Site d’exception ● Rédaction Bernard Bal, Olivier Billant, Jean-Baptiste Bosson et Lisa Wirtz 28 avril 2020 ● NOTE RÉALISÉE AVEC LE SOUTIEN FINANCIER DE de la Haute-Savoie Table des matières Remerciements 4 Préambule : Protéger le toit de l’Europe 4 1. Éléments de contexte 5 1.1. Un concentré de superlatifs 5 1.2. Un massif sous pression à l’Anthropocène 5 1.2.1. Un bouleversement climatique sans précédent dans l’Histoire 5 1.2.2. L’enjeu de la fréquentation 8 2. Analyse topographique de la zone de protection proposée 9 3. Patrimoine géologique et hydrologique 11 3.1. Géologie 11 3.2. Géomorphologie et hydrologie 12 3.2.1. Formes et processus glaciaires 13 3.2.2. Formes et processus périglaciaires et gravitaires 21 3.2.3. Formes et processus torrentiels et lacustres 25 3.3. Richesse, état et enjeux de conservation du patrimoine géologique et hydrologique 27 4. Patrimoine biologique 30 4.1. Habitats 30 4.1.1. Sources de données 30 4.1.2. Liste des habitats / commentaire 31 4.1.3. Cartographie / analyse 32 4.1.4. Etat de conservation /menaces / sensibilité 33 4.2. Flore 36 4.2.1. Sources de données 36 4.2.2. Liste des espèces / commentaires 36 4.2.3. Cartographie / Analyse 37 4.2.4. Etat de conservation / menaces / sensibilité 37 4.3. -
Steep Rise of the Bernese Alps
Corporate Communication Media release, 24 March 2017 EMBARGOED UNTIL FRIDAY 24 MARCH 2017 11:00H CET Steep rise of the Bernese Alps The striKing North Face of the Bernese Alps is the result of a steep rise of rocKs from the depths following a collision of two tectonic plates. This steep rise gives new insight into the final stage of mountain building and provides important knowledge with regard to active natural hazards and geothermal energy. The results from researchers at the University of Bern and ETH Zürich are being published in the «Scientific Reports» specialist journal. Mountains often emerge when two tectonic plates converge, where the denser oceanic plate subducts beneath the lighter continental plate into the earth’s mantle according to standard models. But what happens if two continental plates of the same density collide, as was the case in the area of the Central Alps during the collision between Africa and Europe? Geologists and geophysicists at the University of Bern and ETH Zürich examined this question. They constructed the 3D geometry of deformation structures through several years of surface analysis in the Bernese Alps. With the help of seismic tomography, similar to ultrasound examinations on people, they also gained additional insight into the deep structure of the earth’s crust and beyond down to depths of 400 km in the earth’s mantle. Viscous rocKs from the depths A reconstruction based on this data indicated that the European crust’s light, crystalline rocks cannot be subducted to very deep depths but are detached from the earth’s mantle in the lower earth’s crust and are consequently forced back up to the earth’s surface by buoyancy forces. -
13 Protection: a Means for Sustainable Development? The
13 Protection: A Means for Sustainable Development? The Case of the Jungfrau- Aletsch-Bietschhorn World Heritage Site in Switzerland Astrid Wallner1, Stephan Rist2, Karina Liechti3, Urs Wiesmann4 Abstract The Jungfrau-Aletsch-Bietschhorn World Heritage Site (WHS) comprises main- ly natural high-mountain landscapes. The High Alps and impressive natu- ral landscapes are not the only feature making the region so attractive; its uniqueness also lies in the adjoining landscapes shaped by centuries of tra- ditional agricultural use. Given the dramatic changes in the agricultural sec- tor, the risk faced by cultural landscapes in the World Heritage Region is pos- sibly greater than that faced by the natural landscape inside the perimeter of the WHS. Inclusion on the World Heritage List was therefore an opportunity to contribute not only to the preservation of the ‘natural’ WHS: the protected part of the natural landscape is understood as the centrepiece of a strategy | downloaded: 1.10.2021 to enhance sustainable development in the entire region, including cultural landscapes. Maintaining the right balance between preservation of the WHS and promotion of sustainable regional development constitutes a key chal- lenge for management of the WHS. Local actors were heavily involved in the planning process in which the goals and objectives of the WHS were defined. This participatory process allowed examination of ongoing prob- lems and current opportunities, even though present ecological standards were a ‘non-negotiable’ feature. Therefore the basic patterns of valuation of the landscape by the different actors could not be modified. Nevertheless, the process made it possible to jointly define the present situation and thus create a basis for legitimising future action. -
Alps Village to Village Hiking
Alps Village to Village Hiking 10 Days Alps Village to Village Hiking Experience picturesque alpine hamlets and sweeping mountain vistas in Switzerland and France on this unforgettable hiking trilogy of the Alps. Tackle the legendary Eiger Trail at the foot of the Eiger's notorious north face, which has challenged mountaineers for over a century. Traverse canyon trails to discover imposing views of the iconic Matterhorn, and complete your tour in Chamonix, where the majestic Mont Blanc looms over the charming town. From Grindelwald to Zermatt to Chamonix, this 10-day tour will inspire and challenge even the most seasoned hiker. Details Testimonials Arrive: Geneva, Switzerland “This trip takes you to some of the most iconic hikes in the world. My only disappointment was that the Depart: Geneva, Switzerland trip was over! Great guides and wonderful hikes.” David M. Duration: 10 Days Group Size: 5-16 Guests "I've taken six MTS trips and they have all exceeded my expectations. The staff, the food, the logistics and Minimum Age: 18 Years Old the communications have always been exceptional. Thank you for being my "go to" adventure travel Activity Level: company!" Margaret I. REASON #01 REASON #02 REASON #03 This MT Sobek-crafted itinerary MT Sobek's expert guides have MT Sobek has been taking covers the must-see Alps in been leading treks in this region our travelers to the Alps since only 10 days — see the Eiger, for nearly 50 years, and this 1970 — we know the best hikes Matterhorn and Mont Blanc. grand tour is not to be missed. -
Alpine Summer Farms – Upland Animal Husbandry and Land Use Strategies in the Bernese Alps (Switzerland)
Special Volume 3 (2012), pp. 279–283 Brigitte Andres Alpine Summer Farms – Upland Animal Husbandry and Land Use Strategies in the Bernese Alps (Switzerland) in Wiebke Bebermeier – Robert Hebenstreit – Elke Kaiser – Jan Krause (eds.), Landscape Archaeology. Proceedings of the International Conference Held in Berlin, 6th – 8th June 2012 Edited by Gerd Graßhoff and Michael Meyer, Excellence Cluster Topoi, Berlin eTopoi ISSN 2192-2608 http://journal.topoi.org Except where otherwise noted, content is licensed under a Creative Commons Attribution 3.0 License: http://creativecommons.org/licenses/by/3.0 Brigitte Andres Alpine Summer Farms – Upland Animal Husbandry and Land Use Strategies in the Bernese Alps (Switzerland) Alpine archaeology; survey; ‘Alpwirtschaft;’ building remains; cultural landscape; Middle Ages; Modern Age. Introduction In 2003, 2004 and 2006 the Archaeological Service of the Canton of Bern carried out alpine archaeological surveys in three valleys of the Bernese Oberland.1 The primary aim of the survey was to enlarge the list of archaeological sites based on which the Archaeo- logical Service reacts to construction projects. The results were a positive surprise. About 400 new archaeological sites—mostly dating to the Middle Ages and Modern Age—could be recorded. A doctoral project will analyse the results of the field surveys.2 The archaeological structures found include remains of building foundations, installa- tions beneath rock shelters, animal pens and field boundary walls. They relate to seasonal alpine animal husbandry (‘Alpwirtschaft’), which has been an important economic factor in this region since the Middle Ages. In addition tracks and pathways, ore extraction sites and sites related to other industrial activities were documented.