Région Du Sanetsch Et De Tsanfleuron
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The Alpina Gstaad Announces New Winter Programs for Active Couples and Families in the Swiss Alps
The Alpina Gstaad Announces New Winter Programs for Active Couples and Families in the Swiss Alps GSTAAD, Switzerland, October 24, 2017 – The Alpina Gstaad, the award-winning hotel in the Swiss Alpine village of Gstaad, has announced two new packages for the 2017-2018 winter season to appeal to couples looking for romance and families who want to bond. The hotel’s new Alpine Couples package specializes in romance with a private helicopter that will whisk the couple up to charming Refuge L'Espace at the top of Glacier 3000. This rustic and cozy hideaway sits next to a mammoth peak in the Diablerets massif called the Quille du Diable (the Devil's Bowling Pin). Skiers-in-the- know are lured by the delicious regional specialties from the Bernese Oberland and the fabulous views into the Val Derborence in the Valais. (An optional tour around the Matterhorn can also be added.) Later, the couple can take a romantic horse-drawn carriage ride around the tranquil village of Lauenen and then have a massage for two in the hotel's Six Senses Spa. A five-course tasting menu at the Michelin-starred Restaurant Sommet and exclusive use of the private cinema for an evening with complimentary popcorn, snacks and drinks will inspire romance. The package starts from Swiss francs (CHF) 5,200 (about $5,300) for two in a Junior Suite for two nights and also includes breakfast, a daily credit of CHF100 per person, per day for food and beverage consumption in the hotel's three restaurants, free access to pools, saunas, steam-baths and relaxation areas at the Spa, parking, service charge, all taxes and VAT. -
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. -
Ein Paar Tips a Few Tips Quelques Recommandations
Arpelistock QUELQUES RECOMMANDATIONS 3035m Munissez-vous de bonnes chaussures, de vêtements imperméables, de lunettes de soleil, d’un pique-nique et Spitzhorn éventuellement de bâtons. Pour les longues marches, dosez vos efforts en rapport avec votre entraînement. 2807m Utilisez les transports publics qui faciliteront vos approches et vos retours. La Fava 2812m Sanetschhorn Mont Gond Il peut y avoir des troupeaux de vaches allaitantes, des mères à l’instinct protecteur marqué. Il convient de Oldenhorn passer discrètement et à bonne distance des animaux sans les caresser ou les effrayer et surtout de tenir les Lac de Sanetsch 2924m 2710m 3123m Cabane de Prarochet chiens en laisse. Lorsque vous traversez des Réserves Naturelles, respectez la faune et la flore protégées qui 28 Gstellihorn 2555m vous entourent et qui sont si précieux à notre écosystème. Schluchhorn 2820m 28 GLACIER Malgré toute l’attention portée à la signalisation et l’entretien de ce vaste réseau de promenades, des indi- 2579m 3000 Quille du diable 2860m cations peuvent disparaître, des marques être détruites par des incidents de la nature. Veuillez avoir la gen- Scex Rouge 27 28 26 27 28 2971m tillesse d’informer l’Office du Tourisme des lacunes ou détériorations que vous pourriez constater. D’avance nous vous remercions de cette précieuse collaboration bénévole. Wittenberghorn Cabane des Diablerets 26 2485m le Dôme 2650m 2986m Profitez de prendre un merveilleux “bol d’air pur”, tout en respectant la nature (faune et flore), et maintenant Vers Gstaad Peak Walk Sommet des Diablerets Gsteig 3210m nous vous souhaitons une “bonne promenade”. Tête aux Chamois Les auteurs de cette carte déclinent toute responsabilité en cas d’accident lors d’une randonnée. -
Geovision 35 New1
Geoheritage popularisation and cartographic visualisation in the Tsanfleuron-Sanetsch area (Valais, Switzerland) Martin, S. (2010). Geoheritage popularisation and cartographic visualisation in the Tsaneuron-Sanetsch area (Valais, Switzerland). Dans G. Regolini-Bissig & E. Reynard (Éds), Mapping Geoheritage (pp. 15–30). Lausanne: Université, Institut de géographie. Simon Martin Institute of Geography University of Lausanne Anthropole CH - 1015 Lausanne E-Mail: [email protected] In Regolini-Bissig G., Reynard E. (Eds) (2010). Mapping Geoheritage, Lausanne, Institut de géographie, Géovisions n°35, pp. 15-30. Geoheritage popularisation and cartographic visualisation - 17 - 1. Introduction This paper presents the underlying concepts developed by the Institute of Geography of the University of Lausanne (Switzerland) for a popularisation project of the geohe- ritage in the Tsanfleuron-Sanetsch area (Valais, Switzerland). Due to its wide scientific interest, the local geoheritage is of great value (Reynard, 2008). The article details the complementary links existing between the different parts of a geotourist project – databases, educational panels, educational material and geotourist map – developed for popularising the geoheritage value of the area. Each element of the project is briefly presented. Special focus is set on mapping questions: how cartographic design and information structure can be set in order to facilitate map’s use and comprehen- sion. In this way, the Tsanfleuron-Sanetsch map is presented as an applied example of the guiding principles proposed by Coratza and Regolini-Bissig (2009). 2. Geoheritage in the Tsanfleuron-Sanetsch area 2.1 Access and location The area of Tsanfleuron is part of Les Diablerets mountain massif (Fig. 1). There are two main entrance points linked by hiking trails. -
Glacier 3000, Les Diablerets ANNEXE C Porteur De Projet
Domaine skiable : Glacier 3000, Les Diablerets ANNEXE C Porteur de projet : Gstaad 3000 AG 2.3.2 Commune(s) concernée(s) : Ormont-Dessus Nom du projet : Renouvellement de la station du Col du Pillon Classification du projet : Offre régionale Description du projet La principale porte d’entrée du domaine d’altitude de Glacier 3000 est assurée par l’axe Col du Pillon – Cabane - Scex Rouge. Après les aménagements réalisés au Sex Rouge, la nouvelle piste Red Run entre le Sex Rouge et la Tête aux Chamois, ainsi que la réalisation projetée de la liaison avec le Col du Pillon via Pierres Pointes, une partie de la station du Pillon doit être renouvelée de par la vétusté de ses installations. Le bâtiment en question, qui abrite notamment les locaux techniques, les ateliers et les vestiaires, a plus de 50 ans et ne répond plus aux exigences en matière de praticabilité par rapport aux dimensions actuelles des machines, ni en termes d’isolation, de sécurité et de confort minimum pour les employés. De plus, il ne s’intègre pas au site et aux bâtiments récents. Le futur bâtiment reprendra l’architecture de la station existante et s’installera dans son prolongement. Outre les locaux destinés aux employés, il comprendra toutes les fonctionnalités nécessaires pour l’entretien technique des installations, ainsi que les bureaux de Glacier 3000. Mesures environnementales Le nouveau bâtiment sera équipé de panneaux solaires et sera aux normes supérieures en termes d’isolation et d’efficience énergétique. La démolition du bâtiment existant permettra un réaménagement cohérent des espaces arrière du Col du Pillon et la création de relations plus spontanées avec les milieux naturels environnants, notamment les falaises de gypse et les dolines. -
Cretaceous Syn-Sedimentary Faulting in the Wildhorn Nappe (SW Switzerland)
Swiss J Geosci (2014) 107:223–250 DOI 10.1007/s00015-014-0166-8 Cretaceous syn-sedimentary faulting in the Wildhorn Nappe (SW Switzerland) G. L. Cardello • Neil S. Mancktelow Received: 25 August 2013 / Accepted: 2 September 2014 / Published online: 7 October 2014 Ó Swiss Geological Society 2014 Abstract During Cretaceous time, the area of the future subsequent sediments reflect a passive adaption to the pre- Helvetic nappes (Central Alps, south-western Switzerland) existing topography of the sea floor, established during the was part of a large ramp-type carbonate depositional sys- earlier tectonic movements. (4) Post-Maastrichtian north- tem on the European margin, in which the area of the directed tilt and erosion. In the Wildhorn Nappe, palaeo- Wildhorn Nappe was transitional to the more distal and fault activity most probably ended in the Early Maas- relatively deeper Ultrahelvetic basin. The Wildhorn Nappe trichtian rather than continuing into the Eocene. Until now, includes an Upper Cretaceous succession bearing clear the regional importance and magnitude of Late Cretaceous evidence for syn-sedimentary normal faulting, such as syn- extension has not been recognized in the Helvetic domain. sedimentary geometries related to well oriented NE-strik- This widespread event may be related to post-breakup ing faults, sedimentary dykes, lateral variations in the extensional tectonics along the European margin or, alter- thickness and facies of formations, anomalous and discor- natively but less likely, to lateral gravitational collapse of dant contacts corresponding to palaeo-escarpments, and the margin. slump folds. Four stages of syn-sedimentary fault activity have been recognized. (1) Post-Cenomanian disruption and Keywords Central Alps Á Helvetic nappes Á exhumation of the Schrattenkalk platform related to dis- Cretaceous extensional faults Á Post-breakup tectonics Á tributed normal faulting, which contributed to the initiation Carbonate depositional systems Á Multiple fault systems of karst erosion on topographic highs and sedimentation in topographic lows. -
Geological Structure, Recharge Processes and Underground Drainage of a Glacierised Karst Aquifer System, Tsanfleuron-Sanetsch, Swiss Alps
Published in Hydrogeology Journal 17, issue 8, 1833-1848, 2009 1 which should be used for any reference to this work Geological structure, recharge processes and underground drainage of a glacierised karst aquifer system, Tsanfleuron-Sanetsch, Swiss Alps Vivian Gremaud & Nico Goldscheider & Ludovic Savoy & Gérald Favre & Henri Masson Keywords Karst . Retreating glacier . Multi-tracer test . Climate change . Switzerland Abstract The relationships between stratigraphic and probably enlarged by mass movements; (3) the variability tectonic setting, recharge processes and underground of glacial meltwater production influences the shape of the drainage of the glacierised karst aquifer system ‘Tsan- tracer breakthrough curves and, consequently, flow and fleuron-Sanetsch’ in the Swiss Alps have been studied by transport in the aquifer. means of various methods, particularly tracer tests (19 injections). The area belongs to the Helvetic nappes and consists of Jurassic to Palaeogene sedimentary rocks. Introduction Strata are folded and form a regional anticlinorium. Cretaceous Urgonian limestone constitutes the main karst The Alps are often considered as the ‘water towers of aquifer, overlain by a retreating glacier in its upper part. Europe’. Just as in most other high mountain areas, annual Polished limestone surfaces are exposed between the precipitation is substantially higher than in the surround- glacier front and the end moraine of 1855/1860 (Little fi ing lowlands; the snow that falls in the cold season is Ice Age); typical alpine karren elds can be observed retained in snowfields and glaciers, from which it is further below. Results show that (1) large parts of the area slowly released during warmer periods to provide large are drained by the Glarey spring, which is used as a volumes of freshwater to springs, streams, rivers and drinking water source, while marginal parts belong to the fl aquifers (e.g. -
EGU Poster ES to Print
Late-glacial to Holocene sediment dynamics in high Alpine regions Insights from multimethodological approach on aeolian deposits (Sanetsch Pass, Switzerland) Elena Serra1,2, Pierre G. Valla3,1,2, Natacha Gribenski1,2, Luc Braillard4 1Institute of Geological Sciences, University of Bern, Switzerland 3Institute of Earth Sciences, CNRS - University Grenoble Alpes, France 2Oeschger Centre for Climate Change Research, University of Bern, Switzerland 4Department of Geosciences, University of Fribourg, Switzerland Email: [email protected] 5°0'E 10°0'E 15°0'E Fig. 2 Grain size distribution and sorting 7°16'E 7°18'E Clay Silt Sand GravelPebl. Bould. OSL (total counts) 100.00 (ARP and CRE). Both grain size distributions Sedimentology 48°0'N (cm) Layers Introduction and sorting indices suggest an aeolian origin Depth 0 10000 20000 30000 40000 1 1 5 8 1 75.00 of ARP and the fine layers of CRE, confirming ARP01 ARP02 ARP03 2 15 2 Widespread loess deposits accumulated the on-field logging. 3 25 3 2 35 4 Depth (cm) during the last glaciations in low-eleva- 46°0'N Arpelistock 50.00 4 5 46°21'N 40 (3036 m.s.l.) 5 8.8±1.1 ka Fig. 4 Stratigraphy, portable OSL counts and conventional tion regions of Europe and are often 25.00 3.1±0.4 ka 2.7±0.4 ka Weigth percentage (%) percentage Weigth IRSL ages of the high-elevation aeolian deposits (ARP). A com- [1, Sediments used as paleo-environmental archives 44°0'N CRE Weathered pebbles plex picture emerges from the luminescence analyses. -
Collection EDYTEM Editorial Par Xavier BERNIER
KARSTS DE MONTAGNE Laboratoire GEOMORPHOLOGIE, PATRIMOINE ET RESSOURCES Avant-Propos par Jean-Jacques DELANNOY, directeur du laboratoire EDYTEM ........................................................3 Collection EDYTEM Editorial par Xavier BERNIER .......................................................................................................................................5 Environnements, Dynamiques et Territoires de la Montagne Liste des participants au colloque et des auteurs ..............................................................................................................6 Sommaire Sommaire .........................................................................................................................................................................7 Numéro 7 - Année 2008 Première partie - Les interactions entre transport et tourisme - Réflexions.............................................................9 Transport et mise en tourisme du Monde, par Jean-Christophe GAY......................................................................11 De la relation entre transport et lieux touristiques, par Philippe DUHAMEL..........................................................23 Tourisme et enclavement : l’exemple du Massif Central français, par Christian JAMOT.......................................33 Cahiers de Géographie Retranscription des débats - Session 1 ...............................................................43 Deuxième partie - L’accès aux destinations touristiques...........................................................................................45 -
Peak to Peak at 3,000 M
Official Partner Unique glacier ski area at an altitude of 3,000 m from October to May Free parking, 20 minutes from Gstaad, Peak to Peak 40 minutes from Montreux at 3,000 m. 28 KM OF SLOPES FREERIDE PARADISE NEW RED RUN SLOPE Challenging Olden slope, 7 km High alpine terrain with countless routes Attractive 8km slope from 3000m 9 Glacier slopes in all levels of difficulty down to 1300m. Quille du Diable, 2908 m Dôme, 3016 m Les Diablerets, 3209 m b d P10 P11 P12 Scex Rouge, 2971 m La Fava, 2612 m Oldenhorn P9 3123 m Sanetschhorn, 2923 m Alpine Coaster P5 NEW Cabane, 2525 m P2 P6 Oldenalp Oldenegg, 1919 m 1834 m P3 Les Diablerets, 1200 m P1 Col du Pillon, 1546 m Basel Zürich Glacier 3000 Luzern Col du Pillon Reusch, 1350 m Bern Diablerets – Gstaad Gstaad P8 08/2017 Lausanne Spiez Interlaken Montreux Infoline +41 (0) 848 00 3000 Gstaad Glacier 3000 Phone +41 (0) 24 492 33 77 Aigle Les Diablerets Villars Information about operating hours on www.glacier3000.ch . Operations subject to weather conditions. Genève [email protected] www.glacier3000.ch www.glacier3000.ch 5 VIEW POINT 3’000 M PEAK WALK BY TISSOT included QUILLE DU DIABLE 2’908 m DIABLERETS 3’209 m REFUGE L’ESPACE SCEX ROUGE 2’971 m 7 4 WATCH & SOUVENIR SHOP RESTAURANT BOTTA SELF-SERVICE ICE EXPRESS SUN TERRACE included CONFERENCES 8. GLACIER WALK Cable car ride of 15 minutes, 1 change, 125 persons per cable car, first ascent Year-round scenic walk over the glacier at 9 am, courses every 20 minutes. -
Understanding the Frequency and Magnitude of Debris Flows on Alpine Talus Slopes Hérens Valley and Col Du Sanetsch (Switzerland)
Understanding the frequency and magnitude of debris flows on Alpine talus slopes Hérens Valley and Col du Sanetsch (Switzerland) Word count: 18 729 Annelies De Bruyne Student number: 01307441 Supervisor: Dr. Amaury Frankl1 Advisor: MSc. Hanne Hendrickx1, Local supervisor: Prof. dr. Reynald Delaloye2 1Department of Geography, Faculty of Science, Ghent University 2Department of Geosciences, Faculty of Science, University of Fribourg A dissertation submitted to Ghent University in partial fulfilment of the requirements for the degree of Master of Science in Geography. Academic year: 2017 - 2018 PREFACE Writing and working on the dissertation has been a very enriching experience to me. The fulfilment of the dissertation could not have been possible without the support of many people. First of all, I would like to thank my supervisor, Dr. Amaury Frankl, my advisor, MSc. Hanne Hendrickx and the local supervisor Prof. Dr. Reynald Delaloye for the opportunity to carry out the dissertation in the Swiss Alps. They played an important role in the setup of the whole dissertation. Their feedback and instructions were crucial to accomplish this document. Secondly, I would also like to express my gratitude to Bart De Wit and Britt Lonneville for their technical support during the drone campaign. I would also like to thank my family, mountaineering friends and fellow geography students for encouraging me during the five weeks of field work in Switzerland and afterwards when starting to write the thesis. Hopefully, more future students will also see the potential of working and studying in the geomorphological rich environment that is offered by the Alps. 1 TABLE OF CONTENTS POPULARIZED TEXT ............................................................................................................................ -
Presskits Summer 2021
Contents. Valais. Valais in Dear10 friends of Valais, figures. 3 10 top summer4 Our Valais is experiences.a region of enchanting landscapes full of Top 10 5places contrasts, a uniquefor land that we invite youhot to get to know days. during the summer season. We hope this will be less Cycling. 6 affected by the Coronavirus crisis than the preceding Mountain biking. 11 summer, and that it will be able to offer our guests once Hiking/trail running. 16 again a wide range of festive, sporting, gastronomic and Excursions. 22 cultural activities and events. Flavours of Valais. 26 Relaxation, spas and In this presswellbeing. pack, let yourself be guided by the best of31 Families. 35 the Valais summer. Together with information on outdoor Culture and traditions.activities, food and wine, culture and39 many other attractions, Innovation. 45 you will also find details of what’s new in Valais and learn Autumn. 49 about inspiring people who find inspiration in our region. Meet Mikaël Magliocco: this winemaker from the “Daniel What's new. 53 Magliocco & fils” winery in Chamoson is proud of his ultra- local approach to winemaking, using organic methods. Some Key events. of his wines have also60 been certified with the Valais brand How to getlabel since 2020. Or meet Margarethto Voide, a mountaineer Valais. 62 from Saas-Fee who has achieved the remarkable feat of Picture library. climbing all 82 peaks62 above 4,000 metres in the Alps. On the innovation side, we would like to introduce you to Jérôme Jacquod, a hydrogeologist who exports his expertise relating to dams throughout the world.