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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. -
Cycling Group Media Trip
Cycling Group Media Trip Destinations: Martigny Region and Alpes vaudoises Dates: from Wednesday 26 to Sunday 30 August 2020 (4 nights, 5 days) Participants: max. 8 international journalists Highlights: Itineraries of the 2020 UCI Road World Championships, “Routes of the Road World Championships” bookable offer, itinerary of the UCI Gran Fondo Switzerland Villars Fitness level: out of 3 stars Tech. level: out of 3 stars www.visitvalais.ch/cycling 1 VALAIS/WALLIS PROMOTION Conditions for taking part in this press trip - You must be in very good physical shape and have the stamina to keep going for several hours a day over several days. - You must have experience in road cycling and ride regularly. - Let us know if you are bringing your own bicycle. - If not, let us know if you ride with flat pedals or with clips. You must bring your own cycling shoes and pedals (these will be adjusted to fit your bicycle). - You must bring your own cycling helmet. Key: Fitness level: I do sports at least twice a month I do sports once or twice a week I do sports three or more times a week Technical level: I have never or hardly ever done this activity I do this activity occasionally I do this activity regularly 2 VALAIS/WALLIS PROMOTION Transport within Switzerland For your comfortable journey through Switzerland, Swiss Travel System (STS) is happy to provide you with a unique all-in-one 1st class Swiss Travel Pass. 4 advantages of your #swisstravelpass: - Unlimited travel by train, bus and boat - Public transportation in more than 90 cities and towns - Including mountain excursions: Rigi, Stanserhorn and Stoos - Free admission to more than 500 museums throughout Switzerland Two informative, free apps are available to you for travel by train, bus and boat. -
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. -
The Imeschs from the Upper Valais - Glimpses of a Swiss and North-American Family
Swiss American Historical Society Review Volume 42 Number 1 Article 3 2-2006 The Imeschs from the Upper Valais - Glimpses of a Swiss and North-American Family Marianne Burkhard Follow this and additional works at: https://scholarsarchive.byu.edu/sahs_review Part of the European History Commons, and the European Languages and Societies Commons Recommended Citation Burkhard, Marianne (2006) "The Imeschs from the Upper Valais - Glimpses of a Swiss and North- American Family," Swiss American Historical Society Review: Vol. 42 : No. 1 , Article 3. Available at: https://scholarsarchive.byu.edu/sahs_review/vol42/iss1/3 This Article is brought to you for free and open access by BYU ScholarsArchive. It has been accepted for inclusion in Swiss American Historical Society Review by an authorized editor of BYU ScholarsArchive. For more information, please contact [email protected], [email protected]. Burkhard: The Imeschs from the Upper Valais THE IMESCHS FROM THE UPPER V ALAIS - GLIMPSES OF A SWISS AND NORTH-AMERICAN FAMILY by Marianne Burkhard 1. Introduction The Valais is the third-largest canton of Switzerland covering 2016 square miles of which only 1107 are productive. It is also a world of its own: it received its name "the valley" from the 100 mile long valley of the Rhone River which has its source above the small town of Gletsch below the highest point of the Furka pass. This main valley is flanked on the north and south side by many of the highest peaks of the Swiss Alps. The northern side toward the Canton of Bern is forbiddingly steep, and the Lotschental and the valley leading to the Leukerbad are the only valleys which branch off on this side while many long and deep valleys branch off on the southern side, e.g. -
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. -
Voyage De Presse Groupe Vélo
Voyage de presse groupe vélo Destinations : Martigny région et les Alpes vaudoises Dates : Du mercredi 26 au dimanche 30 août 2020 (4 nuits, 5 jours) Participants : max. 8 journalistes internationaux Highlights : Des itinéraires des Championnats du Monde Route UCI 2020, l’offre réservable « Sur les traces des Championnats du Monde », l’itinéraire de l’UCI Gran Fondo Suisse Villars Niveau fitness : niveau 3/3 Niveau tech. : niveau 3/3 www.valais.ch/velo 1 VALAIS/WALLIS PROMOTION Conditions pour une participation à ce voyage de presse - Vous êtes en très bonne forme physique et êtes capable de fournir un effort de plusieurs heures sur plusieurs jours consécutifs. - Vous avez de l’expérience en vélo de route et pratiquez régulièrement ce sport. - Veuillez nous informer si vous emmenez votre propre vélo. - Si vous ne venez pas avec votre propre vélo, informez-nous si vous roulez en pédales plates ou à clips. Vous devez emporter vos propres chaussures de vélo et pédales (ces dernières seront ajustées à votre vélo de location). - Vous devez vous munir de votre propre casque de vélo. Légende : Niveau fitness : Je pratique du sport moins de deux fois par mois Je pratique du sport une ou deux fois par semaine Je pratique du sport trois fois et plus par semaine Niveau technique : Je n’ai jamais ou rarement pratiqué cette activité Je pratique de temps en temps cette activité Je pratique régulièrement cette activité 2 VALAIS/WALLIS PROMOTION Transports en Suisse Pour vous permettre de voyager confortablement dans toute la Suisse, Swiss Travel System (STS) a conçu pour vous un Swiss Travel Pass de 1re classe. -
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