2016 Online Catalogue
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Welttag Der Berge“ Am 11
Insta-Ranking zum „Welttag der Berge“ am 11. Dezember: Die beliebtesten Naturkolosse in Österreich und der Schweiz Rang Berg Instagram-Beiträge Höhe in Metern Staat(en) Gebirgsgruppe 1 Matterhorn 764.340 4478 Schweiz Italien Walliser Alpen 2 Monte Rosa: Grenzgipfel 206.977 4618 Schweiz Italien Walliser Alpen 3 Titlis 122.853 3238 Schweiz Urner Alpen 4 Großglockner 115.920 3798 Österreich Glocknergruppe 5 Kitzsteinhorn 112.705 3203 Österreich Glocknergruppe 6 Dents du Midi 34.577 3257 Schweiz Chablais-Alpen 7 Piz Buin 24.573 3312 Österreich Schweiz Silvretta 8 Breithorn 17.726 4164 Schweiz Italien Walliser Alpen 9 Weisshorn 16.090 4505 Schweiz Walliser Alpen 10 Wetterhorn 11.551 3692 Schweiz Berner Alpen 11 Mittagskogel 9.077 3162 Österreich Ötztaler Alpen 12 Wildspitze 8.396 3768 Österreich Ötztaler Alpen 13 Bouquetins 8.361 3838 Schweiz Italien Walliser Alpen 14 Piz Nair 7.722 3059 Schweiz Glarner Alpen 15 Piz Bernina 7.389 4049 Schweiz Bernina-Alpen 16 Piz Palü 7.176 3882 Schweiz Bernina-Alpen 17 Großvenediger 7.006 3657 Österreich Venedigergruppe 18 Klein Matterhorn 6.628 3883 Schweiz Walliser Alpen 19 Schreckhorn 5.503 4078 Schweiz Berner Alpen 20 Kranzberg 5.187 3742 Schweiz Berner Alpen 21 Bietschhorn 5.057 3934 Schweiz Berner Alpen 22 Allalinhorn 4.811 4027 Schweiz Walliser Alpen 23 Olperer 4.567 3476 Österreich Zillertaler Alpen 24 Schwarzhorn 4.556 3620 Schweiz Walliser Alpen 25 Schwarzhorn 4.556 3201 Schweiz Walliser Alpen 26 Schwarzhorn 4.556 3146 Schweiz Albula-Alpen 27 Schwarzhorn 4.556 3105 Schweiz Berner Alpen 28 Dufourspitze -
Matterhorn Guided Ascent Ex Zermatt 2021
MATTERHORN 4,478M / 14,691FT EX ZERMATT 2021 TRIP NOTES MATTERHON EX ZERMATT TRIP NOTES 2021 TRIP DETAILS Dates: Available on demand July to September Duration: 6 days Departure: ex Zermatt, Switzerland Price: €5,870 per person A classic ‘must-do’ European climb. Photo: Mike Roberts The Matterhorn is undeniably the most magnificent and well-known peak in the Alps. Its bold pyramidal shape evokes emotions of wonderment and even fear in those who view it for the first time, as its four distinct faces stand omnipotent and menacing over the green meadows below. Separated by sharp ridges, the four faces are orientated to the four points of the compass, the northern aspects within Switzerland while the southern side lies in Italy. We ascend via the Hörnli Ridge that separates the rich heritage adds to the superb facilities, including North and East Faces via a long and technical route catered huts and lift systems offering services not requiring the utmost attention from climbers. The seen elsewhere. steep rock ridge is very involving and a successful attempt requires a rapid rate of ascent and full The Hörnli Ridge is the route by which the concentration by a fit party. The steep North and Matterhorn’s first ascent was made in 1865 by the East Faces drop away spectacularly on either side tenacious Englishman, Edward Whymper, after and the sense of exposure is dramatic. many attempts on the mountain. In what became the most famous alpine calamity of all time, the With its formidable history and the magnificent group suffered a terrible tragedy on the descent grandeur of its architecture, the Hörnli Ridge on when a rope broke resulting in the loss of four of the Matterhorn is a climb that is definitely worth the party. -
IFP 1707 Dent Blanche – Matterhorn – Monte Rosa
Inventaire fédéral des paysages, sites et monuments naturels d'importance nationale IFP IFP 1707 Dent Blanche – Matterhorn – Monte Rosa Canton Communes Surface Valais Evolène, Zermatt 26 951 ha Le Gornergletscher et le Grenzgletscher IFP 1707 Dent Blanche – Matterhorn – Monte Rosa Stellisee Hameau de Zmutt Dent Blanche avec glacier de Ferpècle 1 IFP 1707 Dent Blanche – Matterhorn – Monte Rosa 1 Justification de l’importance nationale 1.1 Région de haute montagne au caractère naturel et sauvage, avec nombreux sommets de plus de 4000 m d’altitude 1.2 Mont Rose, massif alpin avec le plus haut sommet de Suisse 1.3 Mont Cervin, montagne emblématique à forme pyramidale 1.4 Plusieurs glaciers de grande étendue avec marges proglaciaires intactes, en particulier le Gornergletscher, l’un des plus grands systèmes glaciaires de Suisse 1.5 Marmites glaciaires, roches polies et stries glaciaires, structures représentatives des diverses formes glaciaires 1.6 Situation tectonique unique dans les Alpes suisses, superposant des unités tectoniques et des roches de provenances paléogéographiques très variées 1.7 Vastes forêts naturelles de mélèzes et d’aroles 1.8 Phénomènes glaciaires et stades morainiques remarquables et diversifiés 1.9 Zones riches en cours d’eau et lacs d’altitude 1.10 Grande richesse floristique et faunistique, comprenant de nombreuses espèces rares et endémiques 1.11 Zmutt, hameau avec des bâtiments traditionnels bien conservés 2 Description 2.1 Caractère du paysage Le site Dent Blanche-Matterhorn-Monte Rosa est une zone de haute montagne encadrée de massifs montagneux imposants dans la partie méridionale du Valais et à la frontière avec l’Italie. -
“Darkening Swiss Glacier Ice?” by Kathrin Naegeli Et Al
The Cryosphere Discuss., https://doi.org/10.5194/tc-2018-18-AC2, 2018 TCD © Author(s) 2018. This work is distributed under the Creative Commons Attribution 4.0 License. Interactive comment Interactive comment on “Darkening Swiss glacier ice?” by Kathrin Naegeli et al. Kathrin Naegeli et al. [email protected] Received and published: 17 April 2018 ——————————————————————————— We would like to thank the referee 2 for this careful and detailed review. We appreciate the in-depth comments and are convinced that thanks to the respective changes, the manuscript will improve substantially. In response to this review, we elaborated the role of supraglacial debris in more detail by: (1) manually delineating medial moraines and areas where tributaries separated from the main glacier trunk and debris has become exposed to obtain a complete Printer-friendly version supraglacial debris mask based on the Sentinel-2 image acquired in August 2016, and (2) applying this debris mask to all data and, thus, to exclude areas with debris cover- Discussion paper age from all consecutive analyses. Additionally, we further developed the uncertainty assessment of the retrieved albedo values by providing more information about the C1 datasets used as well as their specific constraints and uncertainties that may result thereof in a separate sub-section in the methods section. Based on these revisions, TCD the conclusions will most likely be slightly adjusted, however, stay in line with the orig- inal aim of our study to investigate possible changes in bare-ice albedo in the Swiss Alps based on readily available Landsat surface reflectance data. Interactive comment Below we respond to all comments by anonymous referee 2. -
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 -
Trip Factsheet: Monte Rosa Climber Zermatt Zermatt Is a Charming
Trip Factsheet: Monte Rosa Climber Zermatt Zermatt is a charming alpine village. It is car-free and reached only by a 15 minute train journey from the valley station of Tasch. As you would expect given its location it is one of Europe's main centres of Alpinism and is a bustling town in both winter and summer. The town is at 1,650m/5,420ft. Zermatt is in the German-speaking section of Switzerland. English (and French) are widely spoken. For further details on Zermatt click on the Zermatt Tourism website at www.zermatt.ch/en/ Monte Rosa (4,634m/15,203ft) Monte Rosa is the second highest mountain in the Alps and the highest mountain in Switzerland. The Monte Rosa is known in German as the Dufourspitze. It is in the Monte Rosa massif which is a range that lies on the border between Switzerland and Italy and is made up of several summits over 4500m, including Nordend, Zumsteinspitze, Signalkuppe and Ludwigshohe. Monte Rosa is located in the Pennine Alps (at 45°56′12.6″N, 7°52′01.4″E), 12kms east of Zermatt. It was first climbed in 1855. We usually ascend Monte Rosa over a 3 day period via the West ridge - the route is graded AD. The ascent begins from the Monte Rosa Hut which is accessed via the Gornergrat railway and a 2 hour trek. Summit day is a long, steady climb with 1800m of ascent to the highest point, called the Dufourspitze. There is a short grade 3 rock section and ice-slopes up to 40 degrees. -
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. -
Lithostratigraphy and U-Pb Zircon Dating in the Overturned Limb of the Siviez-Mischabel Nappe: a New Key for Middle Penninic Nappe Geometry
1661-8726/08/020431-22 Swiss J. Geosci. 101 (2008) 431–452 DOI 10.1007/s00015-008-1261-5 Birkhäuser Verlag, Basel, 2008 Lithostratigraphy and U-Pb zircon dating in the overturned limb of the Siviez-Mischabel nappe: a new key for Middle Penninic nappe geometry FLORIAN GENIER1, JEAN-LUC EPARD 1, FRANÇOIS BUSSY 2 & TOMAS MAGNA2 Key words: alps, Middle Penninic, Siviez-Mischabel nappe, Permo-Carboniferous, Randa orthogneiss, zircon typology, U-Pb geochronology ABSTRACT Detailed field work and zircon analysis have improved the knowledge of the This coherent overturned sequence can be observed from the St-Niklaus area to lithostratigraphy at the base of the Siviez-Mischabel nappe in the Mattertal the Moosalp pass to the north. Detailed mapping revealed that the St-Niklaus (St-Niklaus-Törbel area). They confirm the existence of an overturned limb syncline is symmetrical and connects the overturned limb of the Siviez-Mischa- and clarify the structure of the St-Niklaus syncline. The following formations bel nappe to the normal series of the Upper Stalden zone. U-Pb zircon geo- can be observed: chronology on magmatic and detrital zircons allowed constraining ages of these formations. Detrital zircons display ages ranging from 2900 ± 50 to 520 ± 4 Ma • Polymetamorphic gneisses; composed of paragneisses, amphibolites and in the Törbel Formation, and from 514 ± 6 to 292 ± 9 Ma in the Moosalp Forma- micaschists (Bielen Unit, pre-Ordovician). tion. In addition, the Permian Randa orthogneiss is intrusive into the polymeta- • Fine-grained, greyish quartzite and graywacke with kerogen-rich hori- morphic gneisses and into the Permo-Carboniferous metasediments of the zons (Törbel Formation, presumed Carboniferous). -
In Memoriam 115
IN MEMORIAM 115 • IN MEMORIAM CLAUDE WILSON 1860-1937 THE death of Claude Wilson within a few weeks of attaining his seventy-seventh birthday came as a terrible shock to his many friends. Few of us even knew that he was ill, but in the manner of his passing none can regret that there was no lingering illness. We can but quote his own words in Lord Conway's obituary: 'the best we can wish for those that we love is that they may be spared prolonged and hopeless ill health.' His brain remained clear up to the last twenty-four hours and he suffered no pain. The end occurred on October 31. With Claude Wilson's death an epoch of mountaineering comes to an end. He was of those who made guideless and Alpine history from Montenvers in the early 'nineties, of whom but Collie, Kesteven, Bradby, ~olly and Charles Pasteur still survive. That school, in which Mummery and Morse were perhaps the most prominent examples, was not composed of specialists. Its members had learnt their craft under the best Valais and Oberland guides; they were equally-proficient on rocks or on snow. It mattered little who was acting as leader in the ascent or last man in the descent. They were prepared to turn back if conditions or weather proved unfavourable. They took chances as all mountaineers are forced to do at times but no fatal accidents, no unfortunate incidents, marred that great page of Alpine history, a page not confined to Mont Blanc alone but distributed throughout the Western Alps. -
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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. -
Název Prezentace
4. Tourist attractions in Central European. Countries Předmět: The Tourist Attractions in the Czech Republic and in the World Geography of Switzerland The beautiful, mountainous country of Switzerland is landlocked in south-central Europe, and remains one of the most popular travel destinations on the planet. Mountains cover 60% of Switzerland's land area, with ranges of the Alps in the south and the Jura Mountains to the north. Switzerland's highest point is Dufourspitze (Monte Rosa), in the Pennine Alps, which rises to (4,634 m). Also located within the Pennine Alps is the infamous Matterhorn whose summit is (4,478 m) high. Moving north, the Rhine River makes up much of Switzerland's border with Germany, as well as part of Lake Constance. Switzerland's two largest lakes are Lake Geneva (shared with France) and Lake Neuchatel - which is the largest lake entirely within the country's borders. The main tourist attractions in Switzerland The Matterhorn, Switzerland's iconic pointed peak is one of the highest mountains in the Alps. On the border with Italy, this legendary peak rises to 4,478 meters, and its four steep faces lie in the direction of the compass points. The first summiting in 1865 ended tragically when four climbers fell to their death during the descent. Today, thousands of experienced climbers come here each summer. One of the most popular experiences in the beautiful Bernese Oberland is the train journey to Jungfraujoch, the "Top of Europe," with an observation terrace and scientific observatory perched at 3,454 meters. The longest glacier in Europe, the Great Aletsch Glacier begins at Jungfraujoch, and is a UNESCO World Heritage Site.