THE NORDEND of MONTE ROSA. T. Graham Brown
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Dufourspitze 4634M £1699
Icicle Mountaineering Ltd | 11a Church Street Windermere | Lake District | LA23 1AQ | UK Tel +44 (0)1539 44 22 17 | [email protected] Website: www.icicle-mountaineering.ltd.uk Online: shop.icicle-mountaineering.ltd.uk 2020 trip dossier | Dufourspitze 4634m £1699 Website link | http://www.icicle-mountaineering.ltd.uk/dufourspitze.html Key features Climb Dufourspitze, the highest mountain in Switzerland and second highest in the Alps.. 5 days guiding (Monday - Friday), with flexible itinerary to take advantage of the best conditions. Previous crampon or climbing experience is required, as this is a progression from an Intro course. Led by top qualified guides (IFMGA), guiding ratio 1:2 throughout the course. All technical equipment (e.g. B3 boots, crampons, ice axe etc.) can be hired from Icicle 2020 dates; 5 - 11 Jul, 19 - 25 Jul, 26 Jul - 1 Aug, 9 - 15 Aug, 30 Aug -+- 5 Sep. Icicle® is the registered trademark of Icicle Mountaineering UK registered company 413 6635. VAT 770 137 933 20 years ‘inspirational mountain adventure holidays’ established in 2000 Icicle Mountaineering Ltd | 11a Church Street Windermere | Lake District | LA23 1AQ | UK Tel +44 (0)1539 44 22 17 | [email protected] Website: www.icicle-mountaineering.ltd.uk Online: shop.icicle-mountaineering.ltd.uk Course overview . Climb the highest summit of Monte Rosa; Dufourspitze 4634m. It's the highest mountain in Switzerland, and the second highest in all of the Alps after Mont Blanc. We offer a week long programme to attempt this peak, as your acclimatisation and flexibility for selecting a weather window are crucial. To keep the itinerary flexibilty, the guiding ratio is 1:2 throughout, so you can take advantage of the best days for the summit weather window. -
Moüjmtaiim Operations
L f\f¿ áfó b^i,. ‘<& t¿ ytn) ¿L0d àw 1 /1 ^ / / /This publication contains copyright material. *FM 90-6 FieW Manual HEADQUARTERS No We DEPARTMENT OF THE ARMY Washington, DC, 30 June 1980 MOÜJMTAIIM OPERATIONS PREFACE he purpose of this rUanual is to describe how US Army forces fight in mountain regions. Conditions will be encountered in mountains that have a significant effect on. military operations. Mountain operations require, among other things^ special equipment, special training and acclimatization, and a high decree of self-discipline if operations are to succeed. Mountains of military significance are generally characterized by rugged compartmented terrain witn\steep slopes and few natural or manmade lines of communication. Weather in these mountains is seasonal and reaches across the entireSspectrum from extreme cold, with ice and snow in most regions during me winter, to extreme heat in some regions during the summer. AlthoughNthese extremes of weather are important planning considerations, the variability of weather over a short period of time—and from locality to locahty within the confines of a small area—also significantly influences tactical operations. Historically, the focal point of mountain operations has been the battle to control the heights. Changes in weaponry and equipment have not altered this fact. In all but the most extreme conditions of terrain and weather, infantry, with its light equipment and mobility, remains the basic maneuver force in the mountains. With proper equipment and training, it is ideally suited for fighting the close-in battfe commonly associated with mountain warfare. Mechanized infantry can\also enter the mountain battle, but it must be prepared to dismount and conduct operations on foot. -
Switzerland. Design &
SWITZERLAND. DESIGN & LIFESTYLE HOTELS Design & Lifestyle Hotels 2021. Design & Lifestyle Hotels at a glance. Switzerland is a small country with great variety; its Design & Lifestyle Hotels are just as diverse. This map shows their locations at a glance. A Aargau D Schaffhausen B B o d Basel Region e n s Rhein Thur e 1 2 e C 3 Töss Frauenfeld Bern 29 Limm B at Baden D Fribourg Region Liestal 39 irs B Aarau 40 41 42 43 44 45 Herisau Delémont 46 E Geneva A F Appenzell in Re e h u R H ss 38 Z ü Säntis r F Lake Geneva Region i 2502 s Solothurn c ub h - s e o e D e L Zug Z 2306 u g Churfirsten Aare e Vaduz G r W Graubünden 28 s a e La Chaux- e lense 1607 e L i de-Fonds Chasseral e n e s 1899 t r 24 25 1798 h le ie Weggis Grosser Mythen H Jura & Three-Lakes B 26 27 Rigi Glarus Vierwald- Glärnisch 1408 Schwyz Bad Ragaz 2119 2914 Neuchâtel re Napf stättersee Pizol Aa Pilatus Stoos Braunwald 2844 l 4 I Lucerne-Lake Lucerne Region te Stans La 5 nd châ qu u C Sarnen 1898 Altdorf Linthal art Ne Stanserhorn R Chur 2834 de e Flims J ac u 16 Weissfluh Piz Buin Eastern Switzerland / L 2350 s Davos 3312 18 E Engelberg s mm Brienzer Tödi e Rothorn 14 15 Scuol Liechtenstein e 12 y Titlis 3614 17 Arosa ro Fribourg 7 Thun 3238 Inn Yverdon B Brienz a D 8 Disentis/ Lenzerheide- L r s. -
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 -
The New Monte Rosa Hut
Beautifully efficient: the New Monte Rosa Hut The Swiss Federal Institute of Technology Zurich (ETH Zurich) and the Swiss Alpine Club (SAC) are intending to set a new milestone in Alpine building with the New Monte Rosa Hut. The foundation stone was laid in August 2008. The mountain hut is one of many projects initiated to mark the 150th anniversary of the ETH Zurich. It is an ambitious building project for a forward-looking SAC hut on 2883 metres above sea level, sustainable in terms of energy and ecology. The SAC was quick to agree to the project. The internationally known Monte Rosa area in the Swiss Canton of Valais, framed by the Matterhorn and the Dufourspitze, was chosen for the planned hut. The existing hut there is in need of refurbishment, and so the project partners decided to replace it with the New Monte Rosa Hut. In the winter term 2003/2004, the Studio Monte Rosa at the ETH Zurich’s architecture and construction department was set up. Working over four terms, a total of over thirty students devised a design for the New Monte Rosa Hut. The student’s ideas developed into a feasible project with the support of professors and experts from various disciplines. So now a five-storey timber construction is to be built on stainless steel foundations thrusting down into the rock. Its metallically shimmering aluminium outer covering and unusual polygonal shape make it look like a rock crystal. The guest rooms can accommodate a total of 120 people, and the enchanting surroundings are effectively invited in as well, by a cascade of steps and a wide window facade. -
A Combination of PROBA-V/MODIS-Based Products with Sentinel-1 SAR Data for Detecting Wet and Dry Snow Cover in Mountainous Areas
remote sensing Article A Combination of PROBA-V/MODIS-Based Products with Sentinel-1 SAR Data for Detecting Wet and Dry Snow Cover in Mountainous Areas Ya-Lun S. Tsai 1,* , Andreas Dietz 1, Natascha Oppelt 2 and Claudia Kuenzer 1 1 German Remote Sensing Data Center (DFD), German Aerospace Center (DLR), Muenchener Strasse 20, D-82234 Wessling, Germany 2 Department of Geography, Earth Observation and Modelling, Kiel University, Ludewig-Meyn-Str. 14, 24118 Kiel, Germany * Correspondence: [email protected] Received: 24 June 2019; Accepted: 13 August 2019; Published: 14 August 2019 Abstract: In the present study, we explore the value of employing both vegetation indexes as well as land surface temperature derived from Project for On-Board Autonomy—Vegetation (PROBA-V) and Moderate Resolution Imaging Spectroradiometer (MODIS) sensors, respectively, to support the detection of total (wet + dry) snow cover extent (SCE) based on a simple tuning machine learning approach and provide reliability maps for further analysis. We utilize Sentinel-1-based synthetic aperture radar (SAR) observations, including backscatter coefficient, interferometric coherence, and polarimetric parameters, and four topographical factors as well as vegetation and temperature information to detect the total SCE with a land cover-dependent random forest-based approach. Our results show that the overall accuracy and F-measure are over 90% with an ’Area Under the receiver operating characteristic Curve (ROC)’ (AUC) score of approximately 80% over five study areas located in different mountain ranges, continents, and hemispheres. These accuracies are also confirmed by a comprehensive validation approach with different data sources, attesting the robustness and global transferability. -
Recent Debris Flow Occurrences Associated with Glaciers in the Alps ⁎ Marta Chiarle A, , Sara Iannotti A, Giovanni Mortara A, Philip Deline B
Global and Planetary Change 56 (2007) 123–136 www.elsevier.com/locate/gloplacha Recent debris flow occurrences associated with glaciers in the Alps ⁎ Marta Chiarle a, , Sara Iannotti a, Giovanni Mortara a, Philip Deline b a CNR‐IRPI, Strada delle Cacce, 73–10135 Torino, Italy b Laboratoire EDYTEM, CNRS‐Université de Savoie, 73376 Le Bouget‐du‐Lac, France Received 12 August 2005; accepted 21 July 2006 Available online 9 January 2007 Abstract Debris flows from glacier forefields, triggered by heavy rain or glacial outbursts, or damming of streams by ice avalanches, pose hazards in Alpine valleys (e.g. the south side of Mount Blanc). Glacier‐related debris flows are, in part, a consequence of general glacier retreat and the corresponding exposure of large quantities of unconsolidated, unvegetated, and sometimes ice‐cored glacial sediments. This paper documents glacier‐related debris flows at 17 sites in the Italian, French, and Swiss Alps, with a focus on the Italian northwest sector. For each case data are provided which describe the glacier and the instability. Three types of events have been recognized, based on antecedent meteorological conditions. Type 1 (9 documented debris flows) is triggered by intense and prolonged rainfall, causing water saturation of sediments and consequent failure of large sediment volumes (up to 800000 m3). Type 2 (2 debris flows) is triggered by short rainstorms which may destabilize the glacier drainage system, with debris flow volumes up to 100000 m3. Type 3 (6 debris flows) occurs during dry weather by glacial lake outbursts or ground/buried ice melting, with debris flow volumes up to 150000 m3. -
Brochure on How to Act in Alpine Terrain
FORS MONTENEGRO FORSMONTENEGRO Foundation for the Development Fondacija za razvoj sjevera of Northern Montenegro Crne Gore Foundation for the Development of Northern Montenegro The project is funded by the European Union DIRECT BROCHURE ON HOW TO ACT IN ALPINE TERRAIN From a geographical standpoint, mountains are natural THE MOUNTAINS OF MONTENEGRO We hope that this brochure will be useful, that it will elevations of the earth’s surface attaining an altitude contribute to greater safety during stay in Montenegrin greater than 500 m. Mountains are formed and shaped by mountains, and that the tourists-hikers who visit our tectonic processes that could be classified as endogenic Montenegro is a South European and a Mediterranean mountains will carry away with them a most pleasant or internal (seismic an volcanic activity) or exogenic or country, mountainous and coastal at the same time, impression of their wild and breathtaking beauty. external (fluvial erosion – wearing away of soil by moving unique for its beauty, and one of the richest countries water, denudation – wearing down and stripping of the in Europe in terms of natural resources. e mountains rocks due to temperature swings, atmospheric influences, of Montenegro belong to the Dinaric Mountain Range. and expansion of plant roots, erosion – mechanical e prominent massifs are Orjen, Lovćen and Rumija disintegration of rocks, etc.). in the south, and Maglić, Durmitor, Vojnik, Morača Mountains, Komovi, Prokletije in the continental region, The tallest mountain ranges in the world are: The with an average elevation of the mountain peaks of over Himalayas with the highest peak in the world Mount 2,000 above sea level. -
ALPINE NOTES. Date of the ALPINE CLUB OBITUARY: Election
Alpine Notes . 381 The Triglav 'N. Face' is between 700 and 800 rrL high in t hat portion traversed by the ' Jug' route, and for the first three parts of the route it is almost sheer. Great smooth slabs, occurring in successive series, constitute the special and characteristic difficulty. The climb occupied 16 hours in all. F . S. C. ALPINE NOTES. Date of THE ALPINE CLUB OBITUARY: Election Allport, D . W. • • • • • • • 1875 Colgrove, J. B . • • • • • • • 1876 Morse, Sir George H. • • • • • • 1887 Holmes, .Alfred • • • • • • • 1894 Shea, C. E .. • • • • • • • 1896 Nicholson, L. D . • • • • • • 1902 Candler, H. • • • • • • • 1905 Collin, T. • • • • • • • • 1907 Schofield, J . W. • • • • • • 1907 Drake, Canon F. W. • • • • • • 1908 Kidd, Canon J. H . • • • • • • 1921 Morshead, Lt.-Col. H. T. • • • • • 1922 Painter, A. R. • • • • • • • 1923 Wright, W. A. • • • • • • • 1925 Peto, R . H . K . • • • • • • • 1929 THE CLOSING OF THE ITALIAN ALPS. If a little easier in fre _quented districts during t he height of summer, there are no real signs of improvement in the general situation, which continues to be unsatisfactory. During the C.A.I. Congress at Botzen, the President announced that 18 passes, hitherto closed, would be open between t he Stelvio and Pontebba in 1932. The S.A.C. and letters of t he REv. W. A. B. CooLIDGE. The Librarian of the S.A.C. Central Library, Zurich, requests us to announce that, ' together with the Alpine portion of Mr. Coolidge's library, the S.A.C. has collected during the course of the year, in their library at Zurich, many letters belonging to that distinguished mountaineer. It is true that Mr. -
Alpine Adventures 2019 68
RYDER WALKER THE GLOBAL TREKKING SPECIALISTS ALPINE ADVENTURES 2019 68 50 RYDER WALKER ALPINE ADVENTURES CONTENTS 70 Be the first to know. Scan this code, or text HIKING to 22828 and receive our e-newsletter. We’ll send you special offers, new trip info, RW happenings and more. 2 RYDERWALKER.COM | 888.586.8365 CONTENTS 4 Celebrating 35 years of Outdoor Adventure 5 Meet Our Team 6 Change and the Elephant in the Room 8 Why Hiking is Important – Watching Nature 10 Choosing the Right Trip for You 11 RW Guide to Selecting Your Next Adventure 12 Inspired Cuisine 13 First Class Accommodations 14 Taking a Closer Look at Huts 15 Five Reasons Why You Should Book a Guided Trek 16 Self-Guided Travel 17 Guided Travel & Private Guided Travel EASY TO MODERATE HIKING 18 Highlights of Switzerland: Engadine, Lago Maggiore, Zermatt 20 England: The Cotswolds 22 Isola di Capri: The Jewel of Southern Italy NEW 24 French Alps, Tarentaise Mountains: Bourg Saint Maurice, Sainte Foy, Val d’Isère 26 Sedona, Arches & Canyonlands 28 Croatia: The Dalmatian Coast 28 30 Engadine Trek 32 Scotland: Rob Roy Way 34 Montenegro: From the Durmitor Mountain Range to the Bay of Kotor 36 New Mexico: Land of Enchantment, Santa Fe to Taos NEW 38 Slovakia: Discover the Remote High Tatras Mountains NEW MODERATE TO CHALLENGING HIKING 40 Heart of Austria 42 Italian Dolomites Trek 44 High Peaks of the Bavarian Tyrol NEW 46 Sicily: The Aeolian Islands 48 Rocky Mountain High Life: Aspen to Telluride 50 New Brunswick, Canada: Bay of Fundy 52 Via Ladinia: Italian Dolomites 54 Dolomiti di -
Articles, Only Recently
Nat. Hazards Earth Syst. Sci., 16, 2085–2106, 2016 www.nat-hazards-earth-syst-sci.net/16/2085/2016/ doi:10.5194/nhess-16-2085-2016 © Author(s) 2016. CC Attribution 3.0 License. Climate anomalies associated with the occurrence of rockfalls at high-elevation in the Italian Alps Roberta Paranunzio1, Francesco Laio1, Marta Chiarle2, Guido Nigrelli2, and Fausto Guzzetti3 1Department of Environment, Land and Infrastructure Engineering, Politecnico di Torino, Torino, Italy 2Research Institute for Geo-hydrological Protection, National Research Council (CNR IRPI), Torino, Italy 3Research Institute for Geo-hydrological Protection, National Research Council (CNR IRPI), Perugia, Italy Correspondence to: Roberta Paranunzio ([email protected]) Received: 29 March 2016 – Published in Nat. Hazards Earth Syst. Sci. Discuss.: 4 April 2016 Revised: 13 July 2016 – Accepted: 22 August 2016 – Published: 12 September 2016 Abstract. Climate change is seriously affecting the 1 Introduction cryosphere in terms, for example, of permafrost thaw, al- teration of rain=snow ratio, and glacier shrinkage. There is concern about the increasing number of rockfalls at high el- The recent decades have seen a pronounced warming in evation in the last decades. Nevertheless, the exact role of global climate, primarily at high elevations and high latitudes climate parameters in slope instability at high elevation has (Schär et al., 2004). Temperature across European Alps has ◦ not been fully explored yet. In this paper, we investigate 41 increased of about 1.4 K per century over the period 1906– rockfalls listed in different sources (newspapers, technical re- 2005, which is more than double the global average (Brunetti ports, and CNR IRPI archive) in the elevation range 1500– et al., 2009) and further increases are expected according to 4200 m a.s.l. -
Tourenverzeichnis 1943
Tourenverzeichnis 1943 Objekttyp: Group Zeitschrift: Jahresbericht / Akademischer Alpen-Club Zürich Band (Jahr): 48 (1943) PDF erstellt am: 25.09.2021 Nutzungsbedingungen Die ETH-Bibliothek ist Anbieterin der digitalisierten Zeitschriften. Sie besitzt keine Urheberrechte an den Inhalten der Zeitschriften. Die Rechte liegen in der Regel bei den Herausgebern. Die auf der Plattform e-periodica veröffentlichten Dokumente stehen für nicht-kommerzielle Zwecke in Lehre und Forschung sowie für die private Nutzung frei zur Verfügung. Einzelne Dateien oder Ausdrucke aus diesem Angebot können zusammen mit diesen Nutzungsbedingungen und den korrekten Herkunftsbezeichnungen weitergegeben werden. Das Veröffentlichen von Bildern in Print- und Online-Publikationen ist nur mit vorheriger Genehmigung der Rechteinhaber erlaubt. Die systematische Speicherung von Teilen des elektronischen Angebots auf anderen Servern bedarf ebenfalls des schriftlichen Einverständnisses der Rechteinhaber. Haftungsausschluss Alle Angaben erfolgen ohne Gewähr für Vollständigkeit oder Richtigkeit. Es wird keine Haftung übernommen für Schäden durch die Verwendung von Informationen aus diesem Online-Angebot oder durch das Fehlen von Informationen. Dies gilt auch für Inhalte Dritter, die über dieses Angebot zugänglich sind. Ein Dienst der ETH-Bibliothek ETH Zürich, Rämistrasse 101, 8092 Zürich, Schweiz, www.library.ethz.ch http://www.e-periodica.ch — 32 — TourenVerzeichnis 1943 Abkürzungen: (V) Versuch, (a) allein Im 1. Abschnitt sind jeweils die Skitouren aufgeführt. A. Berichte