SAMPLING the EASTERN ALPS. by Miriam E. Underhill
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Rosskopf Flyer
I.P. Prices Winter 2019/2020 Ascent facilities Cable car .....................................................6 pers. 2.756 m Main season Low season 22.12.2019 – 06.01.2020 06.12.2019 – 21.12.2019 Telemix “Panorama“ ............................6-8 pers. 885 m 02.02.2020 – 01.03.2020 07.01.2020 – 01.02.2020 Chairlift “Stock“ .........................................4 pers. 1.487 m 02.03.2020 – 29.03.2020 Adults Children Seniors Adults Children Seniors Ski slopes Single round trips easy medium hard Single ride 14 10 13 12 9 11 Ramingeralm ...........................................................3.000 m Winter 2 single rides 25 18 23 23 17 21 Sonne .........................................................................2.000 m Round trip 18 13 17 17 12 16 2019/2020 Training .....................................................................1.000 m Hourly tickets valid from first entry International I .........................................................1.600 m 3 h 38 27 34 35 24 32 International II ........................................................1.500 m 4 h 40 28 36 37 26 34 Slalom ........................................................................1.300 m Single tour ski mountaineering (incl. descent) Gringesboden .........................................................2.200 m 8,5 6 7,5 8,5 6 7,5 Favorit ........................................................................2.000 m Daily card for sled riders Favorit Variant ......................................2.700 m Beginners field ..............................................................70 -
Hiking and Climbing Your Personal Karwendel
Around the top station Hiking and climbing Your personal Karwendel experience Prices Summer 2017 A visit to the nature information centre is part of any ex- The top station of the Karwendel cable car is an ideal Whether it’s a family outing at the weekend or a moun- cursion in the Karwendel. The “giant telescope” projects starting point for tours into the Northern Karwendel tain hike with friends there are lots of possibilities. For Return Single spectacularly over the cliff edge towards Mittenwald with range. Alongside enjoyable walking paths for the whole that really special experience you can even get married, Adults € 27.50 € 17.50 a view of the breathtaking 1,300m drop over the wide family there are also challenging via ferrata for adrena- hold a conference or celebrate your birthday at 2,244m. Youths / Children € 17.50 € 12.50 Isar valley. Inside you can find out many interesting facts line junkies. about the Karwendel, the largest nature reserve of the Alongside regular public events of the Karwendelbahn AG Directly at the top station, the Passami path leads around Family discount for parents with their children Eastern Alps and the natural habitat for animals and fauna. such as our New Year’s or Easter brunch we can organise the Karwendel basin. This panoramic path is ideal to get your own personal festival. We would be glad to send you (6 to 17 years old) The nature information centre “Bergwelt Karwendel” is a breathtaking view of the impressive Karwendel in the a customised offer for your celebration, conference, group 2 adults + 2 adults + 2 adults + 2 adults + open during the regular operating times of the Karwendel shortest possible time. -
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 Supreme Discipline of Mountaineering
The Supreme Discipline of Mountaineering To what heaven would it lead me to climb a mountain that flew? Christoph Ransmayr, “The Flying Mountain” MMM Corones on Kronplatz – between the Gader Valley, Olang and the Puster Valley – is the final act in the Messner Mountain Museum project (which comprises a total of six facilities). On the edge of South Tyrol’s mountain plateau with the most spectacular views, in the unique museum architecture created by Zaha Hadid, I present the crowning of traditional mountaineering. Kronplatz offers views beyond the borders of South Tyrol to all points of the compass: from the Lienz Dolomites in the east to the Ortler in the west, from the Marmolada in the south to the Zillertal Alps in the north. The museum is a mirror of the world of my childhood - the Geislerspitzen, the central buttress of the Heiligkreuzkofel (the most difficult climb in my whole life) and the glaciated granite mountains of the Ahrn Valley. On Kronplatz I present the development of modern mountaineering and 250 years of progress with regard to the equipment. I speak of triumphs and tragedies on the world’s most famous peaks – the Matterhorn, Cerro Torre, K2 – and the depiction of our activity, however contradictory it may seem. As in my other museums, I shed light on alpinism with the help of relics, thoughts, works of art (pictures and sculptures) and by reflecting the outside mountain backcloth in the interior of MMM Corones. As the storyteller of traditional mountaineering, it is not my intention to judge or dramatise but simply to condense human experience of a world that is my world, of the 250-year-old contest between man and the mountain. -
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. -
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. -
Revisiting the Subalpine Mesolithic Site Ullafelsen in the Fotsch Valley, Stubai Alps
Research article E&G Quaternary Sci. J., 70, 171–186, 2021 https://doi.org/10.5194/egqsj-70-171-2021 © Author(s) 2021. This work is distributed under the Creative Commons Attribution 4.0 License. Revisiting the subalpine Mesolithic site Ullafelsen in the Fotsch Valley, Stubai Alps, Austria – new insights into pedogenesis and landscape evolution from leaf-wax-derived n-alkanes, black carbon and radiocarbon dating Michael Zech1,2;, Marcel Lerch1,2;, Marcel Bliedtner3, Tobias Bromm2, Fabian Seemann1, Sönke Szidat4, Gary Salazar4, Roland Zech3, Bruno Glaser2, Jean Nicolas Haas5, Dieter Schäfer6, and Clemens Geitner7 1Heisenberg Chair of Physical Geography with Focus on Paleoenvironmental Research, Department of Geosciences, Technische Universität Dresden, Helmholtzstr. 10, 01096 Dresden, Germany 2Soil Biogeochemistry Group, Institute of Agronomy and Nutritional Sciences, Martin-Luther University Halle-Wittenberg, Von-Seckendorff-Platz 3, 06120, Halle (Saale), Germany 3Chair of Physical Geography, Institute of Geography, Friedrich Schiller University of Jena, Löbdergraben 32, 07743 Jena, Germany 4Department of Chemistry, Biochemistry and Pharmaceutical Sciences & Oeschger Centre for Climate Change Research, University of Bern, Freiestrasse 3, 3012 Bern, Switzerland 5Institute of Botany, University of Innsbruck, Sternwartestr. 15, 6020 Innsbruck, Austria 6Institute of Archaeology, University of Innsbruck, Langer Weg 11/3, 6020 Innsbruck, Austria 7Institute of Geography, University of Innsbruck, Innrain 52, 6020 Innsbruck, Austria These authors contributed equally to this work. Correspondence: Michael Zech ([email protected]) Relevant dates: Received: 11 January 2021 – Revised: 29 May 2021 – Accepted: 16 June 2021 – Published: 13 July 2021 How to cite: Zech, M., Lerch, M., Bliedtner, M., Bromm, T., Seemann, F., Szidat, S., Salazar, G., Zech, R., Glaser, | downloaded: 4.10.2021 B., Haas, J. -
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 -
Cretaceous Thrusting in the Western Part of the Northern Calcareous Alps (Austria) - Evidences from Synorogenic Sedimentation and Structural Data
ZOBODAT - www.zobodat.at Zoologisch-Botanische Datenbank/Zoological-Botanical Database Digitale Literatur/Digital Literature Zeitschrift/Journal: Austrian Journal of Earth Sciences Jahr/Year: 2001 Band/Volume: 94 Autor(en)/Author(s): Ortner Hugo Artikel/Article: Cretaceous thrusting in the western part of the Northern Calcareous Alps (Austria) - evidences from synorogenic sedimentation and structural data. 63-77 © Österreichische Geologische Gesellschaft/Austria; download unter www.geol-ges.at/ und www.biologiezentrum.at Mitt. Osterr. Geol. Ges. i ISSN 0251-7493 94(2001) 63-77 Wien, August 2003 Northern Calcareous Alps thrust sequence ramp-flat-model strain partitioning ^. .. _•_••.• . .,_* Vorarlberg, Tirol, Salzburg Cretaceous thrusting in the western part of the Northern Calcareous Alps (Austria) - evidences from synorogenic sedimentation and structural data HUGO ORTNER1 8 Figures Content Abstract 63 1. Introduction 63 1.1 Relationship between synorogenic sediments and thrusting 65 2. Nappe geometries and age of synorogenic sediments in the western Northern Calcareous Alps 67 2.1 The Lechtal and Allgäu nappes 67 2.2 The Inntal Nappe 69 2.2.1 Post Nappe-stacking movements 71 2.3 The Thiersee thrust 71 2.4 The Achental thrust 71 2.5 The Berchtesgaden nappe complex 73 3. Discussion 73 4. Conclusions 75 5. Acknowledgements 75 References 75 Abstract The application of a simple ramp-flat model to Cretaceous nappe stacking in the Northern Calcareous Alps and its relation to synorogenic sedimentation allows to assess the large scale geometry of the nappe stack. Different synorogenic formations are related to specific positions within the ramp-flat model: Gosau and Branderfleck Fms. are found on the hangingwall anticlines of the Inntal and Lechtal nappes, respectively, Losenstein and Tannheim Fms. -
Get on Your Bike!
Mountain bike and cycling tours Get on your Bike! www.alpenwelt-karwendel.de/enBiking in Alpenwelt Karwendel 1 Welcome to _________________________________________________ Welcome - Presenting Alpenwelt Karwendel Page 3 _________________________________________________ Adventure in the mountains - Mountain bike tours Page 4 _________________________________________________ Easy tour Enjoyment and family - Trekking bike tours Page 18 _________________________________________________ Explore the region - Racing bike tours Page 26 _________________________________________________ Medium tour Cycling with a tail wind - E-bike tours Page 30 _________________________________________________ Better orientation - Alpenwelt overview Page 32 _________________________________________________ Difficult tour Good to know - Information for cyclists Page 34 _________________________________________________ Each of these tours can be started from all three municipalities in Alpenwelt Karwendel. Welcome to Alpenwelt Karwendel! These two mountain bikers have had a good laugh. They are returning from a break at Vereiner Alm. In the deep south of Germany, at the border with Austria, a pleasant valley with undula- ting meadows, lakes and streams extends between rocky peaks, forested mountain flanks and hills. Alpenwelt Karwendel with the three Upper Bavarian municipalities of Mittenwald, Krün and Wallgau is surrounded by four mountain massifs: the Karwendel mountains and the Soiern group to the East, the Ester mountains to the North and the Wetterstein mountains to the South-West. Because of this, the region is the ideal starting point for all kinds of mountain bike and cycling tours. If you like to take it easy, you can linger in the valley between the flower meadows, lakes and the expansive river landscape of the Isar with its shingle and gravel banks. If you prefer the forested foothills, explore the Ester mountains and the Soiern group with their shady forest roads and single trails. -
Humid Climate During Deposition of Sapropel 1 in the Mediterranean Sea: Assessing the Influence on the Alps
Global and Planetary Change 71 (2010) 242–248 Contents lists available at ScienceDirect Global and Planetary Change journal homepage: www.elsevier.com/locate/gloplacha Humid climate during deposition of sapropel 1 in the Mediterranean Sea: Assessing the influence on the Alps Christoph Spötl a,⁎, Kurt Nicolussi b, Gernot Patzelt c, Ronny Boch a and Daphne team 1 a Institut für Geologie und Paläontologie, Universität Innsbruck, Innrain 52, 6020 Innsbruck, Austria b Institut für Geographie, Universität Innsbruck, Innrain 52, 6020 Innsbruck, Austria c Patscher Straße 20, 6080 Innsbruck-Igls, Austria article info abstract Article history: Cave and lake isotope records from the circum-Mediterranean realm show anomalously low O isotope values Received 23 January 2009 suggesting high rainfall intensity during the time of sapropel 1 deposition (9.5 to 6.5 ka; all ages are given Accepted 2 October 2009 before the year AD 2000, i.e. b2k), coincident with an interval of conspicuously low sea-surface salinities in Available online 22 October 2009 the entire Mediterranean Sea. Speleothem data from Corchia Cave (Tuscany) currently provide the most precise terrestrial chronology and constrain the wettest interval to ca. 8.2 to 7.3 ka. We have traced this Keywords: Holocene isotopic signal to the north and observe a synchronous isotopic change in stalagmites from southalpine and Alps eastalpine caves, but in opposite direction. We attribute this to a shift in the local moisture balance, i.e. to a palaeoclimate higher proportion of moisture advected from the Mediterranean Sea relative to the otherwise dominant stable isotopes northwesterly air masses in the Alps.