Archaeology of the Schnidejoch
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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 -
Alpes Bernoises, De L'archéologie Sur Le Schnidejoch
Lenk Avez-vous découvert quelque chose dans la 0 1000m glace ou à sa proximité ? – Ne déplacez pas l’objet ou uniquement s’il est directe ment menacé. – Photographiez l’objet en détail ainsi que dans son contexte de découverte élargi. Département de la mobilité, du territoire et de l’environnement du canton du Valais – Marquez si possible l’emplacement de découverte. Service des bâtiments, monuments – Relevez les coordonnées de la découverte ou 3 et archéologie inscrivezla sur une carte. Departement für Mobilität, Raumentwicklung 2 – Les trouvailles appartiennent au canton dans lequel und Umwelt des Kantons Wallis Dienststelle für Hochbau, Denkmalpflege elles ont été découvertes. Annoncezles au plus vite und Archäologie au service cantonal compétent : Case postale, 1950 Sion Téléphone +41 27 606 38 00 Archäologischer Dienst des Kantons Bern Brünnenstrasse 66 [email protected] Postfach www.vs.ch/web/sbma/patrimoine-archeologique 3001 Bern 4 +41 31 633 98 98 Cabane CAS du Wildhorn [email protected] Erziehungsdirektion des Kantons Bern www.be.ch/archaeologie Direction de l’instruction publique du canton de Berne Service des bâtiments, monuments et archéologie Amt für Kultur | Office de la culture Avenue du midi 18 3 Archäologischer Dienst des Kantons Bern Case postale Service archéologique du canton de Berne 1950 Sion +41 27 606 38 00 Postfach, 3001 Bern SBMA[email protected] Telefon +41 31 633 98 00 www.vs.ch/web/sbma/patrimoinearcheologique 1 Schnidejoch [email protected] www.be.ch/archaeologie Merci beaucoup ! D’autres services et informations sous www.alparch.ch Informations pratiques : L’Iffigenalp et le barrage de Tseuzier sont acces Le Schnidejoch et l’Iffigsee comme objectifs sibles en transports publics. -
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 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. -
Steep Rise of the Bernese Alps
Corporate Communication Media release, 24 March 2017 EMBARGOED UNTIL FRIDAY 24 MARCH 2017 11:00H CET Steep rise of the Bernese Alps The striKing North Face of the Bernese Alps is the result of a steep rise of rocKs from the depths following a collision of two tectonic plates. This steep rise gives new insight into the final stage of mountain building and provides important knowledge with regard to active natural hazards and geothermal energy. The results from researchers at the University of Bern and ETH Zürich are being published in the «Scientific Reports» specialist journal. Mountains often emerge when two tectonic plates converge, where the denser oceanic plate subducts beneath the lighter continental plate into the earth’s mantle according to standard models. But what happens if two continental plates of the same density collide, as was the case in the area of the Central Alps during the collision between Africa and Europe? Geologists and geophysicists at the University of Bern and ETH Zürich examined this question. They constructed the 3D geometry of deformation structures through several years of surface analysis in the Bernese Alps. With the help of seismic tomography, similar to ultrasound examinations on people, they also gained additional insight into the deep structure of the earth’s crust and beyond down to depths of 400 km in the earth’s mantle. Viscous rocKs from the depths A reconstruction based on this data indicated that the European crust’s light, crystalline rocks cannot be subducted to very deep depths but are detached from the earth’s mantle in the lower earth’s crust and are consequently forced back up to the earth’s surface by buoyancy forces. -
Active Strike-Slip Faulting in the Chablais Area (NW Alps) from Earthquake Focal Mechanisms and Relative Locations
CORE Metadata, citation and similar papers at core.ac.uk Provided by RERO DOC Digital Library 0012-9402/05/020189-11 Eclogae geol. Helv. 98 (2005) 189–199 DOI 10.1007/s00015-005-1159-4 Birkhäuser Verlag, Basel, 2005 Active strike-slip faulting in the Chablais area (NW Alps) from earthquake focal mechanisms and relative locations BASTIEN DELACOU1,NICHOLAS DEICHMANN2,CHRISTIAN SUE1,FRANÇOIS THOUVENOT3, JEAN-DANIEL CHAMPAGNAC1 & MARTIN BURKHARD1 Key words: Western Alps, Chablais, Prealpes, seismotectonics, relative location, active faulting ABSTRACT d’identifié des failles actives dans une région où les indices néotectoniques sont rares et controversés. L’alignement sismique ainsi défini correspond au The Chablais area is characterized by a complex geological setting, resulting plan nodal E-W du mécanisme au foyer du choc principal, permettant de défi- from the transport of nappes of various internal origins (the Prealpine nir une faille dextre, subverticale, orientée E-W. Ce régime décrochant, repla- nappes), thrusted in Oligocene times onto the Helvetic cover of the external cé dans son contexte tectonique régional, correspond à celui observé dans la zones of the Alps. While the structural setting and timing of nappe emplace- région Jura/Plateau Molassique, caractérisé par un système de décrochements ment are well understood, current tectonics and associated faulting remain un- conjugués (dextre orienté E-W, sénestre orienté NW-SE) et contraste avec clear. The detailed analysis of the Bonnevaux and Samoëns earthquakes, pre- celui exclusivement dextre, orienté NE-SW, observé au niveau de l’alignement sented in this study, constitutes a significant contribution to the active tecton- Wildhorn/Martigny. ics of the Chablais area. -
13 Protection: a Means for Sustainable Development? The
13 Protection: A Means for Sustainable Development? The Case of the Jungfrau- Aletsch-Bietschhorn World Heritage Site in Switzerland Astrid Wallner1, Stephan Rist2, Karina Liechti3, Urs Wiesmann4 Abstract The Jungfrau-Aletsch-Bietschhorn World Heritage Site (WHS) comprises main- ly natural high-mountain landscapes. The High Alps and impressive natu- ral landscapes are not the only feature making the region so attractive; its uniqueness also lies in the adjoining landscapes shaped by centuries of tra- ditional agricultural use. Given the dramatic changes in the agricultural sec- tor, the risk faced by cultural landscapes in the World Heritage Region is pos- sibly greater than that faced by the natural landscape inside the perimeter of the WHS. Inclusion on the World Heritage List was therefore an opportunity to contribute not only to the preservation of the ‘natural’ WHS: the protected part of the natural landscape is understood as the centrepiece of a strategy | downloaded: 1.10.2021 to enhance sustainable development in the entire region, including cultural landscapes. Maintaining the right balance between preservation of the WHS and promotion of sustainable regional development constitutes a key chal- lenge for management of the WHS. Local actors were heavily involved in the planning process in which the goals and objectives of the WHS were defined. This participatory process allowed examination of ongoing prob- lems and current opportunities, even though present ecological standards were a ‘non-negotiable’ feature. Therefore the basic patterns of valuation of the landscape by the different actors could not be modified. Nevertheless, the process made it possible to jointly define the present situation and thus create a basis for legitimising future action. -
Alps Village to Village Hiking
Alps Village to Village Hiking 10 Days Alps Village to Village Hiking Experience picturesque alpine hamlets and sweeping mountain vistas in Switzerland and France on this unforgettable hiking trilogy of the Alps. Tackle the legendary Eiger Trail at the foot of the Eiger's notorious north face, which has challenged mountaineers for over a century. Traverse canyon trails to discover imposing views of the iconic Matterhorn, and complete your tour in Chamonix, where the majestic Mont Blanc looms over the charming town. From Grindelwald to Zermatt to Chamonix, this 10-day tour will inspire and challenge even the most seasoned hiker. Details Testimonials Arrive: Geneva, Switzerland “This trip takes you to some of the most iconic hikes in the world. My only disappointment was that the Depart: Geneva, Switzerland trip was over! Great guides and wonderful hikes.” David M. Duration: 10 Days Group Size: 5-16 Guests "I've taken six MTS trips and they have all exceeded my expectations. The staff, the food, the logistics and Minimum Age: 18 Years Old the communications have always been exceptional. Thank you for being my "go to" adventure travel Activity Level: company!" Margaret I. REASON #01 REASON #02 REASON #03 This MT Sobek-crafted itinerary MT Sobek's expert guides have MT Sobek has been taking covers the must-see Alps in been leading treks in this region our travelers to the Alps since only 10 days — see the Eiger, for nearly 50 years, and this 1970 — we know the best hikes Matterhorn and Mont Blanc. grand tour is not to be missed. -
Alpine Summer Farms – Upland Animal Husbandry and Land Use Strategies in the Bernese Alps (Switzerland)
Special Volume 3 (2012), pp. 279–283 Brigitte Andres Alpine Summer Farms – Upland Animal Husbandry and Land Use Strategies in the Bernese Alps (Switzerland) in Wiebke Bebermeier – Robert Hebenstreit – Elke Kaiser – Jan Krause (eds.), Landscape Archaeology. Proceedings of the International Conference Held in Berlin, 6th – 8th June 2012 Edited by Gerd Graßhoff and Michael Meyer, Excellence Cluster Topoi, Berlin eTopoi ISSN 2192-2608 http://journal.topoi.org Except where otherwise noted, content is licensed under a Creative Commons Attribution 3.0 License: http://creativecommons.org/licenses/by/3.0 Brigitte Andres Alpine Summer Farms – Upland Animal Husbandry and Land Use Strategies in the Bernese Alps (Switzerland) Alpine archaeology; survey; ‘Alpwirtschaft;’ building remains; cultural landscape; Middle Ages; Modern Age. Introduction In 2003, 2004 and 2006 the Archaeological Service of the Canton of Bern carried out alpine archaeological surveys in three valleys of the Bernese Oberland.1 The primary aim of the survey was to enlarge the list of archaeological sites based on which the Archaeo- logical Service reacts to construction projects. The results were a positive surprise. About 400 new archaeological sites—mostly dating to the Middle Ages and Modern Age—could be recorded. A doctoral project will analyse the results of the field surveys.2 The archaeological structures found include remains of building foundations, installa- tions beneath rock shelters, animal pens and field boundary walls. They relate to seasonal alpine animal husbandry (‘Alpwirtschaft’), which has been an important economic factor in this region since the Middle Ages. In addition tracks and pathways, ore extraction sites and sites related to other industrial activities were documented. -
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. -
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. -
Karst and Caves of Switzerland
Jeannin, R-Y., 2016. Main karst and caves of Switzerland. Boletin Geoiôgico y Minera, 127 (1 ): 45-56 ISSN: 0366-0176 Main karst and caves of Switzerland R-Y Jeannin Swiss Instituts for Speleology and Karst-Studies, SISKA, PO Box 818, 2301 La Chaux-de-Fonds, Switzerland. [email protected] ABSTRACT This paper présents an overview of thé main karst areas and cave Systems in Switzerland. The first part encloses descriptions of thé main geological units that hold karst and caves in thé country and summari- zes a brief history of research and protection of thé cave environments. The second part présents three régions enclosing large cave Systems. Two régions in thé Alps enclose some of thé largest limestone caves in Europe: Siebenhengste (Siebenhengste cave System with -160 km and Bàrenschacht with 70 km) and Bodmeren-Silberen (Hblloch cave System with 200 km and Silberen System with 39 km). Thèse Systems are also among thé deepest with depths ranging between 880 and 1 340 m. The third example is from thé Jura Mountains (northern Switzerland). Key-words: caves, Hdlloch, karst, Siebenhengste, Switzerland. El karst y las cuevas mas importantes de Suiza RESUMEN Este îrabajo présenta una vision général de las principales areas kârsticas y sisiemas de cuevas en Suiza. La primera parte incluye descripciones de las principales unidades geologicas donde se desarrollan et karst y las cuevas en el pais, y résume una brève historia de la investigaciôn y protecciôn de los entornos de la cueva. La segunda parte présenta très regiones que incluyen sisîemas de grandes cuevas.