ALPBIONET2030 Integrative Alpine Wildlife and Habitat Management for the Next Generation
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Marc JOUBERT Né Le 14 Juillet 1927 Guide De Haute Montagne À Rive De Gier 42
MJMAMONTAGNE.doc MA MONTAGNE CRE 2001 / MAJ 18072015 Marc JOUBERT Né le 14 juillet 1927 Guide de Haute Montagne à Rive de Gier 42 Pourquoi j’aime gravir les sommets ! <><> 31/05/19 110 1 MJMAMONTAGNE.doc MA MONTAGNE CRE 2001 / MAJ 18072015 Pour mes enfants et mes petits enfants, et mes ami(e)s de la montagne. SOMMAIRE Chapitre I : Comment j’ai eu la révélation du rocher ? (Le déclic !). Chapitre II : Mon armée aux Chasseurs Alpins. (Les camarades, l’Autriche, les manœuvres …). Chapitre III : Mon Brevet de Guide de Haute Montagne. Chapitre IV : Description de quelques-unes de mes plus belles courses. (La Bérarde, le Chardonnet, la Traversée Nonne-Evêque, le Dru face ouest, L’arête sud de la Noire, le tour du Mont Blanc, …). Chapitre V : Le ski de raid. (Chamonix-Zermatt…) Chapitre VI : Randonnées pédestres. (Les Calanques…) Chapitre VII : Expéditions à l’étranger. <><> 31/05/19 110 2 MJMAMONTAGNE.doc MA MONTAGNE CRE 2001 / MAJ 18072015 Marc JOUBERT Guide de Haute Montagne Chapitre I : COMMENT J’AI EU LA REVELATION DU ROCHER ? <><> 31/05/19 110 3 MJMAMONTAGNE.doc MA MONTAGNE CRE 2001 / MAJ 18072015 MA DECOUVERTE DE LA MONTAGNE. Je me souviens, c’était en 1943 que j’ai connu l’escalade dans la carrière du Mouillon à RIVE DE GIER. J’avais 16 ans. C’était un amoncellement de blocs de grès qui ont écorché pas mal mes genoux. Une corde, qui était plus une corde à faire des bottes de foin, que j’avais achetée chez le quincaillier du coin, a été mon premier accessoire de grimpeur avec des espadrilles de corde. -
Geological Excursion BASE-Line Earth
Geological Excursion BASE-LiNE Earth (Graz Paleozoic, Geopark Karavanke, Austria) 7.6. – 9.6. 2016 Route: 1. Day: Graz Paleozoic in the vicinity of Graz. Devonian Limestone with brachiopods. Bus transfer to Bad Eisenkappel. 2. Day: Visit of Geopark Center in Bad Eisenkappel. Walk on Hochobir (2.139 m) – Triassic carbonates. 3. Day: Bus transfer to Mezica (Slo) – visit of lead and zinc mine (Triassic carbonates). Transfer back to Graz. CONTENT Route: ................................................................................................................................... 1 Graz Paleozoic ...................................................................................................................... 2 Mesozoic of Northern Karavanke .......................................................................................... 6 Linking geology between the Geoparks Carnic and Karavanke Alps across the Periadriatic Line ....................................................................................................................................... 9 I: Introduction ..................................................................................................................... 9 II. Tectonic subdivision and correlation .............................................................................10 Geodynamic evolution ...................................................................................................16 Alpine history in eight steps ...........................................................................................17 -
Zur Geologie Des Hochlantsch (Grazer Paläozoikum, Steiermark)
Jb. Geol. B.-A. ISSN 0016-7800 Band 128 S.43-73 Wien, Mai 1985 Zur Geologie des Hochlantsch (Grazer Paläozoikum, Steiermark) Von JOHANN GOLLNER & CHRISTIAN ZIER*) Mit 9 Abbildungen, 2 Tabellen und 6 Tafeln Steiermark Grazer Paläozoikum Stratigraphie 6sterreichische Karte1: 50.000 Fazies Blatt 134 Tektonik Inhalt Zusammenfassung, Summary 43 1. 6i;~e~~~~O~~ik~~':::::::::::::::::::::::::::::::::::::::::::::::::::::::::::::::::::::::::::::::::: 1.1. Die Hochlantschgruppe 44 1.1.1. Dolomitsandsteinfolge 46 1.1.2. "Gesteine des Breitalmkreuz" 47 1.1.3. Barrandeischichten " 47 1.1.4. Tyrnauer Alm-Formation 48 1.1.5. Zachenspitzformation 50 1.1.6. Steinbergkalk 51 1.1.7. Hochlantschkalk 51 1.1.8. Mixnitzer Karbon 52 1.2. Laufnitzdorfer Gruppe 52 1.3. "Kalkschieferfolge" 53 1.3.1. Tektonische Position der "Kalkschieferfolge" 53 1.3:2. "Gschwendtformation", "Heubergformation" , "Koglerformation", "Höllgrabeneinheit" 53 1.3.3. Größkogelgruppe 54 2. Postpaläozoische Ablagerungen 55 2.1. Gams/Bärenschützkonglomerat 55 2.2. Tertiärkonglomerat 55 2.3. Burgstallbrekzie 55 2.4. Gehängebrekzien und Schuttbildungen 56 2.5. Quartäre Spalten 57 3. Tektonischer Bau 57 ~i~;r~tu'r' : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : : ~g Zusammenfassung campan) verglichen wird, tritt in unterschiedlichen Höhenni- Der Hochlantsch als nördlicher Eckpfeiler des Grazer Paläo- veaus im Hangenden des Hochlantschkalks (Hochlantschgrup- zoikums ist -
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. -
Revue N°10, 1982 Sommaire
Revue n°10, 1982 Sommaire EDITORIAL .......................................................................................................................................................................................3 LA PETITE REINE ............................................................................................................................................................................4 LA COLITE ........................................................................................................................................................................................5 LA COLITE FRÉNÉTIQUE ..............................................................................................................................................................7 DES PETITS VÉLOS SUR L’ETNA .................................................................................................................................................8 TOUR DE FRANCE .........................................................................................................................................................................9 LES CARTES !!!.................................................................................................................................................................................10 FAUT LE FER ....................................................................................................................................................................................12 UN JOUR QU’IL FAISAIT TRES -
The ALPS in 25 MAPS Imprint
The ALPS in 25 MAPS Imprint Editor: Coordination: Permanent Secretariat of the Alpine Convention Marianna Elmi (Permanent Secretariat of the Alpine Convention) Thomas Streifeneder (Institute for Regional Development, Eurac Research) Editing: Marianna Elmi Cartographic coordination: Elisa Ravazzoli (Institute for Regional Development, Eurac Research) Contributors: Marianna Elmi (Permanent Secretariat of the Alpine Convention) Thomas Streifeneder, Elisa Ravazzoli, Peter Laner (Institute for Regional Development, Eurac Research) Marcello Petitta, Kathrin Renner (Institute for Earth Observation, Eurac Research) Giulia Garegnani, Valentina D’Alonzo (Institute for Renewable Energy, Eurac Research) Alice Brambilla, Bruno Bassano (Alpine Wildlife Research Centre, Gran Paradiso National Park, IT) and Main office: Achaz von Hardenberg (Conservation Biology Research Group, Department of Biological Sciences, University of Chester, UK) Herzog-Friedrich-Straße 15 Dominik Cremer-Schulte, Maša Klemenčič (ALPARC) A-6020 Innsbruck Austria In cooperation with Branch office: English revision: iui – innsbruck university innovations Viale Druso - Drususallee 1 I-39100 Bolzano - Bozen Graphic design: De Poli e Cometto - Printing: Stampatori della Marca - Cover photo: Shutterstock Italy ISBN: 9788897500438 www.alpconv.org [email protected] Facebook: Alpine Convention © Permanent Secretariat Twitter: @alpconv of the Alpine Convention, 2018 ALPINE CONVENTION The ALPS in 25 MAPS Foreword The Alps belong to our collective imagination. It is virtually impossible to repercussions. Mapping these phenomena comes almost as a first instinct speak about the Alps without evoking specific memories of places, sounds and allows us to represent them in a simple, immediate way. It lets us and tastes in individuals with different experiences and perspectives. If interpret spatial impacts, sometimes down to a very fine level of detail. -
How to Reach Bolzano/Bozen by Plane by Bus And/Or Train
How to reach Bolzano/Bozen By plane The nearest international airports are Innsbruck (Austria) and Verona (Italy). Other airports you can fly to are Bologna, Milan, Venice and Munich (Germany). From these airports, you can travel to Bolzano/Bozen by shuttle bus, by train or by car. On the websites of these airports, you can find the information regarding the bus transfer to/from railway stations. See also the information below. By bus and/or train Bolzano/Bozen can be reached easily from Munich (Germany) and Innsbruck (Austria) as well as from Verona, Bologna, Venice and Milan (Italy). Bus shuttles from the airports to Bolzano can be booked online at https://www.altoadigebus.com and http://www.busgroup.eu/en. Flixbus runs buses from various German, Austrian and Italian cities to Bolzano/Bozen. More information and timetables on https://www.flixbus.com. The railway connections are the following: From north: From Munich, Eurocity-trains run every two hours during the day directly to South Tyrol (via Innsbruck). More Information and timetables on www.bahn.de. From Innsbruck, there are several daily regional trains Bolzano/Bozen. Information and timetables on www.oebb.at. More information on the public regional transport in South Tyrol at http://www.sii.bz.it. From east: From Vienna via Villach to Lienz (Austria), by regional trains further to South Tyrol. Information and timetables on www.oebb.at. More information on the public regional transport in South Tyrol at http://www.sii.bz.it. From south: Fast train connections from Rome (direct train 5 times a day), Bologna (direct trains), Milan and Venice (changing in Verona) to Bolzano/Bolzano. -
Engineering Geology in Mountainous Regions 257-286 ©Geol
ZOBODAT - www.zobodat.at Zoologisch-Botanische Datenbank/Zoological-Botanical Database Digitale Literatur/Digital Literature Zeitschrift/Journal: Abhandlungen der Geologischen Bundesanstalt in Wien Jahr/Year: 1980 Band/Volume: 34 Autor(en)/Author(s): Horninger Georg, Weiss Ernst Heinrich Artikel/Article: Engineering Geology in Mountainous Regions 257-286 ©Geol. Bundesanstalt, Wien; download unter www.geologie.ac.at Abh. Geol. B.-A. 34 26e C. G. I. p. 257—286 14 figures Wien 1. 5. 1980 International Geological Congress 26th Session Excursion 132 C Engineering Geology in Mountainous Regions by G. HORNINGER and E. H. WEISS Address of the authors: Prof. Dr. G. HORNINGER, Department Head, Technical University, Karlsplatz 13, A-1040 Vienna, Austria; Prof. Dr. ERNST H. WEISS, Head, Department of Soil Science and Engineering Geology, Universität für Bodenkultur, Gregor Mendel Straße 33, A-1180 Vienna, Austria. ©Geol. Bundesanstalt, Wien; download unter www.geologie.ac.at Introduction window" to the east of the valley, and the overriding western complex of the austro-alpine ötztal gneiss- The basic idea to this excursion is to take the partici mass. The rocks bordering the said overthrust plane are pants to structures that offered special problems, either heavily solicitated, partly down to loamlike ultramylo- to the design or, as in most cases, to construction, last nites (see stop 1.2, Stefansbrücke, pit for brickloam and but not least even to the state of exploitation on grounds gravel pit). Additional solicitations derived from se of long-term security measures and permanent moni condary displacements along parts of the overthrust, toring. i. e. "Silltal fault", dipping under medium angles to the Because of the necessity to fix the final schedule to SW to W. -
Canton Ticino and the Italian Swiss Immigration to California
Swiss American Historical Society Review Volume 56 Number 1 Article 7 2020 Canton Ticino And The Italian Swiss Immigration To California Tony Quinn 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 Quinn, Tony (2020) "Canton Ticino And The Italian Swiss Immigration To California," Swiss American Historical Society Review: Vol. 56 : No. 1 , Article 7. Available at: https://scholarsarchive.byu.edu/sahs_review/vol56/iss1/7 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]. Quinn: Canton Ticino And The Italian Swiss Immigration To California Canton Ticino and the Italian Swiss Immigration to California by Tony Quinn “The southernmost of Switzerland’s twenty-six cantons, the Ticino, may speak Italian, sing Italian, eat Italian, drink Italian and rival any Italian region in scenic beauty—but it isn’t Italy,” so writes author Paul Hofmann1 describing the one Swiss canton where Italian is the required language and the cultural tie is to Italy to the south, not to the rest of Switzerland to the north. Unlike the German and French speaking parts of Switzerland with an identity distinct from Germany and France, Italian Switzerland, which accounts for only five percent of the country, clings strongly to its Italian heritage. But at the same time, the Ticinese2 are fully Swiss, very proud of being part of Switzerland, and with an air of disapproval of Italy’s ever present government crises and its tie to the European Union and the Euro zone, neither of which Ticino has the slightest interest in joining. -
Vues Nouvelles Sur La Structure Des Massifs Des Bornes Et Des Bauges Orientales
Géologie Alpine, 1996, t. 72, p. 35-59 Vues nouvelles sur la structure des massifs des Bornes et des Bauges orientales par Maurice GIDON * RÉSUMÉ. — Les failles de l'Arcalod (dans les Bauges) et du Charvin (dans les Bornes orientales), d'une part, et (plus hypothétiquement) l'accident médian de Belledonne, d'autre part, ne constituent qu'une seule et même grande cassure. Apparue en faille extensive au Nummulitique elle a ensuite été reprise en coulissement (comme prolongement du grand cisaillement dextre Simplon-Rhône), puis finalement déformée par enroulement lors de la surrection de l'antiforme des massifs cristallins externes. Le synclinal de Serraval - Arclusaz est l'un des responsables de cette déformation posthume. Au sens strict il ne représente que le tronçon intéressant les massifs des Bornes et des Bauges d'un grand "synclinal bordier des massifs cristallins externes" qui s'est formé après la phase de plissement général des massifs subalpins septentrionaux et en recoupe les virgations. La géométrie des autres failles du massif témoigne également d'une tectonique polyphasée analogue à celle antérieurement reconnue à la latitude de Grenoble. Ces conclusions permettent de mieux préciser la chronologie des étapes de déformation des massifs subalpins septentrionaux. Elles contredisent beaucoup des arguments avancés en faveur de l'hypothèse d'un éventuel chevauchement profond des massifs cristallins externes des Alpes septentrionales françaises et conduisent à envisager d'autres schémas explicatifs pour les rapports de ces derniers avec les chaînes subalpines septentrionales. MOTS CLÉS. — Bauges, Bornes, Décrochement, Chevauchement, Plis, Failles, Tectonique polyphasée Tectonics of the Bornes and eastern Bauges massifs (french external Alps, Haute-Savoie, France) : new data and their régional significance ABSTRACT. -
The Italian Swiss DNA
Swiss American Historical Society Review Volume 52 Number 1 Article 2 2-2016 The Italian Swiss DNA Tony Quinn 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 Quinn, Tony (2016) "The Italian Swiss DNA," Swiss American Historical Society Review: Vol. 52 : No. 1 , Article 2. Available at: https://scholarsarchive.byu.edu/sahs_review/vol52/iss1/2 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]. Quinn: The Italian Swiss DNA The Italian Swiss DNA by Tony Quinn* DNA testing is the new frontier in genealogical research. While the paper records of American and European churches and civil bodies are now generally available on line, DNA opens a new avenue of research into the period well before the advent of written records. And it is allowing people to make connections heretofore impossible to make. Recent historical examples are nothing short of amazing. When the bodies thought to be the last Russian Czar and his family, murdered in 1918, were discovered, a 1998 test using the DNA of Prince Philip proved conclusively that the bodies were indeed the Czar and his family. That is because Prince Philip and the Czarina Alexandra shared the same maternal line, and thus the same mitochondrial DNA. Even more remarkable was the "king in the car park," a body found under a parking lot in England thought to be King Richard III, killed at the Battle of Bosworth Field in 1485. -
Richtlinien Für Die Herstellung
12th Congress INTERPRAEVENT 2012 Grenoble / France – Extended Abstracts www.interpraevent.at HIGH-FREQUENCY MONITORING OF DEBRIS FLOWS IN THE FRENCH ALPS PRELIMINARY RESULTS OF A STARTING PROGRAM Oldrich Navratil1, Frédéric Liébault1, Hervé Bellot1, Joshua Theule1, Eric Travaglini1, Xavier Ravanat1, Frédéric Ousset1, Dominique Laigle1, Vincent Segel2 and Marc Fiquet3 Small upland catchments in degraded terrains are prone to debris flows which may endanger the safety of life and infrastructure in the vicinity of torrent channels. These flows mobilise high sediment loads and they are often responsible for most of the sediment yield from upland headwaters. Despite their importance in terms of natural hazard prevention and sediment management in upland catchments, our understanding of the mechanisms that control debris-flow initiation, propagation and deposition is still largely insufficient. This is partly explained by the paucity of field observation programs dedicated to channelized debris flows. Such programs need to overcome several difficulties related to the nature of the phenomena: debris flows are rapid, short-lasting, rare and destructive events that need a sophisticated and robust monitoring strategy to guarantee a performing reconstitution of natural processes. Over the last 20 years, increasing efforts have been undertaken in Europe, United States and Asia to develop high-frequency debris-flow monitoring stations. However, in the French Alps, despite the presence of very active debris-flow torrents and a long historical legacy of torrent-control works, there isn’t any instrumented torrent dedicated to the study of debris-flow activity. Another deficiency is that monitoring programs generally focus on at-a-station flow properties (velocity, stage, shear strength), but they don’t really emphasized the downstream changing nature of a debris flow and its interactions with torrent channel morphology.