Group of Experts on Geographical Names Bevenm Sess.Cn WORKING PAPER Geneva, 15-23 October 1984 No
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St. Jodok, Schmirntal and Valsertal Mighty Mountains − Gentle Valleys
St. Jodok, Schmirntal and Valsertal Mighty mountains − gentle valleys MIT UNTERSTÜTZUNG VON BUND UND EUROPÄISCHER UNION Europäischer Landwirtschasfonds für die Entwicklung des ländlichen Raums: Hier investiert Europa in die ländlichen Gebiete Contents Mountaineering villages and the Alpine Convention 04 St. Jodok, Schmirntal and Valsertal – Mighty mountains – gentle valleys 06 Arrival and getting around 08 Special features 09 Recommended tours for summer 14 Recommended tours for winter 27 Alternative options for bad weather 33 Partners 34 Mountain huts 36 Important addresses 37 Publication details and picture credits 38 Tips on good conduct in the mountains 39 PEFC certified This product is from sustainably managed forests and controlled PEFC/06-39-27 sources. www.pefc.org Printed in accordiance to the Guideline “Low pollutant print products” of the Austrian ecolabel. klimaneutral klimaneutral gedruckt CP IKS-Nr.: 53401-1709-1017 gedruckt klimaneutral gedruckt “Bergsteigerdörfer” (mountaineering villages) are an initiative of the Austrian Alpine Association in cooperation with neighbouring Alpine Associations. They are supported by funding from the Austrian Federal Ministry of Agriculture, Forestry, Environment and Water Management (Ministry for a Liveable Austria) and the European Agricultural Fund for Rural Development. Mountaineering villages are an official implementation project of the Alpine Convention. Special edition, Innsbruck 2017 4 5 Mountaineering villages. The Alpine Convention in practice ! Linz Legend !Augsburg ! ! Wien National border !München Perimeter Alpine Convention Freiburg ! G E R M A N Y ! City ! make the Convention accessible to the wider public, atmosphere, a charming appearance, traditions kept River Salzburg !Kempten Lake transposing it from cumbersome German legalese alive, a high altitude landscape, an Alpine history !Basel Bregenz Leoben Glaciated area (> 3000 m) ! ! !Zürich into practical examples. -
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 -
National Parks Austria. Time for Nature
Time for nature. 6 national parks Nothing touches us under one roof. NATIONALPARK THAYATAL like the untouched. Nationalparkhaus, 2082 Hardegg T: +43 29 49 / 70 05-0 www.np-thayatal.at NATIONALPARK NATIONALPARK @nationalparkthayatal npthayatal Austria's six national parks, Thayatal (Thaya Valley), Hohe Tauern, DONAU-AUEN KALKALPEN Donau-Auen (Danube wetland), Gesäuse, Neusiedlersee- schlossORTH Nationalpark- Nationalpark Zentrum Molln parks the national of Austria for Time Zentrum, 2304 Orth/Donau Nationalpark Allee 1, 4591 Molln Seewinkel and the Kalkalpen (Limestone alps), protect the T: +43 22 12 / 35 55 T: +43 75 84 / 36 51 greatest natural treasures of our nation. Across a total of 2,380 www.donauauen.at www.kalkalpen.at square kilometres, they accommodate astonishing natural @np_donau_auen @nationalparkkalkalpen donauauen WaldWildnis NATIONALPARK landscapes and provide vital habitats for a large number of HOHE TAUERN endangered animals and plant species. Here in these enclosures, Carinthia: Besucherzentrum Mallnitz nature has enough space to evolve freely. It is the expressed Mallnitz 36, 9822 Mallnitz purpose of the national parks to safeguard these areas and keep T: +43 48 25 / 61 61 Salzburg: them alive for future generations Nationalparkzentrum Mittersill to come. NATIONALPARK NATIONALPARK Gerlosstraße 18, 5730 Mittersill T: +43 65 62 / 408 49 GESÄUSE NEUSIEDLER SEE Tyrol: Under the umbrella association “Nationalparks Austria”, these six Informationsbüro Admont – SEEWINKEL Nationalparkhaus Matrei Hauptstraße 35, 8911 Admont Kirchplatz 2, 9971 Matrei Austrian national parks are closely collaborating with the Federal Nationalpark Informations zentrum T: +43 36 13 / 211 60 20 T: +43 48 75 / 51 61-10 Illmitz, Hauswiese, 7142 Illmitz Ministry for Sustainability and Tourism, in a steady effort to raise www.nationalpark.co.at T: +43 21 75 / 34 42 www.hohetauern.at awareness for the immeasurable value of our natural heritage. -
51 20 Sommerfaltkarte EN.Indd
Want to see the towns and villages on the map? Please turn over! 1 Good to know 2 Region & people 1.1 Tourism Boards Long-distance hiking MTB Climbing Families X 1.2 Travelling to Tirol 2.1 Tirol‘s Mountains XX 2.3 Food & Drink Telephone number & Towns and villages in this region e-mail address Webseite Region good for ARRIVING BY TRAIN coming from Switzerland Tirol is a land of mountains, home to more than 500 summits International Intercity via St. Anton am Arlberg. over 3,000 metres. The northern part of Tirol is dominated by 1 Achensee Tourismus Achenkirch, Maurach, Pertisau, +43.5246.5300-0 www.achensee.com trains run by the ÖBB Drivers using Austrian the Northern Limestone Alps, which include the Wetterstein Steinberg am Rofan [email protected] (Austrian Federal Rail- motorways must pay a and Kaiser Mountains, the Brandenberg and Lechtal Alps, the ways) are a comfortable way toll charge. Toll stickers Karwendel Mountains and the Mieming Mountains. The Sou- 2 Alpbachtal Alpbach, Brandenberg, Breitenbach am Inn, +43.5337.21200 www.alpbachtal.at to get to Tirol. The central (Vignetten) can be bought Brixlegg, Kramsach, Kundl, Münster, Radfeld, [email protected] thern Limestone Alps run along the borders with Carinthia Rattenberg, Reith im Alpbachtal train station in Innsbruck from Austrian automobile and Italy. They comprise the Carnic and Gailtal Alps as well serves as an important hub associations as well as at as the Lienz Dolomites. The Limestone Alps were formed long 3 Erste Ferienregion Aschau, Bruck am Ziller, Fügen, Fügenberg, +43.5288.62262 www.best-of-zillertal.at im Zillertal Gerlos, Hart, Hippach, Hochfügen, Kaltenbach, [email protected] and so do the stations at petrol stations and border ago by sediments of an ancient ocean. -
Comparison of Mesozoic Successions of the Central Eastern Alps and the Central Western Carpathians 715-739 ©Geol
ZOBODAT - www.zobodat.at Zoologisch-Botanische Datenbank/Zoological-Botanical Database Digitale Literatur/Digital Literature Zeitschrift/Journal: Jahrbuch der Geologischen Bundesanstalt Jahr/Year: 1993 Band/Volume: 136 Autor(en)/Author(s): Häusler Hermann, Plasienka Dusan, Polak Milan Artikel/Article: Comparison of Mesozoic Successions of the Central Eastern Alps and the Central Western Carpathians 715-739 ©Geol. Bundesanstalt, Wien; download unter www.geologie.ac.at Gedenkband zum 100. Todestag von Dionys Stur Redaktion: Harald Lobitzer & Albert Daurer • Jb. Geol. B.-A. I ISSN 0016-7800 I Band 136 I Heft 4 S.715-739 I Wien, Dezember 1993 Comparison of Mesozoic Successions of the Central Eastern Alps and the Central Western Carpathians By HERMANN HÄUSLER, DUSAN PLASIENKA & MILAN POLAK*) With 5 Text-Figures and 2 Tables Österreich Slowakei Ostalpen Westkarpaten Mesozoikum Fazieskorrelation Paläogeographie Vahikum Contents Zusammenfassung 716 Abstract 716 1. Introduction 716 2. Mesozoic Tectonic Evolution: An Outline 718 2.1. Central Eastern Alps (H. HAuSLER) 720 2.2. Central Western Carpathians (D. PLA$IENKA) 721 3. Mesozoic Series ofthe Central Eastern Alps (H. HAuSLER) 724 3.1. The Lower Austroalpine 724 3.1.1. The Tarntal Mountains 724 3.1.2. The Radstadt Mountains 725 3.1.3. Semmering Series 725 3.2. The South Penninie System 725 3.2.1. The Northern Frame ofthe Tauern Window ("Nordrahmenzone") 721 3.2.1.1. The Penken-Gschößwand Range West of Mayrhofen/Zillertal (Tuxer Voralpen) 726 3.2.1.2. TheGerlosZone 726 3.2.1.3. The "Nordrahmenzone" South ofthe Salzach River 727 3.2.1.4. The "Nordrahmenzone" South ofthe Zederhaus Valley 727 3.2.2. -
Toll Prices 2020 Tmmm.At BREATHE in Ötztaler Alpen the Toll Prices Include Use of the Timmelsjoch High Alpine Garnets Road on Both the Austrian and the Italian Side
Meran timmelsjoch.tirol Toll prices 2020 tmmm.at BREATHE IN Ötztaler Alpen The toll prices include use of the Timmelsjoch High Alpine Garnets Road on both the Austrian AND the Italian side. the fresh alpine air Cars (max. 9 seats incl. driver, mobile homes up to 3.5 tons) single 17,– Moos / Moso TIMMELSJOCH Top Mountain Star Obergurgl return 24,– HIGH ALPINE ROAD M Passeiertal Skiing Area Motorcycles 2.509 Val Passiria Telescope Hochgurgl-Obergurgl (Reduction available for groups of 10 or more motorcycles) single 15,– Opening hours: May until October, 7 am to 8 pm Rabenstein return 21,– Hochgurgl Other VEHICLES (Mobile homes over 3.5 tons, lorries etc.) 28,– Pass Museum Walkway Schönau BUSES return (as well as all vehicles used for commercial Transit passenger transport e.g. taxis, hire cars, hotel minibuses etc.) Top Mountain Crosspoint per adult 5,– Timmelsjoch / Passo Rombo 2.509 m Summit tavern Toll station Ötztal per child (from 7 till 15 years) 3,– maximum 100,– minimum 25,– Season ticket for cars/motorcycles 80,– Ötztal Card: Holders of the Ötztal Card can use the Timmelsjoch Timmelsjoch High Alpine Road Innsbruck Smugglers High Alpine Road free of charge when travelling on the local bus. Trail E5 - European Walking Route Opening times At 2,509 m, the Timmelsjoch High Alpine The Timmelsjoch High Alpine Road is open daily from 7 am Road ranks among the highest paved passes to 8 pm from approximately the end of May until the end of October. The exact opening date can be found at: in Europe. Even in June, you may still see www.timmelsjoch.tirol metre-high walls of snow along the road. -
Age and Structure of the Stolzalpe Nappe
AgeAge andand structurestructure ofof thethe StolzalpeStolzalpe nappenappe -- EvidenceEvidence forfor VariscanVariscan metamorphism,metamorphism, EoalpineEoalpine top-to-the-WNWtop-to-the-WNW thrustingthrusting andand top-to-the-ESEtop-to-the-ESE normalnormal faultingfaulting (Gurktal(Gurktal Alps,Alps, Austria)Austria) Geological Survey of Austria C. IGLSEDER1,*) , B. HUET1,*) , G. RANTITSCH2,*), L. RATSCHBACHER3,*) & J. PFÄNDER3,*) INTRODUCTION: OVERVIEW: 17° 16° 15° 14° 10° 11° 12° 13° Tectonic map of the Alps Passau S.M. Schmid, B. Fügenschuh, E. Kissling and R. Schuster , 2004 Donau Inn In the Gurktal Alps (Austria,) the Drauzug-Gurktal nappe system represents the Graphics : S. Lauer Wien 5° 6° 48° 48° 7° München 8° 9° 5240000 Rhein Basel Zürich uppermost tectonic part of the Upper Austro-Alpine nappe stack. The Stolzalpe Nappe Besancon 47° 47° Graz Bern Maribor ± Drava (s. str.) is its uppermost unit. It consists of interbedded metasedimentary rocks of the Genève 46° 46° Rhone T Zagreb agliamento Sava 5230000 Trieste Milano Venezia Verona Padova Spielriegel Complex, overlain by metavolcanic rocks of the Kaser-Eisenhut Complex. Grenoble Torino 45° 45° Po 17° Po 16° 15° 14° 100 km 11° 12° 13° Both are covered by the Pennsylvanian clastic Stangnock Formation. In the Genova 44° Durance 5° 6° Nice 7° 8° 9° 10° investigated area, located at UTM-map sheet Radenthein (NL-33-04-06), the 5220000 Stolzalpe Nappe tectonically overlays the Stangnock Formation belonging to the Tectonic map of the investigated area Königstuhl Subnappe, also part -
A New Evaluation of Fluid Inclusion Data Based on Thermal Basin Modeling for the Drau Range, Eastern Alps
ZOBODAT - www.zobodat.at Zoologisch-Botanische Datenbank/Zoological-Botanical Database Digitale Literatur/Digital Literature Zeitschrift/Journal: Austrian Journal of Earth Sciences Jahr/Year: 2000 Band/Volume: 93 Autor(en)/Author(s): Rantitsch Gerd Artikel/Article: A new evaluation of fluid inclusion data based on thermal basin modeling for the Drau Range, Eastern Alps. 77-85 © Österreichische Geologische Gesellschaft/Austria; download unter www.geol-ges.at/ und www.biologiezentrum.at Mitt. Osterr. Geol. Ges. ISSN 0251-7493 93(2000) 77-85 Wien, Juni 2003 Eastern Alps Drau Range Fluid inclusions Basin modeling A new evaluation of fluid inclusion data based on thermal basin modeling for the Drau Range, Eastern Alps GERD RANTITSCH1 3 Figures and 1 Table Content Abstract 77 Zusammenfassung 77 1. Introduction 79 2. Geological setting 79 3. Fluid inclusion data 79 4. Isochore calculation 82 5. Discussion 82 6. Conclusions 84 7. Acknowledgement 84 References 84 Abstract Published microthermometrical data of fluid inclusions, which were trapped near or subsequent to the time of maximum subsidence of the Drau Range (Eastern Alps) have been used to evaluate the relationship between fluid flow and heat transfer. The evaluation is based on a numerical 1-D heat flow model, calibrated with vitrinite reflectance values. Aqueous fluid inclusions in quartz fissures crosscutting Permo-Scythian sediments and in fluorites hosted by Carnian carbonates give evidence for conductive heat transfer during fluid flow in the Late Cretaceous/Neogene. This implies that trapping temperatures of these fluids (125 °C to 220 °C in quartz, 115 °C to 180 °C in fluorite) can be used to approximate the burial temperatures (190 °C in the Permo-Scythian, 130 °C to 150 °C in the Carnian). -
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. -
AUSTRIAN JOURNAL of EARTH SCIENCES Volume 98 2005
© Österreichische Geologische Gesellschaft/Austria; download unter www.geol-ges.at/ und www.biologiezentrum.at AUSTRIAN JOURNAL of EARTH SCIENCES [MITTEILUNGEN der ÖSTERREICHISCHEN GEOLOGISCHEN GESELLSCHAFT] an INTERNATIONAL JOURNAL of the AUSTRIAN GEOLOGICAL SOCIETY volume 98 2005 István DUNKL, Joachim KUHLEMANN, John REINECKER & Wolfgang FRISCH: Cenozoic relief evolution of the Eastern Alps – constraints from apatite fission track age-provenance of Neogene intramontane sediments__________________________________________________________________________ www.univie.ac.at/ajes EDITING: Grasemann Bernhard, Wagreich Michael PUBLISCHER: Österreichische Geologische Gesellschaft Rasumofskygasse 23, A-1031 Wien TYPESETTER: Irnberger Norbert, www.irnberger.net Copy-Shop Urban, Bahnstraße 26a, 2130 Mistelbach PRINTER: Holzhausen Druck & Medien GmbH Holzhausenplatz 1, 1140 Wien ISSN 0251-7493 © Österreichische Geologische Gesellschaft/Austria; download unter www.geol-ges.at/ und www.biologiezentrum.at Austrian Journal of Earth Sciences Volume 98 Vienna 2005 Cenozoic relief evolution of the Eastern Alps – con- straints from apatite fission track age-provenance of Neogene intramontane sediments István DUNKL1)*), Joachim KUHLEMANN2), John REINECKER2) & Wolfgang FRISCH2) KEYWORDS paleogeography fission track provenance 1) Sedimentology, Geoscience Center, University of Göttingen exhumation 2) Institute of Geosciences, University of Tübingen sediment relief *) Corresponding author, [email protected] Alps Abstract Fission track (FT) ages -
Jahrbuch Der Geologischen Bundesanstalt
ZOBODAT - www.zobodat.at Zoologisch-Botanische Datenbank/Zoological-Botanical Database Digitale Literatur/Digital Literature Zeitschrift/Journal: Jahrbuch der Geologischen Bundesanstalt Jahr/Year: 2018 Band/Volume: 158 Autor(en)/Author(s): Schönlaub Hans-Peter Artikel/Article: Review of the Devonian/Carboniferous boundary in the Carnic Alps 29- 47 JAHRBUCH DER GEOLOGISCHEN BUNDESANSTALT Jb. Geol. B.-A. ISSN 0016–7800 Band 158 Heft 1–4 S. 29–47 Wien, Dezember 2018 Review of the Devonian/Carboniferous boundary in the Carnic Alps HANS P. SCHÖNLAUB* 16 Text-Figures Österreichische Karte 1:50.000 Italy BMN / UTM Carnic Alps 197 Kötschach / NL 33-04-09 Oberdrauburg Devonian 197 Kötschach / NL 33-04-10 Kötschach-Mauthen Carboniferous Conodonts Hangenberg Crisis Contents Abstract ................................................................................................ 29 Zusammenfassung ........................................................................................ 30 Current knowledge ........................................................................................ 30 Review of sedimentary and tectonic history ..................................................................... 32 Important stratigraphic markers .............................................................................. 32 Middle and Upper Ordovician ............................................................................. 32 Silurian .............................................................................................. 32 Devonian............................................................................................ -
Final Report
Final Report edited by Martin Rutzinger Kati Heinrich Axel Borsdorf Johann Stötter “permAfrost – Austrian Permafrost Research Initiative. Final Report” edited by Martin Rutzinger, Kati Heinrich, Axel Borsdorf, and Johann Stötter (Institute for Interdisciplinary Mountain Research, ÖAW) Design: Kati Heinrich & Fides Braun (Institute for Interdisciplinary Mountain Research, ÖAW) Responsibility for content, tables and figures of each chapter rests with the corresponding authors. All visuals are by the respective authors if no sources are given. ISBN: 978-3-7001-7577-3 (online) DOI: 10.1553/IGF-1 Preface The Austrian Permafrost Research Initiative (permAfrost) is a national project started in 2009 and funded by the research framework program “Alpenforschung” administrated by the Austrian Academy of Sciences. The project has been conducted by five research partners in Austria, which are the Institute of Geography and Re- gional Sciences of the University of Graz, the Institute of Geology of the University of Innsbruck, the Depart- ment of Geography and Geology of the University of Salzburg, the Institute of Geography of the University of Innsbruck. The project was coordinated by the Institute for Interdisciplinary Mountain Research of the Austrian Academy of Sciences. permAfrost is the first Austrian effort to bring together permafrost research on a national scale. Major tasks within the project are the research fields of • permafrost reformation and degradation • monitoring climate change impact on rock glacier behavior • hydrogeological investigation of changed permafrost discharge • detecting and quantifying area wide permafrost change The project finalized in 2013 is now looking back to the establishment of a close network of national per- mafrost activities including a large variety of research activities resulting in several outputs such as scientific papers partly published in index scientific journals, contributions at national and international conferences and workshops, and the elaboration of PhD, MSc and BSc thesis.