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Development Concept River Alpine Rhine
DEVELOPMENT CONCEPT RIVER ALPINE RHINE Zarn Benno1 THE RIVER ALPINE RHINE At Reichenau the Upper Rhine and Lower Rhine join and form the River Alpine Rhine (Fig. be- low). It mouths after 90 km into the Lake of Constance and drainages a catchment area of 6123 km2, which is situated in Switzerland (Cantons Grisons, St. Gallen and Ticino), in Austria (State of Vorarlberg), in Principality of Liechtenstein and in Italy. At the mouth of the Lake of Con- stance the mean annual discharge lies at 230 m3/s. The 100-year flood amounts in this reach to 3’100 m3/s. Fig.1: Overview over the River Alpine Rhine 1 Dr. Benno Zarn, dipl. Bau-Ing. ETH, [email protected], HUNZIKER, ZARN & PARTNER AG, VIA FLUCS 10, CH- 7013 DOMAT/EMS – 440 – – 441 – BASIC INVESTIGATION Before the work for the Development Concept started, comprehensive investigations in different fields were carried out. The most important studies were about hydrology, morphology and sedi- ment budget, damage risk at events higher than the design discharge, development of the River Rhine Valley, river and fish ecology, turbidity and daily discharge change due to hydro power and renaturation and hydro power. DEVELOPMENT CONCEPT The Development Concept was developed in a participatory planning process. The comparison of the actual state of the Alpine Rhine with the aims showed the need of action. An overview of the investigations of flood protection, river ecology, groundwater, and “live and work” was the basis. The Development Concept recommends a strategy and measures, which can summarised into six different measure types: river bed widening, improving fish wandering, reduction of the daily discharge change due to hydro power, hydro power, riverine zone, emergency release in case of events higher than the design discharge. -
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 -
High-Mountain Permafrost in the Austrian Alps (Europe)
HIGH-MOUNTAIN PERMAFROST IN THE AUSTRIAN ALPS (EUROPE) Gerhard Karl Lieb Institute of Geography University of Graz Heinrichstrasse 36 A-8010 Graz e-mail: [email protected] Abstract Permafrost research in the Austrian Alps (Eastern Alps) is based on a variety of methods, including at large scales, the measurement of the temperature of springs and of the base of winter snow cover, and at small scales, mainly an inventory of some 1450 rock glaciers. Taking all the information available into consideration, the lower limit of discontinuous permafrost is situated near 2500 m in most of the Austrian Alps. These results can be used for modelling the permafrost distribution within a geographical information system. Detailed investi- gations were carried out in the Doesen Valley (Hohe Tauern range) using additional methods, including several geophysical soundings. In this way, realistic estimates of certain permafrost characteristics and the volume of a large active rock glacier (some 15x106m3) were possible. This rock glacier has been chosen as a monitoring site to observe the effects of past and future climatic change. Introduction snow cover (BTS) and geophysical soundings, such as seismic, geoelectric, electromagnetic and ground pene- Although mountain permafrost in the Austrian Alps trating radar surveys have been published (survey and has caused construction problems and damage to buil- references in Lieb, 1996). The best results for mapping dings at several high-altitude locations, specific investi- the mere existence of permafrost were obtained by mea- gations of permafrost did not start until 1980. Since suring spring temperatures and BTS, both procedures then, studies of the distribution and certain characteris- being easily applicable and providing quite accurate tics of permafrost have been carried out at a number of interpretation. -
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. -
Chasmophytic Vegetation of Silicate Rocks on the Southern Outcrops of the Alps in Slovenia
ZOBODAT - www.zobodat.at Zoologisch-Botanische Datenbank/Zoological-Botanical Database Digitale Literatur/Digital Literature Zeitschrift/Journal: Wulfenia Jahr/Year: 2011 Band/Volume: 18 Autor(en)/Author(s): Juvan Nina, Carni [ÄŒarni] Andraz [Andraž], Jogan Nejc Artikel/Article: Chasmophytic vegetation of silicate rocks on the southern outcrops of the Alps in Slovenia. 133-156 © Landesmuseum für Kärnten; download www.landesmuseum.ktn.gv.at/wulfenia; www.biologiezentrum.at Wulfenia 18 (2011): 133 –156 Mitteilungen des Kärntner Botanikzentrums Klagenfurt Chasmophytic vegetation of silicate rocks on the southern outcrops of the Alps in Slovenia Nina Juvan, Andraž Čarni & Nejc Jogan Summary: Applying the standard central-European method we studied the chasmophytic vegetation of the silicate rocks on the southern outcrops of the Alps in the territory of Slovenia, in the Kamnik- Savinja Alps, the eastern Karavanke mountains, on Mt. Kozjak and the Pohorje mountains. Three communities of the order Androsacetalia vandellii (Asplenietea trichomanis) were recognized: Campanulo cochleariifoliae-Primuletum villosae ass. nova (Androsacion vandellii ), Woodsio ilvensis-Asplenietum septentrionalis (Asplenion septentrionalis) and Hypno-Polypodietum (Hypno-Polypodion vulgaris). The communities are distinguished by altitude, light intensity, temperature and the number of endemic species, south-European orophytes or cosmopolite species. Altitude is a signifi cant factor aff ecting the fl oristic composition of the studied vegetation. Keywords: chasmophytic -
Public Participation in River Basin Management in Switzerland
Public Participation in River Basin Management in Switzerland "Fighting against floods" This report has been produced as part of Workpackage 4 of the HarmoniCOP Project Colenco Power Engineering AG Täfernstrasse 26, CH-5405 Baden/Switzerland Tel.: ++41 56 483 12 12, Telefax ++41 56 483 12 55 [email protected] http://www.colenco.ch 15 December 2003 Contents Page Foreword .................................................................................................................................... 0 1 Introduction to Switzerland and general History ............................................................... 1 1.1 Country Profile........................................................................................................... 1 1.1.1 History................................................................................................................ 1 1.1.2 Political structure................................................................................................ 2 1.2 Geography, Climate and Hydrology .......................................................................... 2 1.2.1 Geography .......................................................................................................... 2 1.2.2 Climate ............................................................................................................... 2 1.2.3 Hydrology and Water Trends............................................................................. 3 1.2.4 Water Balance ................................................................................................... -
Provenance Determination of Paleochannel Infillings in the Alsatian Upper Rhine Floodplain Using Mid-Infrared Spectroscopy- Discriminant Analysis
EGU21-6701, updated on 27 Sep 2021 https://doi.org/10.5194/egusphere-egu21-6701 EGU General Assembly 2021 © Author(s) 2021. This work is distributed under the Creative Commons Attribution 4.0 License. Provenance Determination of Paleochannel Infillings in the Alsatian Upper Rhine Floodplain Using Mid-Infrared Spectroscopy- Discriminant Analysis Mubarak Abdulkarim1,4, Stoil Chapkanski2, Damien Ertlen3, Claire Rambeau3, Laurent Schmitt3, Louis Le Bouteiller3, and Frank Preusser1 1Institute of Earth and Environmental Science, University of Freiburg, Germany ([email protected] freiburg.de) 2Laboratory of Physical Geography (LGP), UMR 8591, University Paris 1, Pantheon-Sorbonne – CNRS, Paris France 3Laboratoire Image Ville Environnement (LIVE), UMR 7362, University of Strasbourg-CNRS-ENGEES, Strasbourg, France 4Department of Geology, Federal University Birnin Kebbi, Kebbi, Nigeria The Alsatian Upper Rhine floodplain (northeastern France) is characterized by a complex anastomosing network of paleochannels inherited from Late Glacial braided fluvial pattern of the Rhine system. These paleochannels are filled by mixed or stratified clastic and organic sediments originating from different sediment sources. Identifying these sediments' provenance is critically important for understanding past surface processes and reconstructing the Upper Rhine Valley evolution in the course of the Holocene. This study employed mid-infrared spectroscopy to determine the source of sediments and, therefore, understand which rivers may have contributed to the paleochannel infilling and establish the main patterns of filling through time. Sediment samples with unknown sedimentary provenance were collected in 16 sites consisting of paleochannels and the Ill River's levees. Mid-Infrared spectroscopic analyses were carried out on powdered (< 2 mm) samples using a Frontier Spectrometer (PerkinElmer) equipped with Diffuse Reflectance Infrared Fourier Transform accessory. -
HIKING in SLOVENIA Green
HIKING IN SLOVENIA Green. Active. Healthy. www.slovenia.info #ifeelsLOVEnia www.hiking-biking-slovenia.com |1 THE LOVE OF WALKING AT YOUR FINGERTIPS The green heart of Europe is home to active peop- le. Slovenia is a story of love, a love of being active in nature, which is almost second nature to Slovenians. In every large town or village, you can enjoy a view of green hills or Alpine peaks, and almost every Slove- nian loves to put on their hiking boots and yell out a hurrah in the embrace of the mountains. Thenew guidebook will show you the most beauti- ful hiking trails around Slovenia and tips on how to prepare for hiking, what to experience and taste, where to spend the night, and how to treat yourself after a long day of hiking. Save the dates of the biggest hiking celebrations in Slovenia – the Slovenia Hiking Festivals. Indeed, Slovenians walk always and everywhere. We are proud to celebrate 120 years of the Alpine Associati- on of Slovenia, the biggest volunteer organisation in Slovenia, responsible for maintaining mountain trails. Themountaineering culture and excitement about the beauty of Slovenia’s nature connects all generations, all Slovenian tourist farms and wine cellars. Experience this joy and connection between people in motion. This is the beginning of themighty Alpine mountain chain, where the mysterious Dinaric Alps reach their heights, and where karst caves dominate the subterranean world. There arerolling, wine-pro- ducing hills wherever you look, the Pannonian Plain spreads out like a carpet, and one can always sense the aroma of the salty Adriatic Sea. -
BROWN BEARS in AUSTRIA 10 Years of Conservation and Actions for the Future
Federal Environment Agency – Austria BROWN BEARS IN AUSTRIA 10 Years of Conservation and Actions for the Future Andreas ZEDROSSER Norbert GERSTL Georg RAUER MONOGRAPHIEN Band M-117 M-117 Wien, 1999 Projektleiter Erich Weigand Maria Tiefenbach (Federal Environment Agency – Austria) Autoren Andreas Zedrosser Norbert Gerstl Georg Rauer (World Wide Fund of Nature) Kartenerstellung Felix Lux (Federal Environment Agency – Austria) Titelphoto „Bears IN Austria“ (Illustration: Sibylle Vogel) Impressum Medieninhaber und Herausgeber: Umweltbundesamt GmbH (Federal Environment Agency Ltd) Spittelauer Lände 5, A-1090 Wien (Vienna), Austria Druck: Weitzer & Partner, 8045 Graz © Umweltbundesamt GmbH, Wien 1999 Alle Rechte vorbehalten (all rights reserved) ISBN 3-85457-524-6 Brown Bears in Austria – Inhalt 3 INHALT Seite SUMMARY............................................................................................................... 5 1 INTRODUCTION..................................................................................................... 6 2 A “SHORT” HISTORY OF BEARS IN AUSTRIA................................................ 7 2.1 The Ötscher Bear – Corn Telemetry and Rnergy Drinks....................................... 8 3 HOW EVERYTHING STARTED............................................................................ 9 4 THE REINTRODUCTION PROJECT.................................................................. 10 4.1 Chronology............................................................................................................ -
Quaternary Glaciation History of Northern Switzerland
Quaternary Science Journal GEOzOn SCiEnCE MEDiA Volume 60 / number 2–3 / 2011 / 282–305 / DOi 10.3285/eg.60.2-3.06 iSSn 0424-7116 E&G www.quaternary-science.net Quaternary glaciation history of northern switzerland Frank Preusser, Hans Rudolf Graf, Oskar keller, Edgar krayss, Christian Schlüchter Abstract: A revised glaciation history of the northern foreland of the Swiss Alps is presented by summarising field evidence and chronologi- cal data for different key sites and regions. The oldest Quaternary sediments of Switzerland are multiphase gravels intercalated by till and overbank deposits (‘Deckenschotter’). Important differences in the base level within the gravel deposits allows the distin- guishing of two complex units (‘Höhere Deckenschotter’, ‘Tiefere Deckenschotter’), separated by a period of substantial incision. Mammal remains place the older unit (‘Höhere Deckenschotter’) into zone MN 17 (2.6–1.8 Ma). Each of the complexes contains evidence for at least two, but probably up-to four, individual glaciations. In summary, up-to eight Early Pleistocene glaciations of the Swiss alpine foreland are proposed. The Early Pleistocene ‘Deckenschotter’ are separated from Middle Pleistocene deposition by a time of important erosion, likely related to tectonic movements and/or re-direction of the Alpine Rhine (Middle Pleistocene Reorganisation – MPR). The Middle-Late Pleistocene comprises four or five glaciations, named Möhlin, Habsburg, Hagenholz (uncertain, inadequately documented), Beringen, and Birrfeld after their key regions. The Möhlin Glaciation represents the most extensive glaciation of the Swiss alpine foreland while the Beringen Glaciation had a slightly lesser extent. The last glacial cycle (Birrfeld Glaciation) probably comprises three independent glacial advances dated to ca. -
Lindau, Germany and Take Your Bike on the Ferry to Rorschach, Switzerland
english Bodensee! LAKE CONSTANCE TRAVEL GUIDE One Lake. Four Countries. All Year Round. BODENSEE MAP INCLUDED HIGHLIGHTS EVENTS INSPIRATION www.bodensee.eu WELCOME Follow us on Instagram: bodensee.eu Share your Bodensee experiences by using the hashtag #bodensee4u © www.bayern.com | Gert Krautbauer © www.bayern.com CONTENT Bodensee passenger ships © Schaffhauserland Tourismus Dörflingen Rhine Welcome ................................................................................................... 3 Seasons .................................................................................................... 4 Must-Do .................................................................................................... 6 WELCOME TO THE Event Highlights ...................................................................................... 8 Four Countries ....................................................................................... 10 Bodensee Cities .................................................................................... 12 BODENSEE! Culinary Delights .................................................................................. 16 INFORMATION Bodensee Region – Unique in the World! Culture .................................................................................................... 20 Tourist Board of Lake Constance Active and nature ................................................................................. 24 Hafenstraße 6, 78462 Constance (Germany) Water ...................................................................................................... -
Aim Wp4 R4.2
Result evaluation and Project basic information Partners Pilot Areas assessment Total eligible Austria France Germany Italy Liechenstein Slovenia Switzerland Crossborder Type (tools, guidelines, methods,...) Title/Name Short description Name, web page Start End Keywords Main objectives Targeted stakeholders Austria France Germany Italy Liechenstein Slovenia Switzerland EU & International level Stage of development costs Name of area Activites on pilot area Name of area Activites on pilot area Name of area Activites on pilot area Name of area Activites on pilot area Name of area Activites on pilot area Name of area Activites on pilot area Name of area Activites on pilot area Name of area Activites on pilot area AlpWaterScarce - Water Management Strategies Autonomous Province of Trento - Geological Survey of Slovenia Federal Office for the Environment, Koralpe Past and Future Groundwater Savoy Implementation of Short-Term Crisis Scrivia River Basin Interregional Strategy to Improve Pohorje with Early Warning System development Spöl River Compromise between River Ecology Karavanken (A-SI) Interregional and Transboundary Cooperation to Secure Water Outcomes and recomendations Water Management in a Changing This is a common comprehensive report, which summarizes the AlpWaterScarce outputs (developed early warning systems adapted to the challenges at the local Final version elaborated against Water Scarcity in the Alps Department for Territorial Planning Federal Department for the Recharge and Runoff analysis. Management (2) Integrated Water