An Introduction to Austrian Karst
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Traces to the Oldest Flint and Rock Crystal Mining Places in the Austrian
Stéfan Tzortzis et Xavier Delestre (dir.) Archéologie de la montagne européenne Actes de la table ronde internationale de Gap, 29 septembre-1er octobre 2008 Publications du Centre Camille Jullian Traces to the oldest flint and rock crystal mining places in the Austrian Alps Les plus anciens sites d’extraction de silex et de cristal de roche dans les Alpes autrichiennes Walter Leitner Éditeur : Publications du Centre Camille Jullian, Éditions Errance Lieu d'édition : Aix-en-Provence Année d'édition : 2010 Date de mise en ligne : 13 février 2020 Collection : Bibliothèque d’archéologie méditerranéenne et africaine ISBN électronique : 9782957155736 http://books.openedition.org Édition imprimée Date de publication : 1 juin 2010 Référence électronique LEITNER, Walter. Traces to the oldest flint and rock crystal mining places in the Austrian Alps In : Archéologie de la montagne européenne : Actes de la table ronde internationale de Gap, 29 septembre-1er octobre 2008 [en ligne]. Aix-en-Provence : Publications du Centre Camille Jullian, 2010 (généré le 03 avril 2020). Disponible sur Internet : <http://books.openedition.org/pccj/337>. ISBN : 9782957155736. II. CHRONOLOGIES, PALÉO-ENVIRONNEMENT, MODALITÉS DE FRÉQUENTATION ET D’EXPLOITATION Fig. 1. Map of Western Austria with the four find-spots in the investigation area (Landsat/ESA ©). Fig. 2. The wooded hilltop of the Bärenkopf in the Gemsteltal. The red circle marks the mining area (© Walter Leitner). Fig. 3. Stepped formation of the radiolarite layers as a result of man-made reduction (© Walter Leitner). 152 Traces to the oldest flint and rock crystal mining places in the Austrian Alps Walter leiTner* Abstract. Recently the Institute of Archaeology (Dep. -
Route Tauernradweg (Pdf)
Dort, wo die Krimmler Wasserfälle tosend in die Tiefe rauschen, liegt der Ausgangspunkt zum Tauernradweg. TAUERNRADWEG GENUSSTOUR ZWISCHEN WASSERFÄLLEN UND MOZARTSTADT Entlang der Flüsse Salzach und Saalach und vor der Bergkulisse der Tauern bietet diese Route eine bemerkenswerte Anzahl an herausragen- den Naturszenarien und kulturellen Höhepunkten zwischen dem Salz- burger Land und Oberösterreich. DIE HIGHLIGHTS DER ROUTE Faszinierender kann ein Tourbeginn nicht sein. Mit den Krimmler Tauernradwegrunde: Zusehends gefragter wird die- IM ÜBERBLICK Wasserfällen, den höchsten Mitteleuropas, präsentiert sich ein ser Klassiker als 270 km lange, grenzüberschreiten- • Krimmler Wasserfälle fesselndes Naturschauspiel: tosend in die Tiefe stürzendes de Rundstrecke. Der Ausgangspunkt ist beliebig • Nationalparkzentrum Wasser, dessen Sprühregen den Radfahrern eine wohltuende wählbar. Startet man in der Mozartstadt Salzburg, Mittersill Abkühlung beschert. Am Rande des Nationalparks Hohe Tauern wird über Bad Reichenhall und Lofer nach Zell am • Liechtensteinklamm und vor herrlicher Bergkulisse geht es der Salzach entlang. Nicht See geradelt. In Zell am See bringt die neue Pinzgau- St. Johann-Alpendorf verpassen sollte man das Nationalparkzentrum in Mittersill oder er Lokalbahn den Radwanderer nach Krimml. Die • Burg Hohenwerfen das neue Tauern Spa in Kaprun. Hier bieten sich auch die Stau- Besichtigung der eindrucksvollen Wasserfälle ist • Eisriesenwelt, größte seen Glockner-Kaprun und der Großglockner als lohnenswerte Pflicht, ehe man entlang der Salzach zurück nach Eishöhle der Welt Abstecher an. Salzburg radelt. • Kelten- und Salinenstadt Gemütlicher geht es weiter zu den Stauseen der Pongauer Via Culinaria: (www.via-culinaria.com) Zu guter Letzt Hallein Salzachkraftwerke, an denen in den letzten Jahren schöne Rad- sei auch die kulinarische Vielfalt dieser Tour er- • Schloss & Zoo Hellbrunn wege entstanden sind. -
Cambridge University Press 978-1-108-44568-9 — Active Faults of the World Robert Yeats Index More Information
Cambridge University Press 978-1-108-44568-9 — Active Faults of the World Robert Yeats Index More Information Index Abancay Deflection, 201, 204–206, 223 Allmendinger, R. W., 206 Abant, Turkey, earthquake of 1957 Ms 7.0, 286 allochthonous terranes, 26 Abdrakhmatov, K. Y., 381, 383 Alpine fault, New Zealand, 482, 486, 489–490, 493 Abercrombie, R. E., 461, 464 Alps, 245, 249 Abers, G. A., 475–477 Alquist-Priolo Act, California, 75 Abidin, H. Z., 464 Altay Range, 384–387 Abiz, Iran, fault, 318 Alteriis, G., 251 Acambay graben, Mexico, 182 Altiplano Plateau, 190, 191, 200, 204, 205, 222 Acambay, Mexico, earthquake of 1912 Ms 6.7, 181 Altunel, E., 305, 322 Accra, Ghana, earthquake of 1939 M 6.4, 235 Altyn Tagh fault, 336, 355, 358, 360, 362, 364–366, accreted terrane, 3 378 Acocella, V., 234 Alvarado, P., 210, 214 active fault front, 408 Álvarez-Marrón, J. M., 219 Adamek, S., 170 Amaziahu, Dead Sea, fault, 297 Adams, J., 52, 66, 71–73, 87, 494 Ambraseys, N. N., 226, 229–231, 234, 259, 264, 275, Adria, 249, 250 277, 286, 288–290, 292, 296, 300, 301, 311, 321, Afar Triangle and triple junction, 226, 227, 231–233, 328, 334, 339, 341, 352, 353 237 Ammon, C. J., 464 Afghan (Helmand) block, 318 Amuri, New Zealand, earthquake of 1888 Mw 7–7.3, 486 Agadir, Morocco, earthquake of 1960 Ms 5.9, 243 Amurian Plate, 389, 399 Age of Enlightenment, 239 Anatolia Plate, 263, 268, 292, 293 Agua Blanca fault, Baja California, 107 Ancash, Peru, earthquake of 1946 M 6.3 to 6.9, 201 Aguilera, J., vii, 79, 138, 189 Ancón fault, Venezuela, 166 Airy, G. -
Liezen KUNDMACHUNG
Bezirkswahlbehörde Liezen KUNDMACHUNG Die Bezirkswahlbehörde Liezen für die Landwirtschaftskammerwahlen 2011 veröffentlicht gemäß § 33 der Landwirtschaftskammer-Wahlordnung 2005, LGBl. Nr. 90, idgF., nachstehend die Namen der von den Wählergruppen vorgeschlagenen Kandidaten für die Bezirkskammer für Land- und Forstwirtschaft Liezen Liste Steirischer Bauernbund STBB 1 1 Kettner Peter 1972 Bauer 8903 Lassing Fuchslucken 14 2 Schmalengruber Reinhard 1961 Bauer 8943 Aigen im Ennstal Vorberg 46 3 Hofer Christoph 1981 Bauer 8967 Haus Ruperting 17 4 Schörkmaier Christa 1964 Bäuerin 8786 Rottenmann Oppenberg 237 5 Stangl Karl 1972 Bauer 8921 Lainbach Mooslandl 65 6 Ruhsam Walter 1969 Bauer 8984 Pichl-Kainisch Pichl 21 7 Moser Franz 1977 Bauer 8962 Gröbming Loyhof 637 8 Gerharter Georg 1968 Bauer 8972 Ramsau am Dachstein Ramsau 32 9 Schachner Leo 1957 Bauer 8982 Tauplitz Wörschachwald 32 10 Pechhacker Peter 1962 Bauer 8933 Sankt Gallen Breitau 5 11 Winterer Martina 1973 Bäuerin 8961 Stein an der Enns Dörfl 11 12 Peer Daniel 1968 Bauer 8940 Weißenbach bei Liezen Schoagagasse 12 13 Stiegler Veronika 1955 Bäuerin 8966 Gössenberg Seewigtal 27 14 Zeiler Johannes 1971 Bauer 8960 Niederöblarn Zeissenberg 15 15 Wilfinger Eva 1978 Bäuerin 8911 Hall Hall 68 16 Zefferer Rudolf 1957 Bauer 8782 Treglwang Treglwang 38 17 Pitzer Michael 1984 Bauer 8966 Aich Assach-Oberdorf 37 18 Maderebner Harald 1974 Bauer 8960 Öblarn Schattenberg 96 19 Zwanzleitner Martha 1955 Bäuerin 8933 Sankt Gallen Hocherb 16 20 Siedler Alois 1970 Bauer 8911 Admont Aigen 50 21 Leitner -
JOURNAL Or GEOPHYSICAL RESEARCH, VOL. 90, NO. B5, PAGES 3589-3615, APRIL 10, 1985 and SOUTHERN PERUVIAN MARGINS of SOUTH AMERICA
JOURNAL or GEOPHYSICAL RESEARCH, VOL. 90, NO. B5, PAGES 3589-3615, APRIL 10, 1985 SEISMIC POTENTIAL FOR LARGE AND GREAT 1NTERPLATE EARTHQUAKES ALONG THE CHILEAN AND SOUTHERN PERUVIAN MARGINS OF SOUTH AMERICA: A QUAITITATIVE REAPPRAISAL l Stuart P. Nishenko Lamont-Doherty Geological Observatory of Columbia University Palisades, New York Abstract. The seismic potential of the al., 1978, 1979; Nishenko and McCann, 1981]. Chilean and southern Peruvian margins of South Seismic gaps have been defined as those segments America is reevaluated to delineate those areas along active convergent or transform plate bound or segments of the margin that may be expected to aries that have not experienced a repeat of a experience large or great interplaZe earthquakes large or great interplate earthquake for more within the next 20 years (1984-2034). Long-term than a few decades and thus are considered likely estimates of seismic potential (or the condi- sites for future large or great events. While tional probability of recurrence within a speci- these observations provide estimates as to the fied period of time) are based on (1) statistical location and maximum likely size of future earth analysis of historic repeat time data using quakes, they do not provide estimates to better Weibull distributions and (2) deterministic esti- than a few tens of years as to the time of occur mates of recurrence times based on the time- rence of future large shocks. The lack of more predictable model of earthquake recurrence. Both precise temporal estimates primarily reflects the methods emphasize the periodic nature of large absence of local recurrence time, source size and and great earthquake recurrence, and are compared plate velocity data in the definition of the with estimates of probability based on the categories of seismic potential. -
From Upper Triassic of the Northern Ca
STUDIA UNIVERSITATIS BABEŞ-BOLYAI, GEOLOGIA, XLVIII, 2, 2003, 101-111 HIRUNDOPORELLA DACHSTEINENSIS N. GEN., N. SP., A NEW PROBLEMATIC DASYCLADALE (GREEN ALGA) FROM THE UPPER TRIASSIC OF THE NORTHERN CALCAREOUS ALPS, AUSTRIA. FELIX SCHLAGINTWEIT1, HARALD LOBITZER2 & OSKAR EBLI3 ABSTRACT. A new problematic dasycladale is described as Hirundoporella dachsteinensis nov. gen., n. sp. from the Upper Triassic bedded Dachstein Limestone of Mount Dachstein, Austria. It is characterized by individualized phloiophorous laterals, open at the ends and secondary laterals of low number arising in the middle part of the primaries. Nothing is known about the obviously thin and poorly calcified main-axis and the overall arrangement of the primaries. The microfacies is represented by a wackestone composed to about 70 % of dismembered laterals of Hirundoporella dachsteinensis n. sp. Key Words: Calcareous Algae, Dasycladales, Upper Triassic, Norian-Rhaetian, Dachstein Limestone, Northern Calcareous Alps, Austria INTRODUCTION The Austroalpine Dachstein nappe with the Dachstein mountains is part of the Triassic shallow marine carbonate shelf that at its southern rim bordered the Tethys ocean with the adjacent deeper water Hallstatt realm (e.g. Haas et al., 1995, Mandl 2000). The Upper Triassic Dachstein-type platforms are widespread in the Mediterranean realm and even Japan (Kristan-Tollmann 1991). The Dachstein facies comprises reefs at the southern border, northward passing into back-reef and lagoonal deposits of the so-called “bedded Dachstein limestone” (e.g. Zankl 1971). The latter exhibits a typical cyclicity, the so-called “Lofer cyclothems” (layer A, B, C) studied by Fischer (1964). With respect to the reefal and near-reef facies, a more detailed differentiation has been established with typical assemblages of benthic foraminifera and dasycladales (Senowbari-Daryan & Schäfer, 1978, 1979; Wurm, 1982). -
Sources for Genealogical Research at the Austrian War Archives in Vienna (Kriegsarchiv Wien)
SOURCES FOR GENEALOGICAL RESEARCH AT THE AUSTRIAN WAR ARCHIVES IN VIENNA (KRIEGSARCHIV WIEN) by Christoph Tepperberg Director of the Kriegsarchiv 1 Table of contents 1. The Vienna War Archives and its relevance for genealogical research 1.1. A short history of the War Archives 1.2. Conditions for doing genealogical research at the Kriegsarchiv 2. Sources for genealogical research at the Kriegsarchiv 2. 1. Documents of the military administration and commands 2. 2. Personnel records, and records pertaining to personnel 2.2.1. Sources for research on military personnel of all ranks 2.2.2. Sources for research on commissioned officers and military officials 3. Using the Archives 3.1. Regulations for using personnel records 3.2. Visiting the Archives 3.3. Written inquiries 3.4. Professional researchers 4. Relevant publications 5. Sources for genealogical research in other archives and institutions 5.1. Sources for genealogical research in other departments of the Austrian State Archives 5.2. Sources for genealogical research in other Austrian archives 5.3. Sources for genealogical research in archives outside of Austria 5.3.1. The provinces of the Austro-Hungarian Monarchy and its “successor states” 5.3.2. Sources for genealogical research in the “successor states” 5.4. Additional points of contact and practical hints for genealogical research 2 1. The Vienna War Archives and its relevance for genealogical research 1.1. A short history of the War Archives Today’s Austrian Republic is a small country, but from 1526 to 1918 Austria was a great power, we can say: the United States of Middle and Southeastern Europe. -
Leisure Activities
2019 EN IN DER REGION Horseback riding Friday Saturday Pleasure of climbing difficulty level III • Afternoon hack for advanced, hack to Halseralm Bergführerbüro - Mountain guide office Ramsau, or Sonnenalm with a break. Reiterparadies Farmers’ and handicraft market Church service tel. 0664 5220080. Zechmannhof stables, tel. 81476. (5th July - 27th September) Catholic church Ramsau-Kulm. Mass: 5.30 pm. • Adventure hike, Alpincenter Dachstein, Schildle- 2 to 4.30 pm, Ramsau Zentrum, in any weather. Tourism Office Ramsau am Dachstein hen, tel. 81430. Day hack Ramsau 372 Leisure Hiking in the Dachstein region 10 am. Up to the die Alm or down to the Enns valley. 8972 Ramsau am Dachstein Nordic Walking lessons for advanced On request atAlpincenter Dachstein, Schildlehen, Reiterhof Brandstätter stables, tel. 81796. Important phone numbers Österreich 10 am to 12 pm. Cross-country school fit & fun, tel. 81430. Tel: +43 3687 818338 activities Glacier Basic Course Fax: +43 3687 81085 tel. 0664 2310231. Country code Austria: + 43 In the footsteps of the Mountain rescuers Bergführerbüro - Mountain guide office Ramsau, [email protected] . www.ramsau.com Area code Ramsau am Dachstein: (0) 3687 Weekly activity programme for your holidays Paragliding taster lessons 31st May to 27th September, guided hike to the original tel. 0664 5220080. in Ramsau am Dachstein Alpincenter Dachstein, Schildlehen, tel. 81430. sets of the German TV Show „Die Bergretter‘ (The Mountain rescue: 140 Mountain rescuers). 10 am at the Bergretter Zentrale (in Paragliding (according to weather condition) European emergency number: 112 Running and Nordic walking Ramsau-Ort), walk to Pernerhof farm (Emilies Hof), with Taster lesson, Flugschule Aufwind, beside BP petrol Ambulance: 144 7 pm at Kobaldhof. -
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. -
Geomorphic Evolution of Dehra Dun, NW Himalaya: Tectonics and Climatic Coupling
Geomorphology 266 (2016) 20–32 Contents lists available at ScienceDirect Geomorphology journal homepage: www.elsevier.com/locate/geomorph Geomorphic evolution of Dehra Dun, NW Himalaya: Tectonics and climatic coupling Swati Sinha, Rajiv Sinha ⁎ Department of Earth Sciences, Indian Institute of Technology Kanpur, Kanpur 208016, India article info abstract Article history: The Dehra Dun is a good example of a piggyback basin formed from the growth of the Siwalik hills. Two large riv- Received 22 November 2015 ers, the Ganga and the Yamuna, and their tributaries deposit a significant part of their sediment load in the Dun Received in revised form 1 May 2016 before they enter the Gangetic plains. This work documents the geomorphic complexities and landform evolu- Accepted 2 May 2016 tion of the Dehra Dun through geomorphic mapping and chronostratigraphic investigation of the incised fan sec- Available online 6 May 2016 tions. Lesser Himalayan hills, inner and outer dissected hills, isolated hills, proximal fan, distal fan, dip slope unit, fl fi Keywords: oodplains, and terraces are the major geomorphic units identi ed in the area. Isolated hills of fan material (IHF), fi Intermontane valleys proximal fan (PF), and distal fan (DF) are identi ed as fan surfaces from north to south of the valley. The OSL Himalayan foreland based chronology of the fan sediments suggests that the IHF is the oldest fan consisting of debris flow deposits Valley fills with a maximum age of ~43 ka coinciding with the precipitation minima. The proximal fan consisting of sheet Fan deposits flow deposits represents the second phase of aggradation between 34 and 21 ka caused by shifting of deposition locus downstream triggered by high sediment supply that exceeded the transport capacity. -
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.