Assessment of Flood Monitoring and Forecasting in the Danube River Basin
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Fish Distribution and Spatial Structure of Fish Assemblages in the Danube River
Fish distribution and spatial structure of fish assemblages in the Danube River Zoltán Szalóky PhD Thesis Eötvös Loránd University Faculty of Science Doctoral School of Environmental Sciences, Environmental Biology Program Head of Doctoral School: Dr. Imre Jánosi, DSc, university professor Head of Doctoral Program: Dr. Éva Ács, DSc, scientific advisor Supervisor: Dr. Tibor Erős, PhD, senior researcher MTA Centre for Ecological Research, Balaton Limnological Institute Made: MTA Centre for Ecological Research, Danube Research Institute Budapest, 2017 Introduction Sampling the biota in the main channel of large rivers presents a continuing challenge for freshwater ecologists. While our knowledge of the organization of shoreline fish assemblages and their representative sampling are increasing (e.g. Jurajda et al., 2001; Erős et al., 2008), information about the composition and spatial and temporal distribution of fishes in deep channel habitats is still relatively sporadic (Dettmers et al., 2001). Inferences about how main channel habitats contribute to the bioassessment of large rivers compared with shoreline monitoring data should also be more precisely developed (de Leeuw et al., 2007; Flotemersch et al., 2011). However, detailed quantitative studies are restricted to only a very few large rivers even in the relatively well studied temperate large river systems of Europe and North- America (see e.g. Wolter and Freyhof, 2004; Gutreuter et al., 2009; Ridenour et al., 2009). It would be thus important to develop deep channel fish monitoring methods for providing data for both basic research and the conservation management of riverine fish species. Matching habitat typology and ecological assemblage types can be useful in environmental management and conservation (Dufrene and Legendre, 1997; Heino et al., 2003). -
The South Slav Policies of the Habsburg Monarchy
University of South Florida Scholar Commons Graduate Theses and Dissertations Graduate School January 2012 Nationalitaetenrecht: The outhS Slav Policies of the Habsburg Monarchy Sean Krummerich University of South Florida, [email protected] Follow this and additional works at: http://scholarcommons.usf.edu/etd Part of the American Studies Commons, Ethnic Studies Commons, and the European History Commons Scholar Commons Citation Krummerich, Sean, "Nationalitaetenrecht: The outhS Slav Policies of the Habsburg Monarchy" (2012). Graduate Theses and Dissertations. http://scholarcommons.usf.edu/etd/4111 This Thesis is brought to you for free and open access by the Graduate School at Scholar Commons. It has been accepted for inclusion in Graduate Theses and Dissertations by an authorized administrator of Scholar Commons. For more information, please contact [email protected]. Nationalitätenrecht: The South Slav Policies of the Habsburg Monarchy by Sean Krummerich A thesis submitted in partial fulfillment of the requirements for the degree of Master of Arts Department of History College of Arts & Sciences University of South Florida Major Professor, Graydon A. Tunstall, Ph.D. Kees Botterbloem, Ph.D. Giovanna Benadusi, Ph.D. Date of Approval: July 6, 2012 Keywords – Austria, Hungary, Serb, Croat, Slovene Copyright © 2012, Sean Krummerich Dedication For all that they have done to inspire me to new heights, I dedicate this work to my wife Amanda, and my son, John Michael. Acknowledgments This study would not have been possible without the guidance and support of a number of people. My thanks go to Graydon Tunstall and Kees Boterbloem, for their assistance in locating sources, and for their helpful feedback which served to strengthen this paper immensely. -
Landeszentrale Für Politische Bildung Baden-Württemberg, Director: Lothar Frick 6Th Fully Revised Edition, Stuttgart 2008
BADEN-WÜRTTEMBERG A Portrait of the German Southwest 6th fully revised edition 2008 Publishing details Reinhold Weber and Iris Häuser (editors): Baden-Württemberg – A Portrait of the German Southwest, published by the Landeszentrale für politische Bildung Baden-Württemberg, Director: Lothar Frick 6th fully revised edition, Stuttgart 2008. Stafflenbergstraße 38 Co-authors: 70184 Stuttgart Hans-Georg Wehling www.lpb-bw.de Dorothea Urban Please send orders to: Konrad Pflug Fax: +49 (0)711 / 164099-77 Oliver Turecek [email protected] Editorial deadline: 1 July, 2008 Design: Studio für Mediendesign, Rottenburg am Neckar, Many thanks to: www.8421medien.de Printed by: PFITZER Druck und Medien e. K., Renningen, www.pfitzer.de Landesvermessungsamt Title photo: Manfred Grohe, Kirchentellinsfurt Baden-Württemberg Translation: proverb oHG, Stuttgart, www.proverb.de EDITORIAL Baden-Württemberg is an international state – The publication is intended for a broad pub- in many respects: it has mutual political, lic: schoolchildren, trainees and students, em- economic and cultural ties to various regions ployed persons, people involved in society and around the world. Millions of guests visit our politics, visitors and guests to our state – in state every year – schoolchildren, students, short, for anyone interested in Baden-Würt- businessmen, scientists, journalists and numer- temberg looking for concise, reliable informa- ous tourists. A key job of the State Agency for tion on the southwest of Germany. Civic Education (Landeszentrale für politische Bildung Baden-Württemberg, LpB) is to inform Our thanks go out to everyone who has made people about the history of as well as the poli- a special contribution to ensuring that this tics and society in Baden-Württemberg. -
Rivers and Lakes in Serbia
NATIONAL TOURISM ORGANISATION OF SERBIA Čika Ljubina 8, 11000 Belgrade Phone: +381 11 6557 100 Rivers and Lakes Fax: +381 11 2626 767 E-mail: [email protected] www.serbia.travel Tourist Information Centre and Souvenir Shop Tel : +381 11 6557 127 in Serbia E-mail: [email protected] NATIONAL TOURISM ORGANISATION OF SERBIA www.serbia.travel Rivers and Lakes in Serbia PALIĆ LAKE BELA CRKVA LAKES LAKE OF BOR SILVER LAKE GAZIVODE LAKE VLASINA LAKE LAKES OF THE UVAC RIVER LIM RIVER DRINA RIVER SAVA RIVER ADA CIGANLIJA LAKE BELGRADE DANUBE RIVER TIMOK RIVER NIŠAVA RIVER IBAR RIVER WESTERN MORAVA RIVER SOUTHERN MORAVA RIVER GREAT MORAVA RIVER TISA RIVER MORE RIVERS AND LAKES International Border Monastery Provincial Border UNESKO Cultural Site Settlement Signs Castle, Medieval Town Archeological Site Rivers and Lakes Roman Emperors Route Highway (pay toll, enterance) Spa, Air Spa One-lane Highway Rural tourism Regional Road Rafting International Border Crossing Fishing Area Airport Camp Tourist Port Bicycle trail “A river could be an ocean, if it doubled up – it has in itself so much enormous, eternal water ...” Miroslav Antić - serbian poet Photo-poetry on the rivers and lakes of Serbia There is a poetic image saying that the wide lowland of The famous Viennese waltz The Blue Danube by Johann Vojvodina in the north of Serbia reminds us of a sea during Baptist Strauss, Jr. is known to have been composed exactly the night, under the splendor of the stars. There really used to on his journey down the Danube, the river that connects 10 be the Pannonian Sea, but had flowed away a long time ago. -
Treating Two 18Th Century Maps of the Danube in Association with Google-Provided Imagery
ON THE DIGITAL REVIVAL OF HISTORIC CARTOGRAPHY: TREATING TWO 18TH CENTURY MAPS OF THE DANUBE IN ASSOCIATION WITH GOOGLE-PROVIDED IMAGERY Evangelos Livieratos Angeliki Tsorlini Maria Pazarli [email protected] Chrysoula Boutoura Myron Myridis Aristotle University of Thessaloniki Faculty of Surveying Engineering University Campus, Box 497 GRE - 541 24 Thessaloniki, Greece Abstract The great navigable Danube River (known as the Istros River to the Ancient Greeks and as one of the crucial ends of the Roman Empire northern territories) is an emblematic fluvial feature of the overall European historic and cultural heritage in the large. Originating in the German Black Forest as two small rivers (Brigach and Breg) converging at the town of Donaueschingen, Danube is flowing for almost 2850 km mainly eastwards, passing through ten states (Germany, Austria, Slovakia, Hungary, Croatia, Serbia, Romania, Bulgaria, Moldova and Ukraine) and four European capitals (Vienna, Bratislava, Budapest and Belgrade) with embouchure in the west coasts of the Black Sea via the Danube Delta, mainly in Romania. Danube played a profound role in the European political, social, economic and cultural history influencing in a multifold manner the heritage of many European nations, some of those without even a physical connection with the River, as it is the case of the Greeks, to whom the Danube is a reference to their own 18th century Enlightenment movement. Due to Danube’s important role in History, the extensive emphasis to its cartographic depiction was obviously a conditio sine qua non especially in the 17th and 18th century European cartography. In this paper, taking advantage of the modern digital technologies as applied in the recently established domain of cartographic heritage, two important and historically significant 18th century maps of the Danube are comparatively discussed in view also to the reference possibilities available today in relevant studies by the digital maps offered by powerful providers as e.g. -
M1928 1945–1950
M1928 RECORDS OF THE GERMAN EXTERNAL ASSETS BRANCH OF THE U.S. ALLIED COMMISSION FOR AUSTRIA (USACA) SECTION, 1945–1950 Matthew Olsen prepared the Introduction and arranged these records for microfilming. National Archives and Records Administration Washington, DC 2003 INTRODUCTION On the 132 rolls of this microfilm publication, M1928, are reproduced reports on businesses with German affiliations and information on the organization and operations of the German External Assets Branch of the United States Element, Allied Commission for Austria (USACA) Section, 1945–1950. These records are part of the Records of United States Occupation Headquarters, World War II, Record Group (RG) 260. Background The U.S. Allied Commission for Austria (USACA) Section was responsible for civil affairs and military government administration in the American section (U.S. Zone) of occupied Austria, including the U.S. sector of Vienna. USACA Section constituted the U.S. Element of the Allied Commission for Austria. The four-power occupation administration was established by a U.S., British, French, and Soviet agreement signed July 4, 1945. It was organized concurrently with the establishment of Headquarters, United States Forces Austria (HQ USFA) on July 5, 1945, as a component of the U.S. Forces, European Theater (USFET). The single position of USFA Commanding General and U.S. High Commissioner for Austria was held by Gen. Mark Clark from July 5, 1945, to May 16, 1947, and by Lt. Gen. Geoffrey Keyes from May 17, 1947, to September 19, 1950. USACA Section was abolished following transfer of the U.S. occupation government from military to civilian authority. -
Paleochannel Evolution of the Leitha River (Eastern Austria) – a Bird’S Eye View A
Geophysical Research Abstracts, Vol. 8, 08976, 2006 SRef-ID: 1607-7962/gra/EGU06-A-08976 © European Geosciences Union 2006 Paleochannel evolution of the Leitha river (eastern Austria) – A bird’s eye view A. Zámolyi (1), E. Draganits (2), M. Doneus (3), K. Decker (1), Martin Fera (3) (1) Department of Geodynamics and Sedimentology, Structural Processes Group, University of Vienna, Austria, *[email protected] (2) Institute for Engineering Geology, Vienna University of Technology, Austria (3) Department for Prehistory and Early History, University of Vienna, Austria The Leitha river is an important tributary to the Danube in eastern Austria. It is formed by the Schwarza river, originating in the Northern Calcareous Alps, and the Pitten river, coming from the Lower Austroalpine unit of the Wechsel area. In contrast to the general trend of the rivers in the southern Vienna Basin towards the NNE di- rectly towards with the Danube, the Leitha river makes an abrupt turn towards the East at Götzendorf. At Rohrau the next turn follows towards the SE and the Leitha runs through the gate of Carnuntum onto the little Hungarian Plain. The confluence with the Moson-Danube lies farther to the East at Mosonmagyaróvár. The geometry of paleochannels of the Leitha river was investigated in the river section between the confluence of Pitten and Schwarza (forming the Leitha) near Lanzenkirchen and Bruck/Leitha by paleochannel digitization using infrared and black and white aerial photography. This study is part of an archaeological project investigating patterns of prehistoric settlements in this region. The section of the Lei- tha river between Lanzenkirchen and Bruck/Leitha is especially suitable for the study of dynamic fluvial processes and the comparison between former natural river behav- ior and present regulated riverbed, because of the transition from relatively high to low river slopes in this section. -
Resolving the Variscan Evolution of the Moldanubian Sector of The
Journal of Geosciences, 52 (2007), 9–28 DOI: 10.3190/jgeosci.005 Original paper Resolving the Variscan evolution of the Moldanubian sector of the Bohemian Massif: the significance of the Bavarian and the Moravo–Moldanubian tectonometamorphic phases Fritz FINGER1*, Axel GERDEs2, Vojtěch JANOušEk3, Miloš RENé4, Gudrun RIEGlER1 1University of Salzburg, Division of Mineralogy, Hellbrunnerstraße 34, A-5020 Salzburg, Austria; [email protected] 2University of Frankfurt, Institute of Geoscience, Senckenberganlage 28, D-60054 Frankfurt, Germany 3Czech Geological Survey, Klárov 3, 118 21 Prague 1, Czech Republic 4Academy of Sciences, Institute of Rock Structure and Mechanics, V Holešovičkách 41, 182 09 Prague 8, Czech Republic *Corresponding author The Variscan evolution of the Moldanubian sector in the Bohemian Massif consists of at least two distinct tectonome- tamorphic phases: the Moravo–Moldanubian Phase (345–330 Ma) and the Bavarian Phase (330–315 Ma). The Mora- vo–Moldanubian Phase involved the overthrusting of the Moldanubian over the Moravian Zone, a process which may have followed the subduction of an intervening oceanic domain (a part of the Rheiic Ocean) beneath a Moldanubian (Armorican) active continental margin. The Moravo–Moldanubian Phase also involved the exhumation of the HP–HT rocks of the Gföhl Unit into the Moldanubian middle crust, represented by the Monotonous and Variegated series. The tectonic emplacement of the HP–HT rocks was accompanied by intrusions of distinct magnesio-potassic granitoid melts (the 335–338 Ma old Durbachite plutons), which contain components from a strongly enriched lithospheric mantle source. Two parallel belts of HP–HT rocks associated with Durbachite intrusions can be distinguished, a western one at the Teplá–Barrandian and an eastern one close to the Moravian boundary. -
Reader – the International Waterway of the Danube
READER – THE INTERNATIONAL WATERWAY OF THE DANUBE Extract of relevant passages from the „Manual of Danube Navigation”, via donau (2019) and of other relevant sources. Pictures: viadonau in Manual on Danube Navigation (2019), p 79, 106 Danube navigation at a glance 15 Source: viadonau/Thomas Bierbaumer viadonau/Thomas Source: Motor cargo vessel entering the lock at Ybbs-Persenbeug The capacity of the Danube waterway is a key factor within the inland navigation system. It is determined above all by the nautical conditions (meaning the navigability of the waterway with an economically viable draught loaded of the vessels over the course of the year); these factors directly influence the loading capacities of the vessel types in operation. Good nautical conditions and suitable, ongoing maintenance of the waterway infrastructure allow shipping companies to offer reliable and competitive transport services. This is a significant precondition for the sustained integration of green inland navigation within the logistical concepts of a modern economy. Danube ports Inland ports enable the combination of the transport modes waterway, road and rail. Working in multimodal logistics chains, rail and road act as partners to water- way transport by enabling the pre- and end-haulage of inland navigation transports. The ports are the important interfaces in this regard. Over recent decades, the Danube ports have underwent profound transformation from conventional inland ports to modern logistics hubs. In addition to basic ser- vices such as transhipment and storage, ports offer an extensive range of logistics services, including commissioning, distribution, project logistics and many more. As production sites as well as cargo collection and distribution centers, they are extremely well integrated into regional economies and contribute substantially to economic growth and the creation of employment. -
Flood Risk Management Plan for the Danube River Basin District Is Based on Information Received from the ICPDR Contracting Parties by 10 November 2015
/ / / / / / / / / / / / / н ϊ ρ κ Y Flood Risk / / / / a v o Management Plan d l uj //// Crna o pб Gor M // C a //// / // Ro // a mân я / in ia //// ρu for the Danube River Basin District Бълѕѕ v o g e c r e H i a n nd //// Ös s schla terreic o ut h //// B e Č / D esk // // á r / / ep a // ub / lik k / a / s / /// t / a / Sl v / ov r / en / sk H / o / / / /// / M // agyar ija н ors n ϊ zág //// Slove ρ κ Y / / / / a v o d l o M / / / / я u ρ ѕ л ъ Б / / / / a i n â m o R / / / / a r o G a n agyarorsz r /// M ág //// C / S ko lov / s en / n ija / e //// / ov H Sl rva j // tska u // //// б ka Bosn Cp bli a i H //// pu ercegovina re ská / Če h /// rreic / Öste land /// ////// eutsch D Disclaimer This Flood Risk Management Plan for the Danube River Basin District is based on information received from the ICPDR Contracting Parties by 10 November 2015. Sources other than the competent authorities have been clearly identified in the Plan. A more detailed level of information is presented in the national Flood Risk Management Plans. Hence, the Flood Risk Management Plan for the Danube River Basin District should be read and interpreted in conjunction with the national Flood Risk Management Plans. The data in this report has been dealt with, and is presented, to the best of our knowledge. Nevertheless inconsistencies cannot be ruled out. -
Geochemical Characteristics of the Late Proterozoic Spitz Granodiorite
Journal of Geosciences, 63 (2018), 345–362 DOI: 10.3190/jgeosci.271 Original paper Geochemical characteristics of the Late Proterozoic Spitz granodiorite gneiss in the Drosendorf Unit (southern Bohemian Massif, Austria) and implications for regional tectonic interpretations Martin LINDNER*, Fritz FINGER Department of Chemistry and Physics of Materials, University of Salzburg, Jakob-Haringer-Straße 2a, 5020 Salzburg, Austria; [email protected] * Corresponding author The Spitz Gneiss, located near the Danube in the southern sector of the Variscan Bohemian Massif, represents a ~13 km² large Late Proterozoic Bt ± Hbl bearing orthogneiss body in the Lower Austrian Drosendorf Unit (Moldanubian Zone). Its formation age (U–Pb zircon) has been determined previously as 614 ± 10 Ma. Based on 21 new geochemical analy- ses, the Spitz Gneiss can be described as a granodioritic I-type rock (64–71 wt. % SiO2) with medium-K composition (1.1–3.2 wt. % K2O) and elevated Na2O (4.1–5.6 wt. %). Compared to average granodiorite, the Spitz Gneiss is slightly depleted in Large-Ion Lithophile (LIL) elements (Rb 46–97 ppm, Cs 0.95–1.5 ppm), Sr (248–492 ppm), Nb (6–10 ppm), Th (3–10 ppm), the LREE (e.g. La 10–30 ppm), Y (6–19 ppm) and first row transitional metals (e.g. Cr 10–37 ppm). The Zr content (102–175 ppm) is close to average granodiorite. The major- and trace-element signature of the Spitz Gneiss is similar to some Late Proterozoic granodiorite suites in the Moravo–Silesian Unit (e.g. the Passendorf-Neudegg suite in the Thaya Batholith). -
JAHRBUCH DER GEOLOGISCHEN BUNDESANSTALT Jb
©Geol. Bundesanstalt, Wien; download unter www.geologie.ac.at JAHRBUCH DER GEOLOGISCHEN BUNDESANSTALT Jb. Geol. B.-A. ISSN 0016–7800 Band 141 Heft 4 S. 377–394 Wien, Dezember 1999 Evolution of the SE Bohemian Massif Based on Geochronological Data – A Review URS KLÖTZLI, WOLFGANG FRANK, SUSANNA SCHARBERT & MARTIN THÖNI*) 7 Text-Figures and 1 Table Bohemian Massif Moldanubian zone Moravian zone European Variscides Österreichische Karte Evolution Blätter 1–9, 12–22, 29–38, 51–56 Geochronology Contents Zusammenfassung ...................................................................................................... 377 Abstract ................................................................................................................. 378 1. Introduction ............................................................................................................. 378 2. Geological Setting ....................................................................................................... 378 2.1. Moravian Zone ...................................................................................................... 379 2.2. Moldanubian Zone .................................................................................................. 379 2.3. South Bohemian Pluton ............................................................................................. 381 3. Pre-Variscan Geochronology ............................................................................................ 382 3.1. Information from Detrital and Inherited