Trace Element Contamination in the Arms of the Danube Delta (Romania/Ukraine): Current State of Knowledge and Future Needs Davide A.L
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Map of the European Inland Waterway Network – Carte Du Réseau Européen Des Voies Navigables – Карта Европейской Сети Внутренних Водных Путей
Map of the European Inland Waterway Network – Carte du réseau européen des voies navigables – Карта европейской сети внутренних водных путей Emden Berlin-Spandauer Schiahrtskanal 1 Берлин-Шпандауэр шиффартс канал 5.17 Delfzijl Эмден 2.50 Arkhangelsk Делфзейл Архангельск Untere Havel Wasserstraße 2 Унтере Хафель водный путь r e Teltowkanal 3 Тельтов-канал 4.25 d - O Leeuwarden 4.50 2.00 Леуварден Potsdamer Havel 4 Потсдамер Хафель 6.80 Groningen Harlingen Гронинген Харлинген 3.20 - 5.45 5.29-8.49 1.50 2.75 р водный п 1.40 -Оде . Papenburg 4.50 El ель r Wasserstr. Kemi Папенбург 2.50 be аф Ode 4.25 нканал Х vel- Кеми те Ha 2.50 юс 4.25 Luleå Belomorsk K. К Den Helder Küsten 1.65 4.54 Лулео Беломорск Хелдер 7.30 3.00 IV 1.60 3.20 1.80 E m О - S s Havel K. 3.60 eve Solikamsk д rn a е ja NE T HERLANDS Э р D Соликамск м Хафель-К. vin с a ная Б Север Дви 1 III Berlin е на 2 4.50 л IV B 5.00 1.90 о N O R T H S E A Meppel Берлин e м 3.25 l 11.00 Меппел o о - 3.50 m р 1.30 IV О с а 2 2 де - o к 4.30 р- прее во r 5.00 б Ш дн s о 5.00 3.50 ь 2.00 Sp ый k -Б 3.00 3.25 4.00 л ree- er Was п o а Э IV 3 Od ser . -
WWF Position “Bystroye Canal” / Danube-Black Sea Deep
WWF Position May 2009 “Bystroye Canal” / Danube-Black Sea Deep Navigation Channel Since 2004, the Ukrainian government has been constructing a canal in the Danube Delta referred to in the official documentation as the Danube-Black Sea Deep Navigation Channel, or “Bystroye canal” as it widely known as an alternative to the Sulina Channel on Romanian territory. The project has been carried out with a number of breaches of international commitments. Local and international stakeholders and environmental organisations have been highly concerned about its likely negative environmental impacts on the unique species and habitats of the Delta, which is protected under the UNESCO Man and Biosphere Programme ( for chronology of events please, see www.panda.org/dcpo). The decision to construct the canal has been based neither on solid socio- economic and environmental analysis nor on proper assessment of alternatives WWF therefore calls for a halt to all further works on a deep sea canal along the Bystroye arm. WWF recommends joint operation of the existing Sulina Channel by Romania and Ukraine as the most economically and environmentally viable option. Should the Ukrainian government not give up its plan to construct a navigation channel on national territory, WWF proposes the careful consideration of alternatives outside the Danube Delta Biosphere Reserve. Project poses severe threat to Danube Delta biodiversity Further works on a deep sea canal along the Bystroye branch presents a severe threat to the Danube Delta’s biodiversity as the canal cuts through the heart of the Ukrainian Danube Delta Biosphere Reserve – an environmentally sensitive area protected by several international agreements. -
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. -
Romania: Danube Delta Integrated Sustainable Development Strategy
Romania: Danube Delta Integrated Sustainable Development Strategy About the Danube Delta Region The Danube Delta is one of the continent’s most valuable habitats for specific delta wildlife and biodiversity. Established as a UNESCO Biosphere Reserve and a Ramsar site in 1990, it is the Europe’s second largest delta, and the best preserved of European deltas. The most significant physical and ecological feature of the Danube Delta is its vast expanse of wetlands, including freshwater marsh, lakes and ponds, streams and channels. With an area of 3,446 km2, is the world’s largest wetland. Only 9% of the area is permanently above water. The Delta hosts extraordinary biodiversity and provides important environmental services. It is the home of over 1,200 varieties of plants, 300 species of birds, as well as 45 freshwater fish species in its numerous lakes and marshes. There are 16 strictly protected areas in the delta where no economic activities are allowed, and areas for ecological rehabilitation and buffer zones between economical areas where tourist activities are permitted as long as the environment is protected. Dual Challenge in Developing the Danube Delta A dual challenge for the sustainable development of the Danube Delta is the conservation of its ecological assets and improvement of the quality of life for its residents. The Danube Delta is the largest remaining natural delta in Europe and one of the largest in the world. It is also the only river that is entirely contained within a Biosphere Reserve. It is important to conserve all of its ecological assets. 1 Danube Delta is perhaps one of the least inhabited regions of temperate Europe, with only about 10,000 people in one town (Sulina) and about 20 scattered villages. -
Manual on Border Controls Along the Danube and Its Navigable Tributaries
EU Strategy for the Danube Region Priority Area 1a – To improve mobility and multimodality: Inland waterways Practical manual on border controls along the Danube and its navigable tributaries Author(s): Milica Gvozdic (viadonau) Simon Hartl (viadonau) Katja Rosner (viadonau) Version (date): 31.08.2015 1 General information .................................................................................................................. 4 2 How to use this manual? .......................................................................................................... 5 3 Geographic scope .................................................................................................................... 5 4 Hungary ................................................................................................................................... 7 4.1 General information on border controls ................................................................................... 7 4.1.1 Control process ................................................................................................................... 8 4.1.2 Control forms ..................................................................................................................... 10 4.1.3 Additional information ....................................................................................................... 21 4.2 Information on specific border control points ......................................................................... 22 4.2.1 Mohács ............................................................................................................................. -
On the Geomorphologic and Geologic Evolution of The
N. Panin - On the Geomorphologicand Geologicevolution of the Nver Danube- Black Sea lnteractionZone ONTHE GEOMORPHOLOGIC AND GEOLOGIC EVOLUTION OF THE RIVERDANUBE . BLACKSEA INTERACTION ZONE NicolaePRxttrt NationalInstitute of MarineGeology and Geo-ecology- GEoEcoMAR 23-25,D. OnciulStr., 70318 Bucharest, Tel/Fax: +fi-1-252.25.94, E-mail: [email protected] Abstract. The presentpaper aims at describingof the evolutionof the mouthzones of three main distributariesof the DanubeDelta system:the northernbranch - Chilia,a medianone - Sulinaand a southernbranch - St. George(Sf.Gheorghe). These main distributaries areresponsible for the formationand the developmentof differentstages of the DanubeDelta. The descriptionis basedon the complex studyof the.entireDanube Delta edifice by aerophotogrammetric,geomorphologic, sedimentologic-geologic, biostratigraphic means, as ''C wellas by datationof deltaicdeposits. The mainstages of developmentthrough which the DanubeDelta reached the presentday aspectinclude:(1)theDanubeGulf andthe"DanubeBlockedDelta"--12-1 1 k.yr.B.P.; (2)lnitial Letea-CaraormanSpit, 11,700-9,800 yr.B. P.; (3) St.GeorgeI Deita,9,000-7,200 yr. B. P.; (4) SulinaDelta, 7 ,2OO-2,000 yr. B P.;(5)St, George ll Deltaand ChiliaDelta, 2,800 yr.B.P.-present;(6) SecondaryCosna-Sinoie Delta, 3,550-2,500 yr B.P. Detaileddescription of the succesivephases of developmentof the mentionedstages is given. 'oC Key words: geomorphologicand geologicevolution, deltaic deposits, phases of development, datation,Danube Delta system. INTRODUCTION THE "BLOCKEDDANUBE DELTA'' The river-sea interaction zones have very ln the period12-11 k.y. BP, when the level of complexdynamic, depositional, biogeo-chemical the Black Sea had reachedthe present level or, and eco-structuralcharacteristics. Geomorpho- probably,had even exceededit with few meters, logicallythese zones are representedmostly by the present area of the Danube Delta was estuariesand deltas. -
Danube Navigation
pistribüted t0 the C0 u n ci1 C. 4 4 4 (a) M. 164 (a). 1 9 2 5 . VIII. and the Members of the League.] v ' — G e n e v a , August 20th, 1 9 2 5 . LEAGUE OF NATIONS REPORT ON DANUBE NAVIGATION SUBMITTED TO THE ADVISORY AND TECHNICAL COMMITTEE FOR COMMUNICATIONS AND TRANSIT OF THE LEAGUE OF NATIONS BY WALKER D. HINES (with the aid of Major Brehon Somervell) TABLE OF CONTENTS. Part 1. P ag e I Introduction ............................................................................................................................................. 11 II, P a s t a n d P r e s e n t U t i l i s a t i o n o f t h e R i v e r .......................................................................................................... 11 Freight traffic ..................................................................................................................................... 11 Total for 1911, 1923, 1924. Increase expected in 1925. Exports, imports and internal traffic of riparian States. Traffic by flag, 1923 and 1924. Comparison with traffic on Rhine Passenger traffic ..................................................................................................................................... 14 III. T h e R i v e r F l e e t s , t h e i r N a t i o n a l i t y a n d C a p a c i t y ................................................................................ 15 Pre-war situation. Present situation. Changes brought about by the war. Present Danube Fleet by flag. Introduction of self-propelled barges. Greater division of shipping interests. Co-operation among navigation companies. IV. S c h e m e o f A n a l y s i s ................................................................................................................................................................................. 16 V. T h e G e n e r a l C h a r a c t e r i s t i c s o f D a n u b e T r a f f i c .......................................................................................... -
Meeting Report Ima 2010 – Budapest
MEETING REPORT IMA 2010 – BUDAPEST Maryse Ohnenstetter relaxes at an IMA gala dinner with husband Daniel at the end of her term of offi ce as IMA Secretary The conference buildings on the campus of Eötvös Loránd University The 20th General Meeting of the International Mineralogical Association took place between 21 and 27 August in Budapest, Hungary. It was a great success, and I and everyone I spoke to seem to have thoroughly enjoyed themselves, not least because of the high standard of many of the presentations. The IMA General Meetings take place in different, interesting cities every four years, and the organizers always make a genuine effort to be truly international. These meetings have a feel that is different, more characterful, than many of the other big meet- Attila Demeny and Amir Mortezo in ings I’ve attended. IMA 2010 was the biggest mineralogical meeting discussion during a poster session ever, with about 1700 participants from 74 countries. The organiza- tion was headed by Tamás Weiszburg from Hungary (Chairman of the International Organizing Committee), Ekkehart Tillmanns from Austria (General Chairman and Chairman of the Scientifi c Programme Committee) and Dana Pop from Romania (Secretary General). They orchestrated a consortium representing the mineralogical or geolog- ical societies of Austria, Bulgaria, Croatia, Czech Republic, Hungary, Poland, Romania, Serbia, Slovakia and Slovenia. That in itself was a considerable feat of organization, and it’s good to see that mineralogy is thriving in countries that until not long ago had the misfortune to be behind the Iron Curtain. Austro-Hungarian The meeting took place in two huge, comfortable, modern buildings of grandeur the Eötvös Loránd University, on the west bank of the Danube (Duna in Hungarian). -
A New Paradigm for Shipping on the Danube River in Terms of Turkey Asst.Prof.Dr.Gökçe Çiçek CEYHUN1
Business Management Dynamics Vol.3, No.11, Nov 2014, pp.01-08 A New Paradigm for Shipping on the Danube River in Terms of Turkey Asst.Prof.Dr.Gökçe Çiçek CEYHUN1 Abstract Key words: Danube River, Cost factor is important in terms of both profitability and competition in transportation, shipping trade, transportation sector as other segments. Particularly in the crisis periods, ceramic different aspects needs bring with new pursuits and bring forward some applications that turn the crisis into the opportunities. This study offers new sights in terms of container shipping for producing companies and merchants. The main subject of this study is analyzing transportation on Danube River in Available online terms of Turkey. There are various studies that offer river transport’s spirits for www.bmdynamics.com container shipping in the world. Among all the rivers which nourish the Black ISSN: 2047-7031 Sea the Danube River is taking place by its extension 2783 km. This huge area is well known not only as a popular river, but also as a transportation territory for some countries. In this manner the basic objective of this study is to handle Danube River -which is one of the superiorities of Turkey caused by location- from the point of it’s economical advantages in transportation. In order to address this question, transportation on the Danube River and Turkey’s trade connection for the river have been analyzed in terms of container shipping. Then the world’s third ceramic exporter country-Turkey’s- ceramic trade options by container shipping on Danube River has been evaluated. -
Evolution of Chilia Lobes of the Danube Delta
G Model ANCENE-47; No. of Pages 6 Anthropocene xxx (2014) xxx–xxx Contents lists available at ScienceDirect Anthropocene jo urnal homepage: www.elsevier.com/locate/ancene Short communication Evolution of Chilia lobes of the Danube delta: Reorganization of deltaic processes under cultural pressures a,b, c, Florin Filip *, Liviu Giosan ** a Department of Geography, University of Bucharest, Bucharest, Romania b FAD Smart Technology SRL, Str. Olari, 7, Bucharest 024056, Romania c Department of Geology and Geophysics, Woods Hole Oceanographic Institution, Woods Hole, MA 02543, USA A R T I C L E I N F O A B S T R A C T Article history: The growth of Chilia deltaic lobes reflects a drastic reorganization of the Danube delta that accompanied Received 12 June 2014 its rapid expansion in the late Holocene. Using new cores collected at the apices of the two older Chilia Received in revised form 20 July 2014 lobes, together with historical maps and satellite photos, we find that a partial avulsion since 1500 Accepted 23 July 2014 years BP led to a gradual rejuvenation of the Chilia distributary. This process led to the successive infilling of a lake and a lagoon and subsequently to the construction of an open coast lobe at the Black Sea coast. Keywords: The Chilia branch became the largest Danube distributary, reaching its maximum sediment load in the Deltas last 300 years as the southernmost St. George branch lost its previous dominance. Here, we propose that Avulsion the intensive deforestation of Danube’s lower watershed leading to this delta reorganization has Land use historical cultural causes: an increase in sheep and timber demand associated to the Ottoman Empire Ottoman Empire Columbian Exchange expansion in Eastern Europe followed by the adoption of maize agriculture as a result of the Columbian Exchange. -
Chapter 5 Drainage Basin of the Black Sea
165 CHAPTER 5 DRAINAGE BASIN OF THE BLACK SEA This chapter deals with the assessment of transboundary rivers, lakes and groundwa- ters, as well as selected Ramsar Sites and other wetlands of transboundary importance, which are located in the basin of the Black Sea. Assessed transboundary waters in the drainage basin of the Black Sea Transboundary groundwaters Ramsar Sites/wetlands of Basin/sub-basin(s) Recipient Riparian countries Lakes in the basin within the basin transboundary importance Rezovska/Multudere Black Sea BG, TR Danube Black Sea AT, BA, BG, Reservoirs Silurian-Cretaceous (MD, RO, Lower Danube Green Corridor and HR, CZ, DE, Iron Gate I and UA), Q,N1-2,Pg2-3,Cr2 (RO, UA), Delta Wetlands (BG, MD, RO, UA) HU, MD, ME, Iron Gate II, Dobrudja/Dobrogea Neogene- RO, RS, SI, Lake Neusiedl Sarmatian (BG-RO), Dobrudja/ CH, UA Dobrogea Upper Jurassic-Lower Cretaceous (BG-RO), South Western Backa/Dunav aquifer (RS, HR), Northeast Backa/ Danube -Tisza Interfluve or Backa/Danube-Tisza Interfluve aquifer (RS, HU), Podunajska Basin, Zitny Ostrov/Szigetköz, Hanság-Rábca (HU), Komarnanska Vysoka Kryha/Dunántúli – középhegység északi rész (HU) - Lech Danube AT, DE - Inn Danube AT, DE, IT, CH - Morava Danube AT, CZ, SK Floodplains of the Morava- Dyje-Danube Confluence --Dyje Morava AT, CZ - Raab/Rába Danube AT, HU Rába shallow aquifer, Rába porous cold and thermal aquifer, Rába Kőszeg mountain fractured aquifer, Günser Gebirge Umland, Günstal, Hügelland Raab Ost, Hügelland Raab West, Hügelland Rabnitz, Lafnitztal, Pinkatal 1, Pinkatal 2, Raabtal, -
Implementation of the Strategic Action Plan for the Rehabilitation and Protection of the Black Sea
Implementation of the Strategic Action Plan for the Rehabilitation and Protection of the Black Sea (2002-2007) A report by the Commission on the Protection of the BLack Sea Against Pollution © 2009, Commission on the Protection of the Black Sea Against Pollution ISBN 978-9944-245-35-7 For bibliographic purposes this document may be cited as: BSC, 2009. Implementation of the Strategic Action Plan for the Rehabilitation and Protection of the Black Sea (2002-22007). Publications of the Commission on the Protection of the Black Sea Against Pollution (BSC), 2009-11, Istanbul, Turkey, 252 pp. This document has been prepared with the financial assistance of the European Union. The views expressed herein can in no way be taken to reflect the official opinion of the European Union. This publication may be reproduced in whole or in part and in any form for educational or non-profit purposes without special permission from the copyright holder, provided acknowledgement of the source is made. Commission on the Protection of the Black Sea Against Pollution would appreciate receiving a copy of any publication that uses this publication as a source. No use of this publication may be made for resale or for any other commercial purpose whatsoever without prior permission in writing from the Permanent Secretariat of the Black Sea Commission on the Protection of the Black Sea Against Pollution. Cover design: Nilufer Akpinar Cover image: The image used on the cover of this book is provided by the NASA's Visible Earth website at: http://earthobservatory.nasa.gov/images/imagerecords/8000/8817/ BlackSea_AMO_2008156_lrg.jpg Published by Referans Çeviri Hizmetleri, Yazýlým ve Yayýncýlýk Ltd.