AQUATIKA GUIDE the Story with the River
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Plitvice Lakes National Park, 96 Pp; I
WORLD HERITAGE NOMINATION - IUCN TECHNICAL EVALUATION PLITVICE LAKES EXTENSION (CROATIA) 1. DOCUMENTATION i) IUCN/WCMC Data Sheet: ii) Literature consulted: S. Bozicevic. (undated) The Plitvice Lakes, Plitvice Lakes National Park, 96 pp; I. Pevalak. 1968. The biodynamics of the Lakes of Plitvice and their protection; S. Bozicevic (ed). 1998. The Plitvice Lakes National Park – Natural History, Guide, Photomonography 96pp, Plitvice Lakes National Park; M. Schneider-Jacoby. 1996. A view from abroad: Nature Preservation in Croatia – An investment in the future of the country, Turizam Vol 44, No 11/12; B. Stilinovic and S. Bozicevic. 1988. The Plitvice Lakes – A natural phenomenon in the middle of the Dinaric Karst in Croatia, European Water Management, Vol 1, No 1. iii) Consultations: three external reviewers; Ministry of Environmental Protection and Physical Planning, Zagreb; Plitvice Lakes National Park, Plitvicka Jezero. iv) Field Visit: Michael Smart, March, 2000. 2. SUMMARY OF NATURAL VALUES The area inscribed on the World Heritage List in 1979 as Plitvice Lakes National Park (PLNP) covered 19,462ha. In 1997, the area of the National Park was extended by the Croatian Parliament to 29,482ha. The Croatian authorities have now proposed that the World Heritage site be extended to include this enlargement of the park by 10,020ha. PLNP is situated in the karst area of Croatia. It consists of a series of lakes in the valley of the Bijela rijeka (White River) and Crna rijeka (Black River), which join to become the Korana River, which flows into the River Kupa and eventually into the River Sava. The lakes are formed by barriers of travertine (or tufa) across the valley which create deep highly oligotrophic lakes. -
Riviera Paklenica
MTB 04* Velebit 3 Road 02* Paklenica 1 This attractive trail through the peaks and slopes of the southern Velebit moun- This bike route is intended for riders who prefer a long, constant but not too tain will be especially appealing to the MTB and trekking riders in better physi- steep ascent. In addition, you will get the chance to see Velebit mountain cal condition for whom long ascents do not represent a greater problem. From range both from the southern and from the northern side. After the start in the sea level start on almost 1000 m hights, beautiful panoramic views of the Starigrad, the route will first take you to the Adriatic road (Jadranska magis- Velebit canal and the Zadar archipelago will help you master a long ascent with- trala) right on the coast until you reach Rovenska and then you will start to out shades. Reaching the highest peak brings the reward of temperature differ- slightly ascent the Zrmanja Canyon up to the highest point (765 m), followed ence and awe of Tulove grede towers. Long serpentine descent to the Zrmanja by 11 km of well-deserved descent towards Gračac and Ričice lake. canyon will surely put a smile on your face. Given that there are no springs nor Start/Finish Starigrad Length 52.5 km gastronomic facilities on the trail, make sure to bring enough liquids. * Via Jasenice - Zaton Physical Difficulty 2/3 Route to be marked by Start/Finish Rovanjska Length 51 km Obrovački - Elevation 831 m Discover MTB, ROAD or FAMILY the end of Via Libinjska kosa - Physical Difficulty 3/3 Gračac - Štikada 2020. -
Primjena Indeksa Kvalitete Vode U Ocjeni Kakvoće Vode Krških Jezera
D. tomas et al. PrimjenA inDeksa kvAlitete voDe u ocjeni kAkvoće voDe kRških Jezera Stručni članak Professional paper UDk 556.55:556.114/.115>(497.5 Cres) primljeno (Received): 10. 7. 2013.; prihvaćeno (Accepted): 27. 11. 2013. primjena inDeKsa Kvalitete voDe u oCjeni KaKvoće voDe KršKih jezera U radu je prikazana kakvoća vode jezera primjenom indeksa Damir tomas, dipl. ing. kvalitete vode (eng. Water Quality Index, WQI) i njihov kemijski Hrvatske vode, Glavni vodnogospodarski laboratorij sastav Piperovim dijagramom. Ispitivana su jezera: Vrana na otoku Ulica Grada Vukovara 220, 10000 Zagreb Cresu, Vransko jezero kod Biograda na Moru, Baćinsko jezero [email protected] Crniševo i akumulacija Butoniga u razdoblju 2010.-2012. godine. Krešimir maldini, dipl. ing. U izračunu WQI korišteni su sljedeći pokazatelji: pH vrijednost, Hrvatske vode, Glavni vodnogospodarski laboratorij ukupna otopljena tvar (TDS), hidrogenkarbonati, ukupna tvrdoća, Ulica Grada Vukovara 220, 10000 Zagreb kloridi, sulfati, nitrati, fluoridi, kalcij, magnezij, željezo i mangan. Za izračun WQI korištene su preporuke vode za piće Svjetske natalija matić, dipl. ing. Hrvatske vode, EU jedinica zdravstvene organizacije (eng. World Health Organization, WHO) Ulica Grada Vukovara 220, 10000 Zagreb te dobiveni WQI predstavlja prikladnost voda za uporabu u vodoopskrbi. mr. sc. marija marijanović rajčić, dipl. ing. Istraživanjem je utvrđeno da je kakvoća vode na Vranskom jezeru Hrvatske vode, Glavni vodnogospodarski laboratorij kod Biograda n/m bila najlošije kvalitete u 2012. godini (WQI=870), Ulica Grada Vukovara 220, 10000 Zagreb dok je najbolja kakvoća vode zabilježena na jezeru Vrana na otoku Cresu u 2012. godini (WQI=31,2). Prema Piperovom dijagramu ispitivana jezera se po kemijskom sastavu razlikuju ovisno o hidrološkom dobu, dok je Vransko jezero na Cresu ujednačene kakvoće. -
Aquatic Molluscs of the Mrežnica River
NAT. CROAT. VOL. 28 No 1 99-106 ZAGREB June 30, 2019 original scientific paper / izvorni znanstveni rad DOI 10.20302/NC.2019.28.9 AQUATIC MOLLUSCS OF THE MREŽNICA RIVER Luboš Beran Nature Conservation Agency of the Czech Republic, Regional Office Kokořínsko – Máchův kraj Protected Landscape Area Administration, Česká 149, CZ–276 01 Mělník, Czech Republic (e-mail: [email protected]) Beran, L.: Aquatic molluscs of the Mrežnica River. Nat. Croat. Vol. 28, No. 1., 99-106, Zagreb, 2019. Results of a malacological survey of the Mrežnica River are presented. The molluscan assemblages of this river between the boundary of the Eugen Kvarternik military area and the inflow to the Korana River near Karlovac were studied from 2013 to 2018. Altogether 29 aquatic molluscs (19 gastropods, 10 bivalves) were found at 9 sites. Theodoxus danubialis, Esperiana esperi, Microcolpia daudebartii and Holandriana holandrii were dominant at most of the sites. The molluscan assemblages were very similar to assemblages documented during previous research into the Korana River. The populations of the endangered bivalves Unio crassus and Pseudanodonta complanata were recorded. An extensive population of another endangered gastropod Anisus vorticulus was found at one site. Physa acuta is the only non-native species confirmed in the Mrežnica River. Key words: Mollusca, Unio crassus, Anisus vorticulus, Mrežnica, faunistic, Croatia Beran, L.: Vodeni mekušci rijeke Mrežnice. Nat. Croat. Vol. 28, No. 1., 99-106, Zagreb, 2019. U radu su predstavljeni rezultati malakološkog istraživanja rijeke Mrežnice. Sastav mekušaca ove rijeke proučavan je na području od Vojnog poligona Eugen Kvarternik do njenog utoka u Koranu blizu Karlovca, u razdoblju 2013. -
Article N° 09 Conf. CM², Split, Croatie, 2017
Conférence Méditerranéenne Côtière et Maritime EDITION 4, SPLIT, CROATIA (2017) Coastal and Maritime Mediterranean Conference Disponible en ligne – http://www.paralia.fr – Available online Adriatic karstic estuaries, their characteristics and evolution Mladen JURAČIĆ 1 1. University of Zagreb, Faculty of Science, Department of Geology, Horvatovac 102a, 10 000 Zagreb, Croatia. [email protected] Abstract: The coastal area of the eastern Adriatic is characterized with a prevalence of carbonate rocks and well-developed karst. Present freshwater input into the Adriatic is quite large, mostly through coastal and submarine springs. However, there are also a number of rivers debouching in the Adriatic from the eastern coast. Most of them have canyon like fluviokarstic valleys that were carved dominantly during Pleistocene and were drowned during post-LGM sea-level rise forming estuaries. These estuaries are filled to a different extent during Holocene highstand (last 7.500 years). The intraestuarine delta progradation is rather different in those estuaries depending on the quantity of the river- borne material. Human impact on progradation rate in some of the estuaries has been shown. Keywords: Estuaries, Sedimentation, Intraestuarine delta, Progradation, Allogenic river, Anthopo- genic influence. https://dx.doi.org/10.5150/cmcm.2017.009 45 Mediterranean rocky coasts: Features, processes, evolution and problems 1. Introduction Eastern Adriatic coastal area is formed predominantly in Mesozoic carbonate rocks with well-developed karst (PIKELJ & JURAČIĆ, 2013). Due to prevalent humid climatic conditions and karst maturation present freshwater input into the Adriatic is large, mostly through coastal and submarine springs (vruljas). However, there are also a number of rivers debouching into the Adriatic. -
Review of Research on Plitvice Lakes, Croatia in the Fields of Meteorology, Climatology, Hydrology, Hydrogeochemistry and Physical Limnology
GEOFIZIKA VOL. 35 2018 DOI: 10.15233/gfz.2018.35.9 Review paper Review of research on Plitvice Lakes, Croatia in the fields of meteorology, climatology, hydrology, hydrogeochemistry and physical limnology Zvjezdana Bencetić Klaić 1, Josip Rubinić 2 and Sanja Kapelj 3 1 Department of Geophysics, Faculty of Science, University of Zagreb 2 Faculty of Civil Engineering, University of Rijeka 3 Faculty of Geotehnical Engineering, University of Zagreb Received 16 April 2018, in final form 22 October 2018 In lakes, several physical, chemical, and biological processes occur simulta- neously, and these processes are interconnected. Therefore, the investigation of lakes requires a multidisciplinary approach that includes physics (including the physics of the atmosphere, i.e., meteorology), chemistry, geology, hydrogeology, hydrology and biology. Each of these disciplines addresses a lake from a different point of view. However, lake studies that primarily belong to one field, at least to some extent, report their findings in ways that are associated with other fields; this type of reporting is caused by the inherent interconnections between phe- nomena from different disciplines. Plitvice Lakes, Croatia, are composed of a unique cascading chain of karst lakes, and these lakes have been investigated by numerous authors. Here, we provide an overview of the studies of the Plitvice Lakes Area (PLA) that address meteorology, climatology, hydrology, hydrogeo- chemistry and physical limnology. Our aim is to synthesize the results from each of these disciplines and make them available to scientists from other related disciplines; thus, this review will facilitate further investigations of the PLA within the natural sciences. In addition, valuable results from early investiga- tions of Plitvice Lakes are generally unavailable to the broader scientific com- munity, and are written in Croatian. -
Groundwater Bodies at Risk
Results of initial characterization of the groundwater bodies in Croatian karst Zeljka Brkic Croatian Geological Survey Department for Hydrogeology and Engineering Geology, Zagreb, Croatia Contractor: Croatian Geological Survey, Department for Hydrogeology and Engineering Geology Team leader: dr Zeljka Brkic Co-authors: dr Ranko Biondic (Kupa river basin – karst area, Istria, Hrvatsko Primorje) dr Janislav Kapelj (Una river basin – karst area) dr Ante Pavicic (Lika region, northern and middle Dalmacija) dr Ivan Sliskovic (southern Dalmacija) Other associates: dr Sanja Kapelj dr Josip Terzic dr Tamara Markovic Andrej Stroj { On 23 October 2000, the "Directive 2000/60/EC of the European Parliament and of the Council establishing a framework for the Community action in the field of water policy" or, in short, the EU Water Framework Directive (or even shorter the WFD) was finally adopted. { The purpose of WFD is to establish a framework for the protection of inland surface waters, transitional waters, coastal waters and groundwater (protection of aquatic and terrestrial ecosystems, reduction in pollution groundwater, protection of territorial and marine waters, sustainable water use, …) { WFD is one of the main documents of the European water policy today, with the main objective of achieving “good status” for all waters within a 15-year period What is the groundwater body ? { “groundwater body” means a distinct volume of groundwater within an aquifer or aquifers { Member States shall identify, within each river basin district: z all bodies of water used for the abstraction of water intended for human consumption providing more than 10 m3 per day as an average or serving more than 50 persons, and z those bodies of water intended for such future use. -
ACTIVE FLOOD DEFENCE in CROATIA: Regulatory Framework, Roles & Responsibilities
Workshop on Flood Risk Management measures & links to EU WFD November 11-12, 2015, Zagreb, Croatia ACTIVE FLOOD DEFENCE IN CROATIA: regulatory framework, roles & responsibilities Zoran Đurokovi ć, M.Sc.C.E. Croatian Waters Main Flood Protection Centre Head of Main Centre ∗ Climate change has intensified in recent years worldwide, including Croatia ∗ Extremely dry and wet periods have been alternating frequently in the last approximately 15 years ∗ Damage from extreme hydrological events is increasing ∗ “Average” or “normal” years are becoming increasingly rarer ∗ The frequency of high water waves and extreme water levels including floods is increasing ∗ There are almost no longer any rules concerning the occurrence of high water waves ∗ Forecasting climate models indicate increasingly frequent extreme climate events, both globally and locally ∗ Only in the last 15 years or so, the major part of the Croatian territory has experienced frequent extreme hydrological events which caused droughts in the years 2000, 2003, 2011 and 2012, but also floods in the years 2002, 2004, 2005, 2006, 2009, 2010, 2012, 2013, 2014 and 2015 ∗ Heavy damage is recorded, primarily in agriculture, but settlements, infrastructure and industrial facilities are also at risk ∗ Still, unlike in many other countries, major fatalities and disastrous damage in the urban areas have been avoided in Croatia ∗ Floods are natural phenomena which cannot be completely prevented. However, flood risks can be reduced to an acceptable level through constant development of flood -
Transboundary Aquifers in Asia Unesdoc.Unesco.Org/Images/0015/ with Special Emphasis to China, UNESCO- 001589/158963S.Pdf>
The designations employed and the presentation of material throughout the publication do not imply the expression of any opinion what- soever on the part of UNESCO and or UNILC, in particular concerning the legal status of any country, territory or city or of its authorities, or concerning the delimitation of its frontier or boundaries. Ms Raya Marina Stephan, Expert in international water law, consultant at UNESCO-IHP, Coordinator of the UNESCO ISARM legal component. This brochure has been prepared for the International Hydrological Program IHP. The editor wishes to thank the UNESCO-IHP Secretariat for its support and in particular Mr. Farès Kessasra and Ms Rosalind Wright. Published in 2009 By the United Nations Educational, Scientific and Cultural Organization 7, place Fontenoy, 75352 Paris 07 SP Composed by Eric Loddé, 93200 Saint-Denis, France. Printed by UNESCO SC-2008/WS/35 REV ©UNESCO 2009 Printed in France #*#-*0(3"1): Appelgren B. Managing Shared Aquifer Resour- Internationally Shared (Transboundary) Aquifer ces in Africa, IHP-VI, UNESCO, Series on Resources Management, Their Significance and Groundwater No. 8, Paris, France, 2004, Sustainable Management. A framework Docu- <http://unesdoc.unesco.org/images/ ment, IHP-VI, Paris, France, November 0013/001385/138581m.pdf>. 2001. <http://unesdoc.unesco.org/ Da Franca N., Miletto M., Donoso M.C et images/0012/001243/124386e.pdf>. al., Sistemas Acuiferos transfronterizos en las Stephan R., Amani A., Otchet A. ‘A Blue Américas: Evaluacion preliminar, Programa Goldmine in Need of Protection’ in UNESCO/OEA ISARM Americas World of Science, Vol. 5, No. 3, July-Sep- No. 1, Montevideo, Washington D.C tember 2007. -
Karta – Nordijsko Hodanje I Pješačenje
Begovo Brdo Begovo Brdo Snos Polojski Varoš Batnoga Donja Glina Ponor Snos Polojski Varoš [email protected] WWW.TZ-SLUNJ.HR | SL6A Batnoga KUPALIŠTE Donja Glina Ponor TEL. 047/777-630 TEL. SLUNJ 47240 7, RADIĆ BRAĆE ULICA | Kutanja JEZERO Cetingrad TOURIST OFFICE SLUNJ OFFICE TOURIST TURISTIČKA ZAJEDNICA GRADA SLUNJA GRADA ZAJEDNICA TURISTIČKA SL6A GRADA SLUNJA GRADA TURISTIČKA ZAJEDNICA TURISTIČKA KUPALIŠTE Kutanja Delić Poljana KUPALIŠTE TC MIRJANA JEZERO Cetingrad KARAČA SL6 CT1 Delić Poljana SL5 KUPALIŠTE GlinskoTC MIRJANAVrelo KARAČA D1 SL6B CRKVA Donji Nikšić SV. NIKOLE SL6 CT1 KOSOVI Donji Cerovac SL5 Glinsko Vrelo MLINOVI Strmačka D1 SL6B CRKVA Gornja Glina SV. NIKOLE KOSOVI Donji Nikšić Donji Cerovac RESTORAN Gornji Cerovac Strmačka PINO MLINOVI Gornja Glina STARI GRAD Gornji Nikšić CETIN RESTORAN Gornji Cerovac MarindolskoPINO Gornje Podcetin NERALIĆ Brdo MLIN Tatar Varoš Gnojnice STARI GRAD SL7 Gornji Nikšić CETIN GRŽANOVE Cvitović Marindolsko Cetinska Varoš Gornje Podcetin LUKE D1 NERALIĆ Brdo MLIN Tatar Varoš Gnojnice Donji Kremen SL7 Gnojnice Bilo GRŽANOVE Cvitović Zečev Varoš Gornje LUKEMali Vuković D1 Cetinska Varoš Taborište Miljevac Donje Donji Kremen Gnojnice Bilo Taborište Sadikovac Zečev Varoš Gornje MaliDonje Vuković Gnojnice Taborište Donje Miljevac SL8 SL1 Taborište KUPALIŠTE Kapljuv Sadikovac Gornji Kremen GNOJNICE Donje Gnojnice Rastoke SL2 KUPALIŠTE KUTEREVČEVA CT2 KOTLAC PEĆINA SALOPEK SL8 MLINSL1 KUPALIŠTE Kapljuv Gornji Kremen Kestenje GNOJNICE Rastoke SLUNJ SL2 KUPALIŠTE KUTEREVČEVA CT2 KOTLAC PEĆINA SALOPEK MLIN Kestenje MATEŠIĆEVA PEĆINA SL3 SLUNJ Lađevačko Srednje Selo Podmelnica Selište SLUNJ RASTOKE RUTA BR. / ROUTE NO. 1 Dubrava Rastočka rapsodija | Rastoke Rhapsody MATEŠIĆEVA ID: SL1 | D: 2.4 km PEĆINA SL3 Luke Gornji Popovac Lađevačko KARTA ZA NORDIJSKO HODANJE I PJEŠAČENJE | NORDIC WALKING AND HIKING D1 RUTA BR. -
Maritime Museums and the Representation of Cultural Boundaries in the Upper Adriatic
Nar. umjet. 43/1, 2006, pp. 15-39, P. Ballinger, Lines in the Water, Peoples on the Map… Original scientific paper Received: 10th Jan. 2006 Accepted: 13th March 2006 UDK 341.222:556.1(497.5-3) PAMELA BALLINGER Department of Sociology and Anthropology, Bowdoin College, Brunswick LINES IN THE WATER, PEOPLES ON THE MAP: MARITIME MUSEUMS AND THE REPRESENTATION OF CULTURAL BOUNDARIES IN THE UPPER ADRIATIC This article explores the relationship between political and symbolic borders in the Gulf of Trieste. The author inquires into the persistence of understandings that map peoples onto specific territories and terrains, such as the stereotypical association of Italians with the coast and Slavic peoples (Slovenes and Croats) with the rural interior. Focusing on representations of maritime culture along two contentious political borders – that between Italy and Slovenia and that between Slovenia and Croatia – the analysis demonstrates that museums become powerful sites for the reproduction of the coast/interior cultural boundary, even when the specific ethnic groups it maps onto change. Keywords: Adriatic, Istria, borders, maritime culture, museums, representations, stereotypes In The Mediterranean and the Mediterranean World in the Age of Philip II, Fernand Braudel famously argued that, at least into the 17th century, "The Adriatic is perhaps the most unified of all the regions of the sea" (Braudel 1972:125).1 In the succeeding centuries, however, the Adriatic has often been imagined as constituting a border zone between culture areas, languages, religions, and environments. In the 19th century, distinctions between peoples living along the coast and in the interior of the Eastern Adriatic increasingly became mapped onto ethno-national divisions even as the Habsburg Empire fostered a multi-ethnic maritime culture centered on Trieste/Trst and 1 The research for this article was made possible by monies from the Rusack Fund at the Coastal Studies Center at Bowdoin College. -
Case Study of Kupa River Watershed in Croatia
J. Hydrol. Hydromech., 67, 2019, 4, 305–313 DOI: 10.2478/johh-2019-0019 Long term variations of river temperature and the influence of air temperature and river discharge: case study of Kupa River watershed in Croatia Senlin Zhu1, Ognjen Bonacci2, Dijana Oskoruš3, Marijana Hadzima-Nyarko4*, Shiqiang Wu1 1 State Key Laboratory of Hydrology-Water resources and Hydraulic Engineering, Nanjing Hydraulic Research Institute, Nanjing 210029, China. 2 Faculty of Civil Engineering and Architecture, University of Split, Matice hrvatske 15, 21000 Split, Croatia. 3 Meteorological and Hydrological Service, Gric 3, 10000 Zagreb, Croatia. 4 Josip Juraj Strossmayer University of Osijek, Faculty of Civil Engineering and Architecture Osijek, Vladimira Preloga 3, 31000 Osijek, Croatia. * Corresponding author. E-mail: [email protected] Abstract: The bio-chemical and physical characteristics of a river are directly affected by water temperature, which therefore affects the overall health of aquatic ecosystems. In this study, long term variations of river water temperatures (RWT) in Kupa River watershed, Croatia were investigated. It is shown that the RWT in the studied river stations in- creased about 0.0232–0.0796ºC per year, which are comparable with long term observations reported for rivers in other regions, indicating an apparent warming trend. RWT rises during the past 20 years have not been constant for different periods of the year, and the contrasts between stations regarding RWT increases vary seasonally. Additionally, multi- layer perceptron neural network models (MLPNN) and adaptive neuro-fuzzy inference systems (ANFIS) models were implemented to simulate daily RWT, using air temperature (Ta), flow discharge (Q) and the day of year (DOY) as predic- tors.