DOCSLIB.ORG

Cultural Informations

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text

Load more

CULTURAL INFORMATIONS DREŽNIK GRAD The old town Drežnik is the fortress which is situated on the edge of the village Drežnik Grad, municipality of Rakovica, County of Karlovac in Central Croatia. Historical happenings in this area are mostly connected with constant warfare concerning borders and defense from conquerors' incursions, which is why the area had not developed as a market town or a settlement, but rather as a defensive fort, especially Drežnik Grad (Drežnik Castle). This area used to be the seat of the one-time County of Drežnik which was first mentioned in the 11th century. Drežnik frotress (Drežnik Castle) was an integral part of a chain of fortifications to defend against the Turks and Drežnik fortress was repeatedly conquered, ruined and rebuilt. The fortress is located on a cliff above a steep canyon of the river Korana which arose from Plitvice lakes and abruptly turns eastward and forms the present-day border with Bosnia and Herzegovina. Old town Drežnik - made of irregular rectangular shape, stone walls, two square towers and one round tower which is located on the north side of fortress. Until recently, it was almost entirely in ruins. Now, the round tower is completely walled in, while some parts of ruined fortress rising (sticking) from the bushes. PLITVICE LAKES NATIONAL PARK ( www.np-plitvicka-jezera.hr) Croatia's first National park established in 1949 covers 296.85 km2 of breathtaking natural splendor becoming with it the largest among the eight national parks of the country. The park was inscribed on the UNESCO's World Heritage List in 1979, in recognition of its "outstanding natural beauty and undisturbed production of travertine (tufa) through chemical and biological action". The park represents a phenomenon of karst hydrography. The park harbours a grand collection of waterfalls, gallery of lakes, forest and diversity of animal life. The lakes are renowned for their distinctive colors, ranging from azure to green, grey or blue. The colors change constantly depending on the quantity of minerals or organisms in the water and the angle of sunlight. The sixteen lakes which are formed by natural dams of travertine are separated into upper and lower lakes. About eight km of pathways and wooden walking trails around lakes are accessible to visitors. Trails are descending from an altitude of 636m to 503m above sea level. From the introduction to “The natural history guide” (by Prof. dr. sc. Milan Mestrov, academic) The natural attributes of the Plitvice Lakes National Park, uniqueness and sensibility of that phenomenon, deserve a full attention of our visitors. Recreational aspect of stay and the amazement with beauty of the area that conquers by its natural diversity and harmony of shapes and colours in any of the seasons, is based on many mutually conditioned natural characteristics. That is a specific geological and hydrogeological phenomenon of karst. The series of 16 bigger and a few smaller lakes, gradually lined up, separated by travertine barriers for which the period of the last ten thousand years was crucial, and which were ruled by ecological relations similar to those of today - suitable for travertine depositing and for the origin of the lakes - are the basic phenomenon of the National Park. Travertine forming plants, algae and mosses have been and still are playing an important role in their creation, thus making a very sensitive biodynamic system. Transitive type of climate between coastal and continental with microclimate diversities makes summer pleasant and sunny, while on the other side winter is relatively long, harsh and snowrich. There are large forestry complexes in the Park area, of which some sections are protected as a special reserve of forestry vegetation due to its primeval characteristics (Corkova uvala virgin forest). Diversity of places and living conditions makes possible for numerous species of plants and animals in watery and terrestrial areas of the Park to develop with no disturbancy. It should be stressed that all fundamental things that do determine the Park, make a very fragile structural and functional complex, sensitive to natural changes and to incautious human actions. CAVES OF BARAĆ (www.baraceve-spilje.hr) Croatia is a speleological El Dorado. Not many countries in the world have so much surface covered in karst. Over fifty per cent of Croatian territory, even seventy per cent if we include the undersea surface area, is made of limestone. Limestone easily dissolves in water. Interaction of water and limestone creates a unique and specific relief with a large number of karst forms. In our country, karst stretches from Istria, over Croatian Littoral, Gorski Kotar, Kordun, Lika and Dalmatia including islands, all through the border with Montenegro. Dinaric Kras extends from Soča, along the Adriatic Sea, all through Albania. Croatia knows a large number of speleological sites marked by abundance of cave jewels, endemic species of cave fauna (such as olms), and valuable paleontological and archaeological findings. Caves of Barać are located some six kilometres to the east of Rakovica, just over half a kilometre to the west from the centre of the village of Nova Kršlja. Entrances to all three caves from the north are called Baraćeve Brine. At the bottom of Brine, between the entrances to the caves, is Baraćevac spring, which, together with two smaller springs (without name) form Kršlja stream that merges with the Suvaja stream some twenty meters downstream. Kršlja flows several kilometres through the field, and at its eastern part, through a series of pits, enters the Varićak Cave, where it accounts for the greatest amount of water mass in its channels. Caves of Barać were once known as Radaković Caves. The last name Barać no longer exists in this region – this is a toponym from the times before or during Turkish invasions. According to the local legend, the caves were named after someone named Barać who defeated the furious Turkish giant in the battlefield and earned himself such honour. We know that there are three caves. The first records of this area, including Caves of Barać, can be found in the History of Cartography of the Area of Krajina by Marsiglia published in 1699. Marsiglia spent time in this area and produced the first known topographic maps of Croatian-Turkish border divided in 37 sections in the scale of 1:30000. After the World War II, Caves of Barać were almost forgotten by the tourists, neglected, in terms of visits and maintenance, although some elements of upkeep could still be visible. It was only recently, through the Decree of the Municipal Council of Rakovica Municipality, that action was initiated and the Committee for the Revitalization of Caves of Barać was formed. Meanwhile, several large-scale, international speleological expeditions were organized that proved very successful: a lot of new speleological sites were discovered and explored. The first Croatian speleologists’ centre was built in Nova Kršlja, the Lower and Upper Caves were barred with iron grid gates, the area surrounding the Baraćevac spring was cleaned, the intensive development of the Cave Protection Survey began, along with preparations for opening the caves to visitors. The Third or the New Cave was rediscovered after keeping its secrets and stories hidden for about a hundred years. The new topographic drawings of all three Caves of Barać were made. in July 2004, the Caves were again open to general public after 112 years. RASTOKE (SLUNJ) ( www.slunj-rastoke.com ) Rastoke is the watermill village situated where the blue-green waters of river Slunjčica flows into the Korana river. Because of its extraordinary natural beauties and historical tradition, in 1962 Rastoke village fell under the protection of the State Directorate for cultural and historical heritage. Many ancient civilizations, as well as contemporary urban environments witness that the water has always attracted people to come to its banks and settle there. For thousands of years, the waters of Korana and Slunjčica, and their flora and fauna, fought the laws of nature, and as a result of this struggle in the limestone plateau, a remarkable canyon was carved in for us to take pleasure in. Seeing this natural phenomenon, this "poured off" ("rastočen") terrain, a place where the waters of river Slunjčica pour off in several backwaters, leaving behind small elevations which then form watercourses and waterfalls, people built a village and named it RASTOKE. Here, they found everything they needed and stayed here, forever bound with nature. Rastoke is a village of ambiance value and authentic heritage when it comes to architecture, and according to some records, it was built in the 17th century, possibly even earlier. Most of the houses were built at the end of the 19th and the beginning of the 20th century. People have always lived in Rastoke. Grain from nearby villages was constantly being milled here, and since its location is by the main road – which connects southern and northern part of Croatia – it became the intersection of various buyers, dealers and live stock traders. This rich village constantly suffered war damages and other social caused troubles that destroyed it and set its development back to the beginning. Although people were forced to move away, the nature always stayed and defied the odds with its distinctiveness. Today, there are about 30 households in Rastoke, and their wish is to renew the water mills and start running businesses thanks especially to the tourism interests. BIHAĆ (Bosnia and Herzegovina) ( www.panacomp.net) Bihać is town situated in Una-Sana Canton, in the northwest part of Bosnia and Herzegovina, on the border between Croatia and Bosnia and Herzegovina, very close /about 30 km/ to the Plitvice Lakes. Bihać is a town with rich history, an economic and cultural center of Una-Sana Canton.
Recommended publications
  • Plitvice Lakes National Park, 96 Pp; I

    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.
  • Aquatic Molluscs of the Mrežnica River

    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.
  • Review of Research on Plitvice Lakes, Croatia in the Fields of Meteorology, Climatology, Hydrology, Hydrogeochemistry and Physical Limnology

    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.
  • ACTIVE FLOOD DEFENCE in CROATIA: Regulatory Framework, Roles & Responsibilities

    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
  • Karta – Nordijsko Hodanje I Pješačenje

    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.
  • Diversity of Alien Macroinvertebrate Species in Serbian Waters

    Diversity of Alien Macroinvertebrate Species in Serbian Waters

    water Article Diversity of Alien Macroinvertebrate Species in Serbian Waters Katarina Zori´c* , Ana Atanackovi´c,Jelena Tomovi´c,Božica Vasiljevi´c,Bojana Tubi´c and Momir Paunovi´c Department for Hydroecology and Water Protection, Institute for Biological Research “Siniša Stankovi´c”—NationalInstitute of Republic of Serbia, University of Belgrade, Bulevar despota Stefana 142, 11060 Belgrade, Serbia; [email protected] (A.A.); [email protected] (J.T.); [email protected] (B.V.); [email protected] (B.T.); [email protected] (M.P.) * Correspondence: [email protected] Received: 29 September 2020; Accepted: 7 December 2020; Published: 15 December 2020 Abstract: This article provides the first comprehensive list of alien macroinvertebrate species registered and/or established in aquatic ecosystems in Serbia as a potential threat to native biodiversity. The list comprised field investigations, articles, grey literature, and unpublished data. Twenty-nine species of macroinvertebrates have been recorded since 1942, with a domination of the Ponto-Caspian faunistic elements. The majority of recorded species have broad distribution and are naturalized in the waters of Serbia, while occasional or single findings of seven taxa indicate that these species have failed to form populations. Presented results clearly show that the Danube is the main corridor for the introduction and spread of non-native species into Serbia. Keywords: Serbia; inland waters; allochthonous species; introduction 1. Introduction The Water Framework Directive (WFD) [1] represents key regulation and one of the most important documents in the European Union water legislation since it was adopted in 2000.
  • Case Study of Kupa River Watershed in Croatia

    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.
  • Memorial of the Republic of Croatia

    Memorial of the Republic of Croatia

    INTERNATIONAL COURT OF JUSTICE CASE CONCERNING THE APPLICATION OF THE CONVENTION ON THE PREVENTION AND PUNISHMENT OF THE CRIME OF GENOCIDE (CROATIA v. YUGOSLAVIA) MEMORIAL OF THE REPUBLIC OF CROATIA APPENDICES VOLUME 5 1 MARCH 2001 II III Contents Page Appendix 1 Chronology of Events, 1980-2000 1 Appendix 2 Video Tape Transcript 37 Appendix 3 Hate Speech: The Stimulation of Serbian Discontent and Eventual Incitement to Commit Genocide 45 Appendix 4 Testimonies of the Actors (Books and Memoirs) 73 4.1 Veljko Kadijević: “As I see the disintegration – An Army without a State” 4.2 Stipe Mesić: “How Yugoslavia was Brought Down” 4.3 Borisav Jović: “Last Days of the SFRY (Excerpts from a Diary)” Appendix 5a Serb Paramilitary Groups Active in Croatia (1991-95) 119 5b The “21st Volunteer Commando Task Force” of the “RSK Army” 129 Appendix 6 Prison Camps 141 Appendix 7 Damage to Cultural Monuments on Croatian Territory 163 Appendix 8 Personal Continuity, 1991-2001 363 IV APPENDIX 1 CHRONOLOGY OF EVENTS1 ABBREVIATIONS USED IN THE CHRONOLOGY BH Bosnia and Herzegovina CSCE Conference on Security and Co-operation in Europe CK SKJ Centralni komitet Saveza komunista Jugoslavije (Central Committee of the League of Communists of Yugoslavia) EC European Community EU European Union FRY Federal Republic of Yugoslavia HDZ Hrvatska demokratska zajednica (Croatian Democratic Union) HV Hrvatska vojska (Croatian Army) IMF International Monetary Fund JNA Jugoslavenska narodna armija (Yugoslav People’s Army) NAM Non-Aligned Movement NATO North Atlantic Treaty Organisation
  • Session 4 SRB Assessment

    Session 4 SRB Assessment

    Status of transboundary waters in South Eastern Europe Characterization Report on the Sava River Basin Dejan Komatina, Ph.D. Civ. Eng., Secretary, ISRBC General description of the basin • The Sava River Basin as a Danube sub-basin – Basin area: 95 720 km 2 (the second largest, after the Tisza basin) – Average flow (at the mouth): 1722 m 3/s (the largest tributary) – River length: 940 km (586 km of which were navigable before the war) Country Share of the Share of the basin (%) territory (%) Albania 0.1 0.5 Bosnia & Herzegovina 40 76 Croatia 26 45 Montenegro 7.5 52 Serbia 15.4 17 Slovenia 11 53 Int. Workshop on ITWRM in SEE, Sarajevo, 18-20 May 2009 2 Overview (location) of the SRB Int. Workshop on ITWRM in SEE, Sarajevo, 18-20 May 2009 3 Int. Workshop on ITWRM in SEE, Sarajevo, 18-20 May 2009 4 Values / uses / threats Int. Workshop on ITWRM in SEE, Sarajevo, 18-20 May 2009 5 Values / uses / threats Int. Workshop on ITWRM in SEE, Sarajevo, 18-20 May 2009 6 Values / uses / threats Int. Workshop on ITWRM in SEE, Sarajevo, 18-20 May 2009 7 Values / uses / threats Int. Workshop on ITWRM in SEE, Sarajevo, 18-20 May 2009 8 Values / uses / threats Int. Workshop on ITWRM in SEE, Sarajevo, 18-20 May 2009 9 Values / uses / threats Int. Workshop on ITWRM in SEE, Sarajevo, 18-20 May 2009 10 Land cover/land use in the SRB Land class % Artificial surfaces 2,23 Agricultural areas 42,36 Forests and semi natural areas 54,71 Wetland 0,08 Inland water 0,63 Int.
  • Okoliš Detection of Coal Combustion

    Okoliš Detection of Coal Combustion

    DETECTION OF COAL COMBUSTION PRODUCTS IN STREAM SEDIMENTS BY CHEMICAL ANALYSIS AND MAGNETIC SUSCEPTIBILITY MEASUREMENTS S. Frančišković-Bilinski Institut “Ruđer Bošković”, Zavod za istraživanje mora i okoliša, Laboratorij za fizičku kemiju tragova OKOLIŠ 1. Introduction The aim of this preliminary study was to apply a rapid and inexpensive, low-field magnetic susceptibility method (MS) to stream sediments, as described by Scholger (1998) and Petrovsky et al. (2000), and to delineate ZAGREB polluted areas in the Kupa river basin. Geochemical characterization of the <63 μm sediment fraction has already Sava River been carried out (Frančišković-Bilinski, 2007). Increased MS was observed in: (1) The lower stretch of the Mrežnica and Korana rivers, where several elements (U, Sb, Sn, Zr, Nb, S, Na, Ni, Se, Sr, Y, Nb) showed Kupa River anomalously high concentrations. This region is located on the Dinaric carbonate platform and the anomalies are of Kupa River KARLOVAC SISAK anthropogenic origin. (2) At the middle flow of Glina River, where several other elements showed anomalously high concentrations (Fe, Sc, V, Zr, Na, Cu, Ga, Y). The anomalies in this region are of natural origin, influenced by Korana River Mrežnica River Supradinaric belt with ophiolites. The MS did not detect extreme Ba anomalies, described in the same drainage basin (Frančišković-Bilinski, 2006). In the present work we concentrated our research on the MS anomaly observed in the lower parts of the Mrežnica and Korana rivers. The study area, including 22 sampling locations, is presented in Figure 1. Sampling station details are listed in Table 1. The pollution source in the Mrežnica river was a large textile factory in Duga Resa (near Karlovac), which burned coal for ~110 y, until 1994; all coal slag and ash were deposited directly into the Mrežnica river.
  • Razvoj Turizma Na Području Značajnog Krajobraza Slunjčica Sadržaj 2

    Razvoj Turizma Na Području Značajnog Krajobraza Slunjčica Sadržaj 2

    GRAD SLUNJ Zagreb, kolovoz 2010. GRAD SLUNJ Autori: Prof. dr. sc. Zoran Klaric Dr. sc. Siniša Horak Zagreb, kolovoz 2010. 1 Razvoj turizma na podrucju znacajnog krajobraza Slunjcica.indd 1 2.8.2010 15:39:21 GRAD SLUNJ 1. POLAZNE OSNOVE 3 2. ANALIZA LOKACIJE I PROSTORNO-PLANSKE DOKUMENTACIJE 4 2.1. Pregled i kritički osvrt na dosadašnja planska rješenja i ideje 4 2.2. Opis lokacije 5 3. ANALIZA POSTOJEĆEG STANJA 9 3.1. Opći osvrt na razvoj turizma na području grada Slunja 9 3.2. Stanje turistifi ciranosti pojedinačnih lokaliteta na području značajnog krajobraza Slunjčica i grada Slunja u cjelini 11 3.3. Stanje razvoja turizma u širem okruženju 14 4. SWOT ANALIZA 15 5. PROCJENA PRIHVATNOG KAPACITETA PROSTORA 19 5.1. Važnost određivanja prihvatnog kapaciteta za ZK Slunjčica 19 5.2. Analiza glavnih parametara važnih za određivanje prihvatnog kapaciteta Rastoka kao glavnog lokaliteta ZK Slunjčica i mogući scenariji razvoja 20 5.3. Okvirni prihvatni kapacitet prostora Rastoka i potrebne intervencije u prostoru nužne za ostvarenje modela održivog razvoja turizma 23 6. PRIJEDLOG TURISTIČKIH AKTIVNOSTI 24 6.1. Prijedlog mogućih turističkih aktivnosti prema vrstama turizma 24 6.2. Sustav kretanja posjetitelja u zoni Rastoka i ZK Slunjčica u cjelini 24 7. ZAKLJUČAK 31 RAZVOJ TURIZMA NA PODRUČJU ZNAČAJNOG KRAJOBRAZA SLUNJČICA SADRŽAJ 2 Razvoj turizma na podrucju znacajnog krajobraza Slunjcica.indd 2 2.8.2010 15:39:29 GRAD SLUNJ 1. POLAZNE OSNOVE Područje rijeke Slunjčice i dio područja rijeke Korane do rubova kanjona, u dužini od 1 km od ušća Slunjčice nizvodno, proglašeno je značajnim krajobrazom (ZK Slunjčica), rješenjem Zavoda za zaštitu prirode, 1964.
  • BRANIMIR BARBARIĆ HISTORIJSKO-GEOGRAFSKI RAZVOJ KORDUNA Diplomski Rad Predan Na Ocjenu Geografskom Odsjeku Prirodoslovno-Matema

    BRANIMIR BARBARIĆ HISTORIJSKO-GEOGRAFSKI RAZVOJ KORDUNA Diplomski Rad Predan Na Ocjenu Geografskom Odsjeku Prirodoslovno-Matema

    View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by Repository of Faculty of Science, University of Zagreb BRANIMIR BARBARIĆ HISTORIJSKO-GEOGRAFSKI RAZVOJ KORDUNA Diplomski rad Predan na ocjenu Geografskom odsjeku Prirodoslovno-matematičkog fakulteta Sveučilišta u Zagrebu radi stjecanja akademskog zvanja magistra edukacije geografije i povijesti Zagreb 2018. Ovaj je diplomski rad izrađen u sklopu integriranog preddiplomskog i diplomskog sveučilišnog studija Geografija i povijest: smjer; nastavnički pri Geografskom odsjeku Prirodoslovno-matematičkog fakulteta Sveučilišta u Zagrebu, pod vodstvom doc. dr. sc. Ružice Vuk. II TEMELJNA DOKUMENTACIJSKA KARTICA Sveučilište u Zagrebu Diplomski rad Prirodoslovno-matematički fakultet Geografski odsjek Historijsko-geografski razvoj Korduna Branimir Barbarić Sažetak: Predmet istraživanja ovoga rada je historijsko-geografski razvoj Korduna od kasnoga srednjeg vijeka do danas, s posebnim naglaskom na etape osmanlijskih osvajanja, Vojne krajine, Drugoga svjetskog rata i Domovinskog rata. Zasebno poglavlje u radu posvećeno je određivanju prostornog obuhvata regije prema različitim kriterijima regionalizacije. Tema završne cjeline su suvremena demografska, gospodarska i prometno-geografska obilježja Korduna. Dugotrajna vojna namjena prostora nepovoljno je utjecala na razvoj regije. Domovinski rat dodatno je pogoršao već postojeće loše demografske trendove. Glavna suvremena razvojna obilježja su izrazito negativna demografska kretanja i gospodarska nerazvijenost. 52 stranice, 12 grafičkih priloga, 11 tablica, 41 bibliografska referenca; izvornik na hrvatskom jeziku Ključne riječi: Historijsko-geografski razvoj, Kordun, Vojna krajina, Domovinski rat Voditelj: Doc. dr. sc. Ružica Vuk Povjerenstvo: Doc. dr. sc. Ružica Vuk Izv. prof. pr. sc. Vuk Tvrtko Opačić Doc. dr. sc. Mladen Maradin Tema prihvaćena: 7.2.2017. Rad prihvaćen: 12.9.2018. Rad je pohranjen u Središnjoj geografskoj knjižnici Prirodoslovno-matematičkog fakulteta Sveučilišta u Zagrebu, Marulićev trg 19, Zagreb, Hrvatska.