The Natural Environment and Economy of Slovakia

Total Page:16

File Type:pdf, Size:1020Kb

The Natural Environment and Economy of Slovakia The natural environment and economy of Slovakia The natural environment and economy of Slovakia Lesson plan (Polish) Lesson plan (English) The natural environment and economy of Slovakia Source: licencja: CC 0, [online], dostępny w internecie: www.pixabay.com. Link to the lesson Before you start you should know where the Slovakia is located in Europe; what Europe's territorial division is; what Czechoslovakia was; what national minorities are; during which folding Carpathians arose. You will learn to characterise Slovakia's natural environment; to discuss Slovakia's location on a map of Europe; to name the main branches of the Slovakian economy; to give examples of tourist attractions in Slovakia. Nagranie dostępne na portalu epodreczniki.pl nagranie abstraktu Slovakia's locaon Task 1 Determine Slovakia's geographical locaon and idenfy which countries Slovakia borders. Slovakia's geographical locaon neighbouring countries Slovakia is a small country in Central Europe, with an area of 49 thousand km2, which is approximately the equivalent size to two large Polish voivodeships. It is our smallest neighbour. Like the Czech Republic, it has no diresct access to the sea, meaning that it is a landlocked country. The capital of Slovakia is Bratislava. The border between Slovakia and Poland is 541 km in length and runs entirely along the Carpathian mountains, including along their highest ridges in the Tatra, Beskid and Pienin mountains. Despite its small surface area, Slovakia borders as many as five countries (the significantly larger Czech republic borders only four) – besides Poland, they are the Czech Republic, Austria, Hungary and the Ukraine. Natural condions Task 2 Characterise Slovakia's natural condions: its landform and river system. Slovakia's natural condions In contrast to the upland Czech Republic, Slovakia is a mountain country. The Carpathians occupy the largest part of the country's area, including: The Beskids – along the border with Poland and the Czech Republic; The Tatras and the Pienins – along the border with Poland; The Low Tatras – a range of tall mountains in the centre of the country; „the smaller brother” (2043 metres above sea level) of the main Tatra mountain range with an almost identical geological structure, which consist mainly of hard granites and crystalline shales as well as soft limestone karst; The Slovak Ore Mountains – a medium‐sized mountain range in the South of the country; volcanic rocks and forms occur in their western part, for example the Pol'ana caldera (1458 metres above sea level); the eastern part, called Slovak Paradise is built of limestone karst full of various rock forms, for example, large caves. In addition to the strongly undulating mountain terrain, flat areas stretch along Slovakia's southern borders. In the centre, a limestone plateau which is known as the Slovak Karst is located. To the South‐West is the Danubian Lowland, which is a part of the Little Hungarian Plain. The Eastern Slovak Lowland, which is part of the Great Hungarian Plain, is located in the South‐East. Lowlands occupy a total of less than 20% of Slovakia's surface area. Slovakia - hypsometric map Source: Wydawnictwo Edukacyjne Wiking, licencja: CC BY 3.0. Almost the whole of the Slovakian region belongs to the Danube basin and the Black Sea basin. The Danube itself – the second largest river in Europe (after the Volga) – has a length of 172 km in Slovakia, flows through Bratislava and further on is a border river with Hungary. Most of the other Slovakian rivers flow from the mountains in a general southern direction. The longest is the Vah with a length of 403 km. Climate of Slovakia In Slovakia there is a temperate, warm transitional climate, but in large areas it is a mountainous type of this climate. In the east of the country there are influences of continental air masses and the climate there is a bit more acute. Long and cold winters are common. In the south, on the Danube, in the summer it is much warmer than in Poland due to the greater solar radiation. The populaon of Slovakia Almost 5.5 million people live in Slovakia, about as many as in our Masovian Voivodeship. The average population density is 110 inhabitants per 1 km2, which is somewhat lower than in Poland. Slovakia's low population is a result of the dominant mountanous terrain, which makes settling difficult. The population mainly lives on lower terrains – lowlands or river valleys. The greatest concentration of the population occurs in the South‐West of the country. Slovakia's populaon distribuon Source: Wydawnictwo Edukacyjne Wiking, licencja: CC BY 3.0. Slovakia's economy Slovakia's free‐market economy is a dynamic and one of the fastest‐growing economies in Europe. Slovakia, after the Czech Republic and Slovenia, is the third most economically developed country in the former Communist Bloc. There are clear differences in economic development between the eastern, poorer part of the country, and the western part, which is richer. Main sectors of the Slovakia's economy The following sectors have the highest value in the overall GDP of Slovakia (2018 data): agriculture and fishery 2.6% industry and construction 33.3% service 54,4% The share of agriculture in Slovakia's GDP amounts to 2.69%. The problem is the lack of improvement in the food self‐sufficiency of Slovakia. Domestic production covers 60% of the demand for agri‐food products. Slovakia has a large tourist potential, which is positively influenced by natural conditions - the location from 95 m (Streda nad Bodrogom) to 2 656 m above sea level. (Gerlachovský štít, the highest peak of the Carpathians), rivers, lakes and thermal springs. Source: licencja: CC 0. Exercise 1 Source: licencja: CC 0. Exercise 2 Source: Civertan, licencja: CC BY-SA 2.5. Exercise 3 Slovakia is a mountain country, which consists of numerous ranges of the Carpathians: The Pienins The Stołowe Mountains The Giant mountains The Golden mountains The Beskids The Tatras The Low Tatras The Slovak Ore mountains Exercise 4 Fill in the missing words. Danube, Slovak, mountain, Carpathians, Danubian, Braslavian, The Beskids, Poprad, tectonic, The Giant mountains, karst, ocean, The Slovak Karst, Balc Sea, The North Sea, The Slovak Ore mountains Slovakia is a small country in Central Europe which does not have access to the ................................................. The border between Poland and Slovakia runs in its enrety along the ................................................. Slovakia is a ................................................ country, which consists of numerous ranges of the Carpathians: The Beskids, The Pienins, The Tatras, The Low Tatras and ................................................. In the centre and the South of the country, regions of ................................................ formaons occur: Slovak Paradise and ................................................. Lowlands: The ................................................ Lowland and The Eastern ................................................ Lowland cover less than 20% of the country's area combined. Almost the whole of the Slovakian region belongs to the ................................................ basin and the Black Sea basin. The Poprad basin is an excepon, which belongs to the ................................................ basin. Keywords Bratislava, Slovak paradise, the Danube Glossary caldera Nagranie dostępne na portalu epodreczniki.pl Nagranie słówka: caldera kaldera - rozległe obniżenie terenu w szczytowej części wulkanu, powstałe w wyniku zniszczenia wierzchołka przez erupcję Lesson plan (Polish) Temat: Środowisko przyrodnicze i gospodarka Słowacji Adresat Uczniowie klasy VI szkoły podstawowej Podstawa programowa VIII Sąsiedzi Polski: przemiany przemysłu w Niemczech; dziedzictwo kulturowe Litwy i Białorusi; środowisko przyrodnicze i atrakcje turystyczne Czech i Słowacji; problemy polityczne, społeczne i gospodarcze Ukrainy; zróżnicowanie przyrodnicze i społeczno‐gospodarcze Ukrainy; zróżnicowanie przyrodnicze i społeczno- gospodarcze Rosji; relacje Polski z sąsiadami. Uczeń: 3) Przedstawia przykłady atrakcji turystycznych i rekreacyjno- sportowych Czech i Słowacji; 7) Rozumie potrzebę kształtowania dobrych relacji Polski z sąsiadami. Ogólny cel kształcenia Uczeń omawia środowisko przyrodnicze oraz podaje przykłady atrakcji turystycznych Słowacji. Kompetencje kluczowe porozumiewanie się w językach obcych; kompetencje informatyczne; umiejętność uczenia się. Kryteria sukcesu omówisz położenie Słowacji na mapie Europy; scharakteryzujesz środowisko przyrodnicze Słowacji; podasz przykłady atrakcji turystycznych Słowacji. Metody/techniki kształcenia podające pogadanka. aktywizujące dyskusja. programowane z użyciem komputera; z użyciem e‐podręcznika. praktyczne ćwiczeń przedmiotowych. Formy pracy praca indywidualna; praca w parach; praca w grupach; praca całego zespołu klasowego. Środki dydaktyczne e‐podręcznik; tablica interaktywna, tablety/komputery. Przebieg lekcji Przed lekcją Nauczyciel prosi wybranego ucznia lub uczniów o zapoznanie się z materiałem abstraktu i przygotowanie materiału ilustracyjnego do lekcji. Faza wstępna Nauczyciel podaje uczniom temat oraz cele lekcji. Nauczyciel uruchamia na tablicy multimedialnej aplikację Learning Apss i korzystając z Planszy interaktywnej prosi uczniów i dokonywanie zapisu skojarzeń związanych z Słowacją Dyskusja. Faza realizacyjna Uczniowie korzystają z atlasów geograficznych. Wyszukują Słowację. Jedna osoba podchodzi do mapy Europy wskazuje omawiane państwo. Praca w parach.
Recommended publications
  • Danubian Lowland - Ground Water Mode
    SK98K0043 Ministry of the Environment, Slovak Republic Commission of The European Communities DANUBIAN LOWLAND - GROUND WATER MODE PHARE PROJECT NO. PHARE/EC/WAT/1 The Old Danube Final Report Volume 1 Summary Report December 1995 Danish Hydraulic Institute, Denmark in association with DHV Consultants BV, The Netherlands TNO - Institute of Applied Geoscience, The Netherlands Water Quality Institute, Denmark I Kriiger, Denmark The Royal Veterinary and Agricultural University, Denmark Danish Hydraulic Institute Danubian Lowland - Ground Water Model Agern Alle 5, DK-2970 Harsholm, Denmark PHARE/EC/WAT/1 Telephone: +45 45 76 95 55 Final Report Telefax: +45 45 76 25 67 Telex: 37 402 dhicph dk Client Client's representative Ministry of the Environment, Programme Implementation F. Kelbel, Director, PIU Unit, Slovak Republic Project Project No Danubian Lowland - Ground Water Model 92-6828 Authors Date Jens Chr. Refsgaard, DHI December 1 995 Henrik R. Sarensen, DHI DHV-Consultants BV, NL TNO-lnstitute of Applied Geoscience, NL Water Quality Institute (VKI), DK 1. Kriiger Consultant AS, DK Approved by Royal Veterinary and Agricultural University, DK VUVH - Water Resources Research Institute, SK Jens Chr. Refsgaard VU2H - Research Institute of Irrigation, SK /J^0) ecL T eanvpSad e r GWC - Ground Water Consulting Ltd., SK Comenius University, SK t 1 Final Report an 0 Draft Final Report Revision Description By Checked App. Date Key words Classification Danube, integrated modelling, water resources management, • Open numerical modelling, model development, river and reservoir, ground water, unsaturated zone, agriculture, sediment • Internal transport, ground water quality, surface water quality, ecology, geographical information system, field Ix! Proprietary investigations, equipment.
    [Show full text]
  • Seismic and Geological Conditions at the Bohunice Npp Site
    XA9952599 SEISMIC AND GEOLOGICAL CONDITIONS AT THE BOHUNICE NPP SITE Emilia Juhasova, Dr., Ing., DrSc. Institute of Construction and Architecture, SAS Dubravska cesta 9, 842 20 Bratislava, SLOVAKIA ABSTRACT The paper brings basic information on geological and seismic characteristics of the site of NPP Jaslovske Bohunice, Slovakia. Western Carpathians and Trnava bay geological properties are briefly introduced. The most important macroseismic data and data obtained from field measurements are analysed. Main features of the expected strong seismic motion are discussed. The attention is devoted to local soil characteristics just under the site of NPP. 1. INTRODUCTION The NPP VI, V2, EBO is located in north-west part of Danubian basin - so called Trnava bay, that is nearly 10 km in south-east direction from the mountains of Small Carpathians and in west direction from the Vali river valley. The Trnava bay territory belongs to the best geologically investigated parts of Slovakia. Many deep boreholes were realised here, together with all supporting seismological investigations. This is connected with prospector works and also with construction of important structures as dams, plants, factories, etc. The mentioned territory of EBO was the subject of intensive geological and seismological investigations during the last decade, v The complex synthesising work of all those investigations was done in the closing document of Institute of the Earth Physics AS in Moscow and C-S Institutes [4]. Due to recommendations of [4] the measurements of the seismic activity of near field of NPP were realised by the help of the very sensitive seismic station network. Thanks to obtained data we have nowadays new useful information about the site behaviour and in this way we can do the additional analyses of the safety degree and the measure of upgrading of NPP structures and technologies.
    [Show full text]
  • Meeting Report
    PROCEEDINGS of the 2nd Meeting on the Follow-up of the Joint Statement on Inland Navigation and Environmental Sustainability in the Danube River Basin Zagreb, March 9-10, 2010 INTRODUCTION Background The ICPDR (International Commission for the Protection of the Danube River), the ISRBC (International Sava River Basin Commission) and the DC (Danube Commission) have jointly launched the process to develop the Joint Statement (JS) on Guiding Principles on the Development of Inland Navigation and Environmental Protection in the Danube River Basin (Joint Statement) . After a year-long process preparing the document, and its adoption by the three river commissions in December 2007 and January 2008, the Joint Statement was publicly announced in March 2008. In accordance with the Joint Statement, the ICPDR, Danube Commission, and International Sava River Basin Commission, including relevant stakeholders, shall meet yearly to discuss specific navigational and environmental developments and to highlight good practices in river maintenance projects. The first meeting was held on January 29-30, 2009, in Budapest in the seat of the Danube Commission and on this meeting it was agreed that the second meeting will be held in 2010 in Zagreb. Organization and objectives The meeting was organized by ISRBC together with ICPDR on March 9-10, 2010, in Zagreb. The objectives of the meeting were to: • inform about progress on the implementation of the Joint Statement on Inland Navigation and Environmental Sustainability in the Danube River Basin, • discuss the further development and application of the Joint Statement and its implications (regular information exchange), • inform and discuss new facts and perspectives of European inland waterway transport, • inform and discuss the current state of legal and policy frameworks of integrated river basin management and environmental protection, • inform about the state of IWT projects in the Danube basin.
    [Show full text]
  • 3D Modeling of a Geothermal Reservoir in the Central Part of Kosice Basin in Eastern Slovakia
    3D Modeling of a Geothermal Reservoir in the Central Part of Kosice Basin in Eastern Slovakia Subtitle Katarína Kamenská 3D MODELING OF A GEOTHERMAL RESERVOIR IN THE CENTRAL PART OF KOSICE BASIN IN EASTERN SLOVAKIA Katarína Kamenská A 30 credit units Master’s thesis Supervisors: Dr. Stanislav Jacko Dr. Hrefna Kristmannsdottir Dr. Axel Björnsson A Master’s thesis done at RES │ the School for Renewable Energy Science in affiliation with University of Iceland & the University of Akureyri Akureyri, February 2009 3D Modeling of a Geothermal Reservoir in the Central Part of Kosice Basin in Eastern Slovakia A 30 credit units Master’s thesis © Katarína Kamenská, 2009 RES │ the School for Renewable Energy Science Solborg at Nordurslod IS600 Akureyri, Iceland telephone: + 354 464 0100 www.res.is Printed in 14/05/2009 at Stell Printing in Akureyri, Iceland ABSTRACT The question of energy needed for enhancing human comfort has recently become very popular and geothermal energy, as one of the most promising renewable energy sources, has started to be utilized not only for recreation purposes, but also for heating and probably electricity generation in Slovakia. Slovakia is a country which has proper geological conditions for geothermal source occurrence. Kosice Basin seems to be the most prospective geothermal area – the reservoir rocks are Middle Triassic dolomites with fissure karstic permeability and basal Karpathian clastic rocks at the depth of 2100 – 2600 m, with an average temperature around 135 °C. Seismic data from the central part of Kosice basin enabled the demonstration of position, spatial distribution, morphology and tectonic structure of reservoir rocks and their Neogene overlier as an insulator.
    [Show full text]
  • Performance of the Slovak Economy in Relation to Labor Productivity and Employment
    Available online at www.sciencedirect.com ScienceDirect Procedia Economics and Finance 23 ( 2015 ) 970 – 975 2nd GLOBAL CONFERENCE on BUSINESS, ECONOMICS, MANAGEMENT and TOURISM, 30-31 October 2014, Prague, Czech Republic Performance of The Slovak Economy in Relation to Labor Productivity and Employment Rastislav Kotulica*,Ivana KravcakovaVozarovaa, Jozef Nagya, Emilia Huttmanovaa, a Roman Vavrek aUniversity of Presov in Presov, Faculty of Management, 17. novembra 1, 080 01 Presov, Slovakia Abstract The regions which are located in the European environment have different primary sources, their quality and their level of utilization, which has a direct impact on their performance and subsequent productivity. The aim of this paper is to evaluate the performance and productivity of the Slovak economy in relation to employment in the period from 1995 to 2012. We assume that between employment and performance of the Slovak economy in individual periods is a strong dependence. This analysis confirmed our assumption. The productivity growth of the Slovak economy is directly proportional related to the ability of enterprises to respond successfully to new challenges in the field of innovation and the optimal use of productive resources. The correct interpretation of the results of performance and employment in the national economy can greatly help to clarify the situation on the labor market and thus to diagnose conditions that influence to a greater extent the behaviour of people of working age. © 20152014 TheThe Authors. Authors. Published Published by by Elsevier Elsevier B.V. B.V. This is an open access article under the CC BY-NC-ND license (Selectionhttp://creativecommons.org/licenses/by-nc-nd/4.0/ and/ peer-review under responsibility of).
    [Show full text]
  • Flood Environmental Impact Risk Analysis
    Urban Water Systems & Floods III 3 FLOOD ENVIRONMENTAL IMPACT RISK ANALYSIS MARTINA ZELEŇÁKOVÁ1, MÁRIA ŠUGAREKOVÁ1 & PETER MÉSÁROŠ2 1Department of Environmental Engineering, Technical University of Košice, Slovakia 2Department of Construction Technology and Management, Technical University of Košice, Slovakia ABSTRACT The aim of this paper is to determine the degree of threat in the floodplain of the Hornád river basin and to propose measures that can be used in practice at the time of the flood. The methodology is based on the principle of FEIRA (Flood Environmental Impact Risk Analysis), where the probability and consequence of the negative impact of floods on environmental components is determined on the basis of the analysis of selected stressors. From these indicators, the degree of risk in the Hornád river basin in the event of a flood is subsequently determined. Since there are several industrial sites in the solved area, which can cause extensive pollution of watercourses in case of floods, the work also presents the calculation of the threat according to the point evaluation of pollution sources. The combination of the FEIRA process and the proposed methodology for the assessment of flood environmental damage determined the overall risk of environmental damage due to floods in the Hornád catchment area. This paper is a proposal for measures to protect against floods in the area in case of floods. Keywords: flood, environmental impact analysis, risk analysis, Hornád river basin. 1 INTRODUCTION A wide range of models and case studies are used to assess flood risks. However, internationally, these models have significant economic differences. The authors Jongman et al.
    [Show full text]
  • Univerzita Palackého V Olomouci
    PALACKÝ UNIVERSITY IN OLOMOUC Faculty of Science Department of Ecology and Environmental Sciences Terrestrial isopods in the Western Carpathians Jana Štrichelová A thesis submitted to the Department of Ecology and Environmental Sciences, Faculty of Science, Palacky University, for the degree of Master of Science Supervisor: RNDr. & Mgr. Ivan H. Tuf, Ph.D. Olomouc 2010 © Jana Štrichelová, 2010 ii Štrichelová, J.: Suchozemské rovnakonôţky Západných Karpát. Diplomová práca. Katedra ekologie a ţivotního prostředí PřF UP v Olomouci, 37 strán, anglicky Abstrakt Predloţená diplomová práca sa skladá z dvoch samostatných manuskriptov, pričom obidva pojednávajú o suchozemských rovnakonôţkach v Západných Karpatoch. Prvý manuskript sa zaoberá spoločenstvami suchozemských rovnakonoţiek Bílých Karpát, s ohľadom na ich rozšírenie v Západných Karpatoch. Výskum prebiehal na 26 lokalitách (lesné, lúčne aj zmiešané biotopy) a študovaní ţivočíchovia boli získavaní v období rokov 2003 aţ 2009 pomocou 4 metód odchytu: zemné pasce, tepelná extrakcia pôdnych vzoriek, tepelná extrakcia priesevov opadu a individuálny zber. Celkovo bolo zaznamenaných 16 druhov a boli nájdené bohaté spoločenstvá (7-10 druhov na polovici lokalít). Medzi spoločenstvami obývajúcimi lesy a spoločenstvami lúk a pastvín existujú rozdiely. Armadillidium vulgare a Trachelipus rathkii prevládali na lúkach a pastvinách, zatiaľčo Protracheoniscus politus a Ligidium hypnorum dominovali v lesoch. Najzaujímavejšími faunistickými výsledkami boli nálezy 2 reliktných druhov a to karpatský endemit Hyloniscus mariae a Ligidium germanicum, ktorý má v Českej Republike len ploškovité rozšírenie. V druhom manuskripte sa pojednáva o spoločenstvách suchozemských rovnakonoţiek v dubovo-hrabových lesoch na území Bratislavy. Ţivočíchovia boli zbieraní pomocou metódy priesevu opadu v rokoch 1999, 2000, 2005 a 2006 na 8 lokalitách, pričom väčšina lokaliít prináleţí Malých Karpatom.
    [Show full text]
  • The Species Composition on Agricultural Terraces in Nw Part of Slovakia
    Ekológia (Bratislava) Vol. 33, No. 4, p. 307–320, 2014 doi:10.2478/eko-2014-0029 THE SPECIES COMPOSITION ON AGRICULTURAL TERRACES IN NW PART OF SLOVAKIA IVA MACHOVÁ, KAREL KUBÁT Jan Evangelista Purkyně University in Ústí nad Labem, Faculty of Environment, Králova výšina 7, 400 96 Ústí nad Labem, Czech Republic; e-mail: [email protected] Jan Evangelista Purkyně University in Ústí nad Labem, Faculty of Science, Za Válcovnou 8, 400 96 Ústí nad Labem, Czech Republic; e-mail: [email protected] Abstract Machová I., Kubát K.: The species composition on agricultural terraces in NW part of Slovakia. Ekológia (Bratislava), Vol. 33, No. 4, p. 307–320, 2014. The article contributes to a deeper understanding of agricultural terraces in NW Slovakia. The agri- cultural terraces found in 12 mountain ranges were characterised in detail on 32 localities. The slope parts of the studied terraces are on average only 2.3 m wide and current and former agricultural areas between them are on average 11 m wide. Furthermore, seventy phytosociological relevés were made on the terraces. Overall, 360 species of vascular plants were found in the relevés, 66 of which appeared regularly. The localities were evaluated by DCA analysis. The main factor influencing the species com- position appears to be the geological composition of the bedrock and, probably, the altitude as well. High coverage of the herb layer (median value 95%), low coverage of the shrub layer (median value 5%) and the absence or a very low coverage of the tree layer is typical for these terraces. Key words: NW Slovakia, agricultural terraces, vascular plants species, properties of the terraces.
    [Show full text]
  • Pišút, P.1 – Falťan, V.1 – Chovanec, P.1 – Petrovič, F.3
    Horáčková et al.: Historical changes and vegetation development after intensive peat extraction in the lowland mires of Slovakia - 5025 - HISTORICAL CHANGES AND VEGETATION DEVELOPMENT AFTER INTENSIVE PEAT EXTRACTION IN THE LOWLAND MIRES OF SLOVAKIA HORÁČKOVÁ, Š.1,2* – PIŠÚT, P.1 – FALŤAN, V.1 – CHOVANEC, P.1 – PETROVIČ, F.3 1Department of Physical Geography and Geoecology, Faculty of Natural Sciences, Comenius University in Bratislava, Ilkovičova 6, 84215 Bratislava 4, Slovakia (e-mails: [email protected], [email protected], [email protected]) 2Geographical Institute, Slovak Academy of Sciences Štefánikova 49, 81473 Bratislava, Slovakia 3Department of Ecology and Environmental Sciences, Faculty of Natural Sciences, Constantine the Philosopher University in Nitra, Trieda A. Hlinku 1, 94974 Nitra, Slovakia (e-mail: [email protected]) *Corresponding author e-mail: [email protected] (Received 10th May 2018; accepted 5th Jul 2018) Abstract. Mires in the Danubian Lowland (Northern part of the Pannonian Basin) are typically overgrown with common alder (Alnus glutinosa). Similar stands at this location are unfortunately very rare, what is caused by continuous human intervention in landscape and its natural pattern from Early Holocene. Peatland degradation near Pusté Úľany village started in the mid - eighteenth century, what is supported by historical maps. In the previous century a huge peat extraction took place at this specific mire. Despite these anthropogenic changes, there are still some remnants of natural habitats present, mostly dependant on ground water level. Methodology includes historical map’s analysis, digital terrain model and vegetation cover mapping. Actual map of biotopes was completed for the current state of the vegetation cover acquaintance.
    [Show full text]
  • Impact of Foreign Direct Investment on the Economy of Slovakia
    NATIONAL BANK OF SLOVAKIA Adela Hošková IMPACT OF FOREIGN DIRECT INVESTMENT ON THE ECONOMY OF SLOVAKIA National Bank of Slovakia Institute of Monetary and Financial Studies Bratislava 2001 IMPACT OF FOREIGN DIRECT INVESTMENT ON THE ECONOMY OF SLOVAKIA © National Bank of Slovakia, Institute of Monetary and Financial Studies Adela Hošková. Bratislava 2001 2 Table of Contents Page INTRODUCTION 4 1. Foreign Direct Investment (FDI) in Slovakia 8 1.1 Inflow of Foreign Direct Investment 8 1.2 Outflow of Foreign Direct Investment 12 2. Impact on Balance of Trade and Payments 14 3. Regional Aspects of FDI in Slovakia 17 4. Impact of FDI on Employment, Labour Productivity and Know-How 27 5. Partnership Between FDI and Domestic Industry 36 CONCLUSION 44 REFERENCES 47 3 IMPACT OF FOREIGN DIRECT INVESTMENT ON THE ECONOMY OF SLOVAKIA According to the latest results, the inflow of foreign direct investment (FDI) to Slovakia has started to gain importance. It is therefore important to understand the impact of FDI on the economy of Slovakia, primarily on the real sector, banking, third sector, etc. This study aims to depict the impact of FDI on selected production areas, i.e. employment, labour productivity, know-how, partnership between FDI and domestic industry, and regional distribution of FDI. The final positives (and/or negatives) boil down to the impact on the balance of trade and payments of the SR, as a result of the capitalisation of pro-export oriented organisations, which sell their output (because of the small size of the Slovak market) in foreign countries, by means of FDI.
    [Show full text]
  • Ore Geology of the Copper Sulfide Mineralization in the Rudabánya Ore-Bearing Complex
    Central European Geology DOI: 10.1556/24.59.2016.005 Ore geology of the copper sulfide mineralization in the Rudabánya ore-bearing complex Norbert Németh*, János Földessy, Judit Turi Institute of Mineralogy and Geology, Faculty of Earth Science and Engineering, University of Miskolc, Miskolc, Hungary Received: July 18, 2016; accepted: September 21, 2016 The mineralized complex of Rudabánya hosts deposits of several mineral resources including base metal ores. Recent exploration provided new information on the enrichment of copper within this complex. The primary copper mineralization consists of sulfides. The paragenetic sequence starts with fahlore, continues with bornite, and concludes in chalcopyrite formation partly replacing the former phases. It is hosted by brecciated carbonate rocks, overprinting the paragenesis of the iron metasomatism. It was found to be spatially separated from zinc and lead enrichments. Oxidation and a subsequent new pulse of mineralization formed several new copper, zinc, and lead minerals, probably by the remobilization of the primary parageneses. Keywords: base metal ore, bornite, chalcopyrite, fahlore, North Hungary, sediment hosted ore Introduction Rudabánya is a historic mining town in NE Hungary. Documented medieval mining activities were targeted on copper and silver ore cropping out in a hill range extending northeastward of the town. Beginning with the 19th century, iron ores attracted the mining entrepreneurs. Limonite, later also siderite ore, was exploited both with opencast and underground mining.
    [Show full text]
  • Monitoring of the Eurasian Lynx (Lynx Lynx) in the Vtáčnik Mountains, Slovakia: Importance for the National and European Management and Conservation of the Species
    MONITORING OF THE EURASIAN LYNX (LYNX LYNX) IN THE VTÁČNIK MOUNTAINS, SLOVAKIA: IMPORTANCE FOR THE NATIONAL AND EUROPEAN MANAGEMENT AND CONSERVATION OF THE SPECIES KUBALA JAKUB, BRANISLAV TÁM, NUNO FILIPE GUIMARÃES, ĽUBOMÍR FERLICA, TIBOR PATAKY, PETER KLINGA, PETER KOVÁČ, MICHAL BELÁK, EVA GREGOROVÁ, PETER SMOLKO, STJEPAN STOPIĆ, LUKÁŠ HOLÁSEK, PETER GRMAN, PETER HOLKA, BEŇADIK MACHCINÍK, JAROSLAV BRNDIAR, MIRKO KRAJČI & RUDOLF KROPIL Technical University in Zvolen, September 2020 Monitoring of the Eurasian lynx (lynx lynx) in the Vtáčnik Mountains, Slovakia: importance for the national and European management and conservation of the species The publication was developed as part of the LIFE Lynx project “Preventing the Extinction of the Dinaric-SE Alpine Lynx Population through Reinforcement and Long-term Conservation" (LIFE16 NAT / SI / 000634) with financial support from the European Commission Authors: Jakub Kubala – Technical university in Zvolen, Zvolen, Slovakia, Branislav Tám – Bojnice National Zoo, Bojnice, Slovakia; Slovak University of Agriculture in Nitra, Nitra, Slovakia, Nuno Filipe Guimarães – OZ DIANA – Carpathian wildlife research, Slovakia, Ľubomír Ferlica – Technical university in Zvolen, Zvolen, Slovakia, Tibor Pataky – Technical university in Zvolen, Zvolen, Slovakia, Peter Klinga – Technical university in Zvolen, Zvolen, Slovakia, Peter Kováč – OZ DIANA – Carpathian wildlife research, Slovakia, Michal Belák – Bojnice National Zoo, Bojnice, Slovakia, Eva Gregorová – Bojnice National Zoo, Bojnice, Slovakia, Peter Smolko
    [Show full text]