Primeval Beech Forests of the Carpathians Slovakia
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Project Agreement
13/2012 Swiss Contribution - Cooperation Programme between Switzerland and the Slovak Republic THE SWISS-SLOVAK COOPERATION PROGRAMME PROJECT AGREEMENT BETWEEN SWITZERLAND REPRESENTED BY THE SWISS AGENCY FOR DEVELOPMENT AND COOPERATION (SDC) AND THE SLOVAK REPUBLIC REPRESENTED BY THE GOVERNMENT OFFICE OF THE SLOVAK REPUBLIC ON THE GRANT FOR THE PROJECT “ZEMPLINSKE HAMRE – DISCOVERING HISTORY OF MINING AND IRON SMELTING IN VIHORLAT MOUNTAINS” TO BE IMPLEMENTED DURING THE PERIOD 23.02.2012 – 30.04.2014 1 13/2012 Swiss Contribution - Cooperation Programme between Switzerland and the Slovak Republic Switzerland and the Slovak Republic Having regard to the friendly relations between the two countries, Desirous of strengthening these relations and the fruitful co-operation between the two countries, Intending to promote further the social and economic development in the Slovak Republic, Referring to the Framework Agreement between the Swiss Federal Council and the Government of the Slovak Republic concerning the implementation of the Swiss-Slovak cooperation programme to reduce economic and social disparities within the enlarged European Union, concluded on 20 December 2007, Considering the Swiss Grant for ZEMPLINSKE HAMRE – discovering history of mining and iron smelting in Vihorlat Mountains, Slovak Republic, have agreed as follows: Article 1 Definitions In this Project Agreement, unless the context otherwise requires, the following terms shall have the following meaning: - "Audit Authority" means the Slovak entity performing the compliance audit and ensuring the execution of system audits and audits of operation within the Swiss-Slovak Cooperation Programme pursuant to the Framework Agreement; - "National Coordination Unit" (hereinafter referred to as "NCU") means the Slovak unit in charge of the coordination of the Swiss-Slovak Cooperation Programme. -
Introduction the Genus Aconitum L. (Ranunculaceae Juss.) Is an Interesting Taxonomical Group Which Is Characterized by High Leve
Modern Phytomorphology 9 (Suppl.): 35–73, 2016 SOME NOTES ON THE GENUS ACONITUM IN CHORNOHOra MTS. Andrew V. Novikoff 1*, Józef Mitka 2, Alexander Kuzyarin 1, Oleg Orlov 1, Marina Ragulina 1 Abstract. The paper is a contribution to ecology and chorology ofAconitum in high-mountain zone of the Ukrainian Carpathians. It was confirmed that genusAconitum in the Chornogora mountain range is represented by 14 taxa, and 7 more taxa were listed as potential for this region. These taxa belong to 3 subgenera and are divided on 4 main biomorphological groups delimited on the base of their habitat, life form, ecology and altitudinal distribution. The soil and vegetation types for all taxa have been identified and the maps of their distribution have been prepared. The most influent threats and their categories were identified. Threat category for A. × nanum was changed from DD to VU, and for A. firmum subsp. fussianum from NT to VU. Key words: Aconitum, Chornogora, sozology, ecology, chorology, soils, vegetation 1 State Natural History Museum NAS of Ukraine, Teatralna str. 18, 79008 Lviv, Ukraine; * [email protected] 2 Institute of Botany of Jagiellonian University, Botanical Garden, Jagiellonian University, Kopernika 27, 31-501 Kraków, Poland; [email protected] Introduction (19 confirmed + 3 unconfirmedAconitum taxa) 9 species and subspecies are listed as clearly The genusAconitum L. (Ranunculaceae endemic or subendemic and 2 more hybrid Juss.) is an interesting taxonomical group which subspecies are considered as probably endemic is characterized by high level of morphological (Novikoff & Hurdu 2015). From other side, diversity, presence of a number of subspecific if we consider all forms and varieties then we taxa, and high number of both infra- and can tell about 17 subendemic and endemic taxa interspecific natural hybrids Gáyer( 1922; in general. -
International Student´S Guide to Slovakia
International Student´s Guide to Slovakia This publication was produced within the National Scholarship Programme of the Slovak Republic funded by the Ministry of Education, Science, Research and Sport of the Slovak Republic and within the Lifelong Learning Programme/Erasmus funded by the European Commission and the Ministry of Education, Science, Research and Sport of the Slovak Republic. This publication reflects the views only of the author, and the Commission cannot be held responsible for any use which may be made of the information contained therein. International Student’s Guide to Slovakia 3rd edition Published by: SAIA, n. o. ❘ Námestie slobody 23 ❘ 812 20 Bratislava 1 ❘ Slovakia SAAIC ❘ Svoradova 1 ❘ 811 03 Bratislava ❘ Slovakia Updated by: Ivana Matulíková and Jana Rehorovská in cooperation with Eva Balažovičová, Michal Fedák, Denisa Filkornová, Katarína Košťálová Graphic design and press: Peter Sedláčik and Marek Mikuláši — 77.production © SAIA, n. o. & SAAIC December 2010 ISBN: 978 — 80 — 89517 — 00 — 8 2 hello ahoj 3 CONTENT I. ABOUT SLOVAKIA 6 1. Slovakia in Brief 6 2. Geography 8 3. Political System and State Bodies 9 4. Religion 11 5. Slovak UNESCO Natural and Cultural Heritage 12 6. Famous Slovaks 14 II. HIGHER EDUCATION IN SLOVAKIA 19 1. Oldest Slovak Universities 19 2. Higher Education Institutions 20 3. Organisation and Structure of Studies 29 4. Admission and Tuition Fee 32 5. Recognition of Diplomas and Qualifications 34 6. Slovak Language Courses for International Students 37 7. Student Organisations 39 8. Student Cards 41 III. GRANTS AND SCHOLARSHIPS 42 1. Funding Based on Slovak Sources 42 2. Funding for Bilateral Cooperation 46 3. -
109 Since 1961 Paleocene Deposits of the Ukrainian Carpathians
since 1961 BALTICA Volume 33 Number 2 December 2020: 109–127 https://doi.org/10.5200/baltica.2020.2.1 Paleocene deposits of the Ukrainian Carpathians: geological and petrographic characteristics, reservoir properties Halyna Havryshkiv, Natalia Radkovets Havryshkiv, H., Radkovets, N. 2020. Paleocene deposits of the Ukrainian Carpathians: geological and petrographic char- acteristics, reservoir properties. Baltica, 33 (2), 109–127. Vilnius. ISSN 0067-3064. Manuscript submitted 27 February 2020 / Accepted 10 August 2020 / Published online 03 Novemver 2020 © Baltica 2020 Abstract. The Paleocene Yamna Formation represents one of the main oil-bearing sequences in the Ukrai- nian part of the Carpathian petroleum province. Major oil accumulations occur in the Boryslav-Pokuttya and Skyba Units of the Ukrainian Carpathians. In the great part of the study area, the Yamna Formation is made up of thick turbiditic sandstone layers functioning as reservoir rocks for oil and gas. The reconstructions of depositional environments of the Paleocene flysch deposits performed based on well log data, lithological and petrographic investigations showed that the terrigenous material was supplied into the sedimentary basin from two sources. One of them was located in the northwest of the study area and was characterized by the predomi- nance of coarse-grained sandy sediments. Debris coming from the source located in its central part showed the predominance of clay muds and fine-grained psammitic material. The peculiarities of the terrigenous material distribution in the Paleocene sequence allowed singling out four areas with the maximum development (> 50% of the total section) of sandstones, siltstones and mudstones. The performed petrographic investigations and the estimation of reservoir properties of the Yamna Formation rocks in these four areas allowed establishing priority directions of further exploration works for hydrocarbons in the study territory. -
East Slovakian Lowland and Its Economical Utilization
Eastern Slovakian lowland and its economical utilization Matias Luostarinen, Teppo Tossavainen, Peter Popovic, Zuzana Baronova, Adria Vila Cufi, Miquel Romero Carrera Contents Introduction ....................................................................................................................................................... 3 Landscapes of the region ................................................................................................................................... 4 Regions identity and regional identity in the landscape ................................................................................... 5 Sources and methods of analysis ...................................................................................................................... 6 Physical geographical characteristics of the territory ....................................................................................... 7 The human geography of the Eastern Slovak Lowland ................................................................................... 13 Tokaj region in Slovakia ................................................................................................................................... 14 Conflict for brand Tokaji .................................................................................................................................. 19 Differences between the Tokaj region of Hungary and Slovakia .................................................................... 20 References ...................................................................................................................................................... -
World Bank Document
_____ /3 /00 714T!hb' / W N' 'C N, 2' "K / 2"' $ / N S '¾ "Ky" 7 N, 2 / '-7. Public Disclosure Authorized Y 7' >2 "2'N < « N N 7" '- "'N7' C. 7. '7"" ¾ 4vY> ;">2; \ 2'$4NN, N)' ' / -. ' ½ 'Wanscarpathian Bio4htersitrIbM 4 ctioni Pe4ect S t * ' C / ' N A "K ' / "'>2 , "14 I / '-<Kr) Public Disclosure Authorized 7 K ,K.t / N -' C? / C, N / <4 / * / ' " K N Public Disclosure Authorized 7¾ 77$ C> 7' N / / '-•1' / ProjectDocument N July1993 >7 A A 4 "C. N - Public Disclosure Authorized / / N. 'N. *C' * ' 7 7 / N 4 V ' '>7 K'> .' C " THS WORLDOANk N N ' 4?' <KX' GEF Docume'ntation The Global Environment F-acility(GEPi assistsdeveloping countries to protect theglobal environment infour areas,:'global, warming, pollution of internationalwaters, destructionofbiodiversity, and depletion ofthe ozone layer. The GEF isjointly implemented, V bytheUnited Nations Development Programme, theUnited Nations Environment Programme, andthe World.Bank. GEF Working Papers - identifiedby the burgundy band on their Govers - provide' generalinformation onthQ Facility's work and miore specific information onmethodological approaches,scientific and technical issues, and policy anid strategic rnatters. GEF Proje-ct Documents - identified,bya green band 7 provide'extendedproject- specificinformation. The impleme-nting agency.responsible foreach project is identifiedby its logoon the cover of the document. Reports by the Chairman - identifiedby a blueband - areprepared by the Off ice of theGEF Administrator in collaboration with fth-'three GEF imple'menting agencies for the biannualParticipants' Meetings. TheGEF Administrator 1818,H Street, NW Washington,DC 20433 USA Telephone:(202) 473-1053 Fax:(202) 477-0551 CURRENCYEQUIVALENT (April 1993) 2,690 Karbovanets(Kb) = US$ 1 WEIGHTS AND MEASURES The metric system is used throughoutthis report. -
UNESCO List of World Heritage Sites in Slovakia
UNESCO list of World Heritage Sites in Slovakia Several of our cultural and natural properties were inscribed into the UNESCO’s World Heritage List. Bardejov and Banská Štiavnica's historical centre and its technical monuments, Spiš Castle- the biggest castle in central Europe, Vlkolínec Village with its wooden houses documenting our traditions and culture, wooden churches situated in eastern Slovakia are just examples of our historical monuments inscribed into the List. We would like to mention some natural treasures from the UNESCO List: unique caves lying in Slovak Paradise, Oak Primaeval Forest in North-East Slovakia. On the other hand, there are some treasures waiting to be inscribed into the List: Gothic wooden altar chiseled out by Master Pavol from Levoča, Limes Romanus-an ancient Rome’s border defence system or Tokai vineyards. Brief Description Spišský Hrad has one of the largest ensembles of 13th and 14th century military, political and religious buildings in eastern Europe, and its Romanesque and Gothic architecture has remained remarkably intact. The extended site features the addition of the historic town-centre of Levoča founded in the 13th and 14th centuries within fortifications. Most of the site has been preserved and it includes the 14th century church of St James with its ten alters of the 15th and 16th centuries, a remarkable collection of polychrome works in the Late Gothic style, including an 18.6 metre high alterpiece by completed around 1510 by Master Paul. Spissky castle, view from Drevenik Outstanding Universal Value The castle of Spišský Hrad, the town of Levoča, the associated sites in Spišské Podhradie, Spišská, Kapitula, and Ţehra constitute a remarkable group of military, urban, political, and religious elements, of a type that was relatively common in medieval Europe, but of which almost none have survived in such a complete condition with equivalent integrity. -
Background and Introduction
Chapter One: Background and Introduction Chapter One Background and Introduction title chapter page 17 © Libor Vojtíšek, Ján Lacika, Jan W. Jongepier, Florentina Pop CHAPTER?INDD Chapter One: Background and Introduction he Carpathian Mountains encompass Their total length of 1,500 km is greater than that many unique landscapes, and natural and of the Alps at 1,000 km, the Dinaric Alps at 800 Tcultural sites, in an expression of both km and the Pyrenees at 500 km (Dragomirescu geographical diversity and a distinctive regional 1987). The Carpathians’ average altitude, how- evolution of human-environment relations over ever, of approximately 850 m. is lower compared time. In this KEO Report, the “Carpathian to 1,350 m. in the Alps. The northwestern and Region” is defined as the Carpathian Mountains southern parts, with heights over 2,000 m., are and their surrounding areas. The box below the highest and most massive, reaching their offers a full explanation of the different delimi- greatest elevation at Slovakia’s Gerlachovsky tations or boundaries of the Carpathian Mountain Peak (2,655 m.). region and how the chain itself and surrounding areas relate to each other. Stretching like an arc across Central Europe, they span seven countries starting from the The Carpathian Mountains are the largest, Czech Republic in the northwest, then running longest and most twisted and fragmented moun- east and southwards through Slovakia, Poland, tain chain in Europe. Their total surface area is Hungary, Ukraine and Romania, and finally 161,805 sq km1, far greater than that of the Alps Serbia in the Carpathians’ extreme southern at 140,000 sq km. -
Developing the GIS-Based Maps of the Geomorphological and Phytogeographical Division of the Ukrainian Carpathians for Routine Use in Biogeography
Biogeographia – The Journal of Integrative Biogeography 36 (2021): a009 https://doi.org/10.21426/B636052326 Developing the GIS-based maps of the geomorphological and phytogeographical division of the Ukrainian Carpathians for routine use in biogeography ANDRIY NOVIKOV Department of Biosystematics and Evolution of the State Natural History Museum of the NAS of Ukraine, Teatralna str. 18, 79008 Lviv (Ukraine) email: [email protected] Keywords: biogeography, mesoregional division, shapefile, Ukrainian Carpathians. SUMMARY The paper introduces GIS-based maps of the geomorphological and phytogeographical division of the Ukrainian Carpathians (a part of Eastern Carpathian Mts.), which were developed for routine use in biogeography and based on the consolidation of the existing publications. The map of the geomorphological division includes 57 OGUs (operational geographic units), and the map of the phytogeographical division – 18 OGUs of the lowest rank. Geomorphological units are supported with available synonyms, which should help in work with different topic-related Ukrainian publications. Both maps follow strict hierarchical classification and are briefly discussed. INTRODUCTION Tsys (1962, 1968) published the first The Ukrainian Carpathians (UC) is part of the complete geomorphologic division of the UC. Eastern Carpathian mountain province Besides five mountainous regions, this division (Kondracki 1989), artificially delimited by the also included adjacent foothills and lowlands western border of Ukraine and covering about (Ciscarpathia and Transcarpathia) and 24,000 km2. In general, these are not high comprised 36 districts. Such regionalization of mountains – only seven peaks of the UC the UC was further developed by many slightly exceed 2000 m of elevation, and all Ukrainian scientists (Herenchuk 1968, these peaks, including the highest point of Marynych et al. -
Western Carpathians, Poland)
Geological Quarterly, 2006, 50 (1): 169–194 Late Jurassic-Miocene evolution of the Outer Carpathian fold-and-thrust belt and its foredeep basin (Western Carpathians, Poland) Nestor OSZCZYPKO Oszczypko N. (2006) — Late Jurassic-Miocene evolution of the Outer Carpathian fold-and-thrust belt and its foredeep basin (Western Carpathians, Poland). Geol. Quart., 50 (1): 169–194. Warszawa. The Outer Carpathian Basin domain developed in its initial stage as a Jurassic-Early Cretaceous rifted passive margin that faced the east- ern parts of the oceanic Alpine Tethys. Following closure of this oceanic basin during the Late Cretaceous and collision of the Inner Western Carpathian orogenic wedge with the Outer Carpathian passive margin at the Cretaceous-Paleocene transition, the Outer Carpathian Basin domain was transformed into a foreland basin that was progressively scooped out by nappes and thrust sheets. In the pre- and syn-orogenic evolution of the Outer Carpathian basins the following prominent periods can be distinguished: (1) Middle Juras- sic-Early Cretaceous syn-rift opening of basins followed by Early Cretaceous post-rift thermal subsidence, (2) latest Creta- ceous-Paleocene syn-collisional inversion, (3) Late Paleocene to Middle Eocene flexural subsidence and (4) Late Eocene-Early Miocene synorogenic closure of the basins. In the Outer Carpathian domain driving forces of tectonic subsidence were syn-rift and thermal post-rift processes, as well as tectonic loads related to the emplacement of nappes and slab-pull. Similar to other orogenic belts, folding of the Outer Carpathians commenced in their internal parts and progressed in time towards the continental foreland. This process was initi- ated at the end of the Paleocene at the Pieniny Klippen Belt/Magura Basin boundary and was completed during early Burdigalian in the northern part of the Krosno Flysch Basin. -
Principal Features of Chornohora Climate (Ukrainian Carpathians) ISSN 2080-7686
Bulletin of Geography. Physical Geography Series, No. 17 (2019): 61–76 http://dx.doi.org/10.2478/bgeo-2019-0015 Principal features of Chornohora climate (Ukrainian Carpathians) ISSN 2080-7686 Krzysztof Błażejczyk* 1, Oleh Skrynyk2 1Polish Academy of Sciences, Warsaw, Poland 2University of Warsaw, Poland * Correspondence: Polish Academy of Sciences, Warsaw, Poland. E-mail: [email protected] https://orcid.org/0000-0002-0439-6642 Abstract. Chornohora is the highest mountain ridge in the Ukrainian Carpathians with 6 peaks of an altitude over 2,000 m above sea level (Hoverla is the highest peak, 2,061 m a.s.l). its climate is explored less than other mountain ridges in Europe. The massif is a climatic barrier for air mass- es on NW-SE line. To describe the climate of this area data from the weather station at Pozhyzhevs- ka alpine meadow for the years 1961-2010 were used. The seasonal and long-term variability of air temperature, atmospheric precipitation and snow cover were investigated on the background of air circulation types. The results show that general features of Chornohora climate depend both, on el- Key words: evation above sea level and on air circulation. Lowest temperature is observed at N-NE circulation Chornohora, and highest precipitation – at western air inflow. Long-term changes of examined climate elements Eastern Carpathians, in Chornohora show significant increase in mean (0.13°/10 years) and minimum (0.22°C/10 years) air air circulation, temperature as well as in snow cover depth and number of snowy days. mountain climate, climate changes Introduction were published in yearbooks of “Kosmos” journal (Szulc 1911, 1912). -
Ukrainian Carpathians (12 Days)
Ukrainian Carpathians (12 days) This 12-day walking tour will give you a possibility to visit the main areas of the Ukrainian Carpathians. You will learn not only about rich and wild nature but also about culture and everyday life of people who inhabit this region of Ukraine, full of numerous historic and architectural monuments, wooden churches which you can’t find anywhere else in Ukraine. Boykys, hutsuls, pidhoryans – these are the ethnic groups of Ukrainians who inhabit the territory this route goes through. The program will suit those who would like to learn more in a short period of time as we suggest an intense excursion program and trekking in mountains with mountaineering the highest peaks of Ukraine. Season: May - October Program Day 1 Meeting of the group in Lviv. Breakfast. Lviv – a 3-hour tour around one of the main cultural centres of Ukraine – the Assumption Church (Uspinnya) and Three Saints Chapel, the Dominican Cathedral, the Rynok Square – the heart of the city (Renaissance period), the City Hall (Ratusha), the Latin Cathedral with the Chapel, the ancient Armenian quarter and the Armenian Cathedral, the Liberty avenue (Prospekt Svobody), the Opera House, Town Arsenal – a part of the city’s original fortification system. Accommodation at a hotel. Dinner. Day 2 Skolivski Beskydy (Lviv region). Breakfast. Journey to the Carpathians (Skolivski Beskydy). Visiting the Rocks of Oleksa Dovbush (caves and rocks complex) – a stone maze full of the ravines, secret passages and paths, formed by the huge rocks and stones reminding the mysterious creatures (1 - 2 hour walk). Urych – the historic-cultural reserve “Tustan” – the Old Rus’ defense complex, the museum of the fortress history.