Transboundary Protected Areas Cooperation in the East Carpathian and Carpathian Biosphere Reserves
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Population in the Slovak Carpathian Mountains
Monitoring protocol for the Eurasian lynx (Lynx lynx) population in the Slovak Carpathian Mountains A1. Assessment and selection of sites and lynx for live-capture from the Carpathian source population in Slovakia D1. Monitoring the effects of lynx removal for translocations on the source populations Authors: Kubala J. Smolko P. Klinga P. Tám B. & Kropil R. September 2018 Report for the implementation of action A1 and D1 Realized in the frame of action A1: Assessment and selection of sites and lynx for live-capture from the Carpathian source population in Slovakia Authors: Kubala J. Smolko P. Klinga P. Tám B. & Kropil R. Content 1. Introduction…………………………………………………………………………….5 2. Objectives and attributes……………………………………………………………….7 3. Survey areas…………………………………………………………………………....7 4. Aims and principles of monitoring……………………………………………………11 5. What will be monitored?................................................................................................11 6. Monitoring network…………………………………………………………………...14 7. Passive monitoring: Collecting a chance (opportunistic information)………………..14 8. Active monitoring: Systematic surveys and monitoring system………………………15 8.1. Snow tracking………………………………………………………………………...15 8.2. Opportunistic and standardized collection of samples for genetic analysis…………..16 8.3. Camera trapping………………………………………………………………….......16 8.3.1. Opportunistic camera trapping……………………………………………………17 8.3.2. Deterministic camera trapping………………………………………………….....18 8.4. Captures and GPS/GSM telemetry…………………………………………………...20 9. Survey, monitoring and capture time-frame…………………………………………..22 References…………………………………………………………………………………….23 Foreword The purpose of this protocol is to provide detailed information about the objectives, attributes, sampling design and data management necessary for the implementation of the actions A1 and D1 within the LIFE LYNX - LIFE16 NAT/SI/000634 Together with the protocol on the A2 action in the Romanian Carpathians - Gazzola et al. (2018) it is required by the need to ensure a technical framework for the LIFE Lynx project team. -
Guidelines for Wildlife and Traffic in the Carpathians
Wildlife and Traffic in the Carpathians Guidelines how to minimize the impact of transport infrastructure development on nature in the Carpathian countries Wildlife and Traffic in the Carpathians Guidelines how to minimize the impact of transport infrastructure development on nature in the Carpathian countries Part of Output 3.2 Planning Toolkit TRANSGREEN Project “Integrated Transport and Green Infrastructure Planning in the Danube-Carpathian Region for the Benefit of People and Nature” Danube Transnational Programme, DTP1-187-3.1 April 2019 Project co-funded by the European Regional Development Fund (ERDF) www.interreg-danube.eu/transgreen Authors Václav Hlaváč (Nature Conservation Agency of the Czech Republic, Member of the Carpathian Convention Work- ing Group for Sustainable Transport, co-author of “COST 341 Habitat Fragmentation due to Trans- portation Infrastructure, Wildlife and Traffic, A European Handbook for Identifying Conflicts and Designing Solutions” and “On the permeability of roads for wildlife: a handbook, 2002”) Petr Anděl (Consultant, EVERNIA s.r.o. Liberec, Czech Republic, co-author of “On the permeability of roads for wildlife: a handbook, 2002”) Jitka Matoušová (Nature Conservation Agency of the Czech Republic) Ivo Dostál (Transport Research Centre, Czech Republic) Martin Strnad (Nature Conservation Agency of the Czech Republic, specialist in ecological connectivity) Contributors Andriy-Taras Bashta (Biologist, Institute of Ecology of the Carpathians, National Academy of Science in Ukraine) Katarína Gáliková (National -
The Carpathian Mountains: a Refuge for Wildlife and a “Paradise” for the People of Slovakia by Ted Bailey
Refuge Notebook • Vol. 7, No. 30 • August 5, 2005 The Carpathian Mountains: A refuge for wildlife and a “paradise” for the people of Slovakia by Ted Bailey Although the fireweed was in bloom and brown half the size of state of Kentucky. It is also a relatively bears, wolves, lynx roamed the surrounding forests; new country having gained its most recent indepen- we were not hiking on the Kenai Peninsula or even in dence a mere twelve years ago after the collapse of Alaska. Despite the similarities we were thousands of the Soviet Union. And Slovakia joined the European miles away in Central Europe’s Carpathian Mountains Union in 2004 only a year ago. The huge, stark, tall and in eastern Slovakia. My wife, daughter and I had trav- gray housing complexes built in the country’s largest eled here in July to find four little villages where my cities of Bratislava and Kosice during the communist grandparents lived over a hundred years ago before era contrasted with the beautifully restored old city they emigrated at a young age to America in search centers where Gothic cathedrals and old palaces are of a better life. We eventually found the villages as attractions for visitors. we traveled by car throughout the eastern regions of One day we hiked a trail into the Slovensky Raj, Slovakia known as Spis and Zemplin. Spis is a moun- one of nine national parks and fourteen protected na- tainous region that borders the southern boundary of ture territories in Slovakia. The park was the first pro- Poland. -
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. -
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. -
Saving the Green Heart of Europe
© WILD WONDERS OF E UROPE / CORNELIA ANNUA ANNUAL REVIEW D OERR / WW L REVIE DCP F W 2013 2013 SAVING WW THE GREEN HEART F . PAN OF EUROPE D A WWF Danube-Carpathian Programme . ORG July 2012–June 2013 FY2013 Annual Review – WWF Danube-Carpathian Programme FY2013 Annual Review – WWF Danube-Carpathian Programme A STRUGGLE FOR 15 YEARS THE GREEN HEART OF EUROPE IN THE REGION ”Last year, thousands of Bulgarians poured into the streets in The Danube River basin is the most international river basin protest over amendments to the Forest Law. Now, thousands of in the world, draining 18 countries on its 2,800 km journey Romanians are thronging the streets of Bucuresti and other from the Black Forest in Germany to the Black Sea. From cities outraged over the Romanian government’s abrupt approval the largely untamed middle and lower stretches of the river of gold mining at Rosia Montana. to the spectacular Danube Delta at its mouth, the Danube is home to some of the richest wetland areas in Europe and the The protests at Eagle’s Bridge in Sofia finally convinced the government to amend world. legislation that would have opened the country’s protected forests to development and facilitated corruption; it is still unclear what effect the protests in Romania will have on The Carpathian Mountains, arching across seven countries the Parliament’s final decision regarding gold mining with cyanide in a valuable area of from the Czech Republic across Poland, Slovakia, Ukraine the Carpathian Mountains. “Our goal is to work The two incidents brought into sharp focus a struggle over the future of the re- with others to secure the and Hungary, and down to Romania and the tip of Serbia, gion’s natural riches and the close link to good governance. -
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. -
Contemporary Geomorphic Processes in the Polish Carpathians Under Changing Human Impact
21 by Adam Lajczak1, Wlodzimierz Margielewski2, Zofia Raczkowska3 Jolanta Swiechowicz4 Contemporary geomorphic processes in the Polish Carpathians under changing human impact 1 Pedagogical University, Institute of Geography, 2 Podchorazych Str., 30-084 Cracow, Poland. E-mail: [email protected] 2 Polish Academy of Sciences, Institute of Nature Conservation, 33 A. Mickiewicza Ave., 31-120 Cracow, Poland 3 Polish Academy of Sciences, Institute of Geography and Spatial Organization, 22 Sw. Jana Str., Cracow, Poland 4 Jagiellonian University in Krakow, Institute of Geography and Spatial Management, 7 Gronostajowa Str., 30-387 Cracow, Poland The paper presents activity of contemporary The Polish Carpathians are relatively densely populated (127 2 geomorphic processes in the Polish Carpathians, taking persons/km ), and more than 65% of the population live in rural areas (Dlugosz and Soja, 1995). For this reason man exerts a strong into account human impact on relief transformation in influence on the course of geomorphic processes, but recent processes the past several centuries. and their effects also pose a threat to man. According to Slaymaker Landsliding in the flysch Carpathians is a principal (2010), human activity is a key driver in present-day landscape process in slope transformation, posing the most serious evolution in mountain areas. threat to man, both in the mountains and the foothills. The aim of this paper is to present such mutual relationships within areas showing four types of relief, indicating the most important On the other hand, unsuitable housing on slopes initiates process, type of geomorphic hazard and type and effect of human mass movements, frequently with catastrophic influence on relief transformation, as well as tendencies in these consequences. -
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). -
Relief Evolution of Landslide Slopes in the Kamienne Mts (Central Sudetes, Poland) – Analysis of a High-Resolution DEM from Airborne Lidar
Contemp.Trends.Geosci., 7(1),2018,1-20 DOI: 10.2478/ctg-2018-0001 Relief evolution of landslide slopes in the Kamienne Mts (Central Sudetes, Poland) – analysis of a high-resolution DEM from airborne LiDAR Aleksandra Osika*, Małgorzata Wistuba, Ireneusz Malik Faculty of Earth Sciences, University of Silesia in Katowice, Bedzinska 60, 41-200 Sosnowiec, Poland * corresponding author: [email protected] Received: 5th November, 2017 Accepted: 9th January, 2018 Abstract The aim of the study is to reconstruct the development of landslide relief in the Kamienne Mountains (Central Sudetes, SW Poland) based on a DEM from LiDAR data. Analyses of relief and geological maps in ArcGIS 10.5 and of slope cross-sections in Surfer 14 allowed to distinguish different types of landslide relief, developed in latites and trachybasalts lying above claystones and mudstones. The types vary from small, poorly visible landslides to vast landslides with complex relief. They were interpreted as consecutive stages of geomorphic evolution of hillslope-valley topography of the study area. Two main schemes have been established which explain the development of landslide slopes in the Kamienne Mts: (1) upslope, from the base of the slope towards the mountain ridge and (2) downslope, beginning on the top of the mountain ridge. The direction of landslide development depends on the thickness of volcanic rocks in relation to underlying sedimentary rocks. When the latter appear only in the lowest part of the slope, landslides develop upslope. If sedimentary rocks dominate on the slope and volcanic rocks form only its uppermost part, landslides develop downslope. The results show that landsliding leads to significant modifications of relief of the study area, including complete degradation of mountain ridges.