2014 Conservation Outlook Assessment (Archived)
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Caves of Aggtelek Karst and Slovak Karst Hungary & Slovakia
CAVES OF AGGTELEK KARST AND SLOVAK KARST HUNGARY & SLOVAKIA The variety and concentration of their formations make these cave systems of 712 caves excellent representatives of a temperate-zone karstic network. They also display an extremely rare combination of tropical and glacial climatic effects, making it possible to study geological history over tens of millions of years. COUNTRY Hungary and Slovakia NAME Caves of Aggtelek Karst and Slovak Karst NATURAL WORLD HERITAGE TRANSBOUNDARY SERIAL SITE 1995: The cave systems of the two protected areas jointly inscribed on the World Heritage List under Natural Criterion viii. 2000: Extended to include Dobšinská cave in Slovakia (660 ha). 2008: Extended by 87.8 ha. STATEMENT OF OUTSTANDING UNIVERSAL VALUE [pending] INTERNATIONAL DESIGNATIONS 1977: Slovensky Kras Protected Landscape Area designated a Biosphere Reserve under the UNESCO Man & Biosphere Programme (36,166 ha). 1979: Aggtelek National Park designated a Biosphere Reserve under the UNESCO Man & Biosphere Programme (19,247 ha); 2001: Baradla Cave System & Related Wetlands, Hungary (2,075 ha) and Domica Wetland in the Slovensky Kras, Slovak Republic (627 ha) both in Aggtelek National Park, designated a transboundary Wetland of International Importance under the Ramsar Convention. IUCN MANAGEMENT CATEGORY II National Parks BIOGEOGRAPHICAL PROVINCE Middle European Forest (2.11.5) GEOGRAPHICAL LOCATION Straddles the Slovensky Kras foothills of the Carpathian mountains on the border of southern Slovakia and northern Hungary 152 km northeast -
2020 Conservation Outlook Assessment
IUCN World Heritage Outlook: https://worldheritageoutlook.iucn.org/ Caves of Aggtelek Karst and Slovak Karst - 2020 Conservation Outlook Assessment Caves of Aggtelek Karst and Slovak Karst 2020 Conservation Outlook Assessment SITE INFORMATION Country: Hungary, Slovakia Inscribed in: 1995 Criteria: (viii) The variety of formations and the fact that they are concentrated in a restricted area means that the 712 caves currently identified make up a typical temperate-zone karstic system. Because they display an extremely rare combination of tropical and glacial climatic effects, they make it possible to study geological history over tens of millions of years. © UNESCO SUMMARY 2020 Conservation Outlook Finalised on 02 Dec 2020 GOOD The conservation outlook for the karst features of the site is positive overall. Only about 1% of the caves are open for visitation and careful monitoring programmes are in place. Protection and management of the karst areas is relatively effective both in Hungary and Slovakia and on transboundary level. However, there are some concerns regarding the lack of resources, particularly in Slovakia where the current staff numbers and funding are insufficient and significantly lower than in the Aggtelek National Park in Hungary. Certain areas will require improvement, including better cooperation between different institutions and better engagement of local communities. Potential threats, such as pollution or infrastructure projects in the broader region, will require monitoring and careful planning, ensuring that the necessary environmental impact assessments have been undertaken, as well as development of an integrated management of the entire water catchment, and this will need to be supported by adequate funding in the long term. -
Information Sheet on Ramsar Wetlands Categories Approved by Recommendation 4.7 the Conference of the Contracting Parties
Information Sheet on Ramsar Wetlands Categories approved by Recommendation 4.7 the Conference of the Contracting Parties NOTE: It is important that you read the accompanying Explanatory Note and Guidelines document before completing this form. 1. Date this sheet was completed/updated: FOR OFFICE USE ONLY. Completed: 26.11.1999. DD MM YY Designation date Site Reference Number 2. Country: Hungary Region: Borsod - Abaúj - Zemplén County, Districts: Aggtelek, Jósvafő 3. Name of wetland: Baradla Cave System and Related Wetlands 4. Geographical coordinates: latitude: min. 48°26’26” max. 48°29’24” longitude: min. 20°27’56” max: 20°33’28” 5. Altitude: (average and/or. max. & min.) 318,3-484,6 m. 6. Area: (in hectares). 2075,196 ha 7. Overview: (general summery, in two or three sentences, of the wetland's principal characteristics) The Baradla Cave System is the Hungarian part of the 25 km long Baradla-Domica Cave System that is a typical and the largest subterranean hydrological system of the karst plateau in the territory of Hungary and Slovakia. The site is listed as a representative part of a bilateral UNESCO Biosphere Reserve and the World Cultural and Natural Heritage site. The site is characterised by a permanent subterranean stream, ponds, rich dripstone formations and diverse representatives of subsurface fauna as well as rich archeological findings. The cave has more levels. 8. Wetland Type (please circle the applicable codes for wetland types as listed in Annex I of the Explanatory Note and Guidelines document.) marine-coastal: A . B . C . D . E . F . G . H . I . J . K inland: L . -
Iucn Summary Caves Ofthe Aggtelekand Slovak Karst
I WORLD HERITAGE NOMINATION - IUCN SUMMARY CAVES OFTHE AGGTELEKAND SLOVAK KARST (HUNGARY/SLOVAK REPUBLIC) Summary prepared by IUCNIWCMC (March 1995) based on the original nomination supplied by the Governments of Hungary and Slovakia. This original and all documents in support of this nomination will be available for consultation at the meetings of the Bureau and the Committee. 1. LOCATION Situated on the southern foothills of the Carpathian mountains, on the southern Slovakian and northeastern Hungarian border. 2. JURIDICAL DATA The Slovak Karst and Caves of Aggtelek were both designated protected landscape areas in 1973 and 1978, respectively. The latter was redesignated a national park in 1985. Both sites have been individually accepted as biosphere reserves, Slovak Karst in 1977 and Caves of Aggtelek in 1979 . 3. IDENTIFICATION The Caves of Aggtelek and Slovak Karst territory extends over a total area of 55,800ha and topographically comprises limestone plateaus dissected by deep river valleys. The territory is characterised by a fully developed karst landscape, of which dolines are the most typical surface landform. These have developed through solution and are, on average, 100m wide and 20m deep. Other surface phenomena include sink holes and karren fields. This is the most extensively explored karst area in Europe, and a total of 712 have so far been identified. Many of the younger caves which have formed at the plateau edges, such as Knlsnohorska and Gombasecka, occur on several levels and contain dripstone decorations. The most notable of these is the Baradla-Domica cave system which is 21 km long and connects Hungary with Slovakia. -
Section II: Summary of the Periodic Report on the State of Conservation, 2006
State of Conservation of World Heritage Properties in Europe SECTION II from the aesthetic or scientific standpoint an extraordinary world value. SLOVAKIA/HUNGARY All the caves, chasms as well as the other karst forms are constituents of one geomorphological unit Caves of Aggtelek Karst and the Slovak Karst and its southern continuation in Slovak Karst Hungary. Therefore they belong to the same physical-geographical formation, to the same biogeographical area, just as the ecosystems are of Brief description the same type. Suggested nature heritage is The variety of formations and the fact that they are propounded to include in the list of the world concentrated in a restricted area means that the heritage in accordance with the Convention in virtue 712 caves currently identified make up a typical of the criteria: iii) and partially as well iv) temperate-zone karstic system. Because they The nature heritage suggested for inclusion in the display an extremely rare combination of tropical world heritage is made up of the remarkable and glacial climatic effects, they make it possible to subterranean cave systems with a unique and study geological history over tens of millions of unrevolving sinter and aragonite decoration. years. The underground cave systems as well as karst surface are also an important and significant place 1. Introduction of natural occurrence of the surviving endangered species of animals of s great scientific value. In Year(s) of Inscription 1995, 2000 addition to it subterranean chambers have a major Agency responsible for site management speleoarchaeological significance, • Ministry of the Environment of the Slovak From the caves of the territory is known so far the Republic highest stalagmite in the world with a height of Environmental Policy and Law Division 32,7m, the only cave with an aragonite decoration Nam. -
Geological Heritage, Geotourism and Local Development in Aggtelek National Park (NE Hungary)
Geoheritage (2020) 12: 5 https://doi.org/10.1007/s12371-020-00438-7 ORIGINAL ARTICLE Geological Heritage, Geotourism and Local Development in Aggtelek National Park (NE Hungary) Tamás Telbisz1 & Péter Gruber2 & László Mari1 & Margit Kőszegi3 & Zsolt Bottlik3 & Tibor Standovár4 Received: 6 April 2019 /Accepted: 7 January 2020 /Published online: 25 January 2020 # The Author(s) 2020 Abstract We examine how geoconservation and geotourism can help the local development of an economically underdeveloped karst area. First, we briefly present the geoheritage of Aggtelek National Park, which largely overlaps the area of the Aggtelek Karst. The area is built up predominantly of Triassic limestones and dolomites. It is a typical temperate zone, medium mountain karst area with doline-dotted karst plateaus and tectonic-fluvial valleys. Besides caves, the past history of iron mining also enriches its geoheritage. Aggtelek National Park was set aside in 1985. The caves of Aggtelek Karst and Slovak Karst became part of the UNESCO World Heritage in 1995 due to the high diversity of cave types and morphology. Socially, the area of the national park is a disadvantaged border region in NE Hungary. Baradla Cave has always been a popular tourist destination, but visitor numbers fell significantly after 1985. Tourism is largely focused on Baradla Cave, and thus it can be considered “sensu lato” geotourism. Reasons for the changes in visitor numbers are discussed in this paper. Tourist motivations, the significance of geotourism and other tourism-related issues were explored in our study by questionnaire surveys and semi-structured interviews. Furthermore, the balance of geoconservation versus bioconservation is also examined.