Aggtelek National Park
Borsod-Abaúj-Zemplén
Aggtelek National Park, established in 1985 from the Aggtelek Landscape Protection Area, is Hungary's fourth national park and the first dedicated specifically to preserving geological values. Covering over 20,000 hectares in the Aggtelek Karst region, it is renowned for its spectacular karst formations and extensive stalactite caves, including the famous Baradla Cave. The park's landscape is primarily low mountainous and hilly, with notable features such as dolines, sinkholes, and underground rivers formed by the dissolution of limestone over millions of years. Its rich biodiversity includes numerous protected plant and animal species that thrive in the karst environment. The park represents a significant geological heritage, showcasing karst phenomena developed since the Mesozoic era, with rock formations dating back approximately 210-240 million years. Aggtelek National Park is part of the UNESCO World Heritage Site shared with the Slovak Karst, highlighting its international importance. Visitors can explore various caves, observe unique geological structures, and enjoy the natural beauty of the surrounding forests and valleys.
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Tip: The best time to visit Aggtelek National Park is during late spring through early autumn when weather conditions favor cave tours and hiking. It is advisable to book guided cave tours, especially for the Baradla Cave, in advance due to their popularity. Visitors should wear comfortable walking shoes and bring warm clothing for the cooler cave temperatures. Discounts are often available for students, seniors, and groups. Check the official website or contact the visitor center for up-to-date information on opening hours and ticketing.
Zajímavosti
- •Aggtelek National Park contains one of the largest stalactite caves in Europe, the Baradla Cave, which extends over 25 kilometers.
- •The park's karst formations began developing around 210-240 million years ago during the Triassic period.
- •It is part of the UNESCO World Heritage Site shared with the Slovak Karst, emphasizing its geological and ecological importance.
- •The region features diverse karst water bodies, including doline lakes and intermittent ponds formed by sinkholes.
- •The park hosts over ninety karst springs, with the Jósva stream being its largest watercourse fed by multiple karst sources.
Historie
The area of Aggtelek National Park has been recognized for its natural and geological significance since the mid-20th century.
In 1940 and 1951, parts of the Baradla Cave were declared protected areas, followed by other caves in the 1950s.
By 1962, all caves within the karst region were granted legal protection under Hungarian nature conservation laws.
The national park itself was officially established in 1985 to safeguard the unique karst landscape and its biodiversity.
The park forms part of the larger Borsod–Abaúj–Zemplén County, an area with a rich historical background tied to medieval castles and the development of Northern Hungary.
Průvodce po místě
Baradla Cavediscovered in prehistoric times, developed over millions of years
The most famous cave system within Aggtelek National Park, known for its vast stalactite formations and underground passages stretching over 25 kilometers. Guided tours showcase spectacular geological formations and subterranean lakes.
Aggtelek Karst Plateauformed during the Mesozoic era (approx. 210-240 million years ago)
A limestone plateau featuring characteristic karst phenomena such as sinkholes, dolines, and karren fields. The plateau's terrain offers hiking opportunities with panoramic views of the surrounding landscape.
Jósva Stream and Springs
A network of over ninety karst springs feeding the Jósva stream, the park's largest watercourse. These springs demonstrate the complex underground water systems characteristic of karst landscapes.
Kontakt
Telefon: (06 48) 506 000