Caves of Aggtelek Karst and Slovak Karst


World Heritage Identification Number: 725

World Heritage since: 1995

Category: Natural Heritage

WHE Type: Natural Landscapes & Geographic Features

Transboundary Heritage: Yes

Endangered Heritage: No

Country: Hungary, Slovakia

Continent: Europe

UNESCO World Region: Europe and North America

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Exploring the Geological Wonders of the Caves of Aggtelek Karst and Slovak Karst

The Caves of Aggtelek Karst and Slovak Karst, a unique and captivating UNESCO World Heritage Site, is a mesmerizing collection of over 1000 karst caves sprawled across a vast area of approximately 55,800 hectares along the shared borders of Hungary and Slovakia. This extraordinary site offers a glimpse into the rich tapestry of geological history spanning tens of millions of years.

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UNESCO Description of the World Heritage Site

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 Justification of the World Heritage Site

Criteria (viii): The property Caves of Aggtelek and Slovak Karst, while typical of many karst localities in Europe, is distinctive in its great number (with 712 recorded at time of inscription) of different types of caves found in a concentrated area. Geological processes causing karst features to be buried by sediment and then later reactivated or exhumed provide evidence pertaining to the geologic history of the last tens of millions of years. Relicts of pre-Pleistocene karst (i.e. more than about 2 million years old) are very distinct in the area, and many of them show evidence for sub-tropical and tropical climate forms. These include rounded hills that are relicts of tropical karst later modified by Pleistocene periglacial weathering. This suite of paleokarst features, showing a combination of both tropical and glacial climates, is very unusual and is probably better documented in the Slovak Karst than anywhere else in the world.

Encyclopedia Record: Caves of Aggtelek Karst and Slovak Karst

The Caves of Aggtelek Karst and Slovak Karst are a series of over 1000 karst caves spread out over a total area of 55,800 ha along the border of Hungary and Slovakia. With an exceptional diversity of karst structures and complex cave systems developing from both temperate and tropical processes, the caves and surrounding areas were inscribed as a UNESCO World Heritage Site in 1995.

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Additional Site Details

Area: 56,650.57 hectares

Number of Components: 7

UNESCO Criteria: (viii) — Outstanding example representing major earth stages

Coordinates: 48.47573 , 20.48687

IUCN World Heritage Outlook

The 2025 Conservation Outlook on Caves of Aggtelek Karst and Slovak Karst reports the following assessment:

Good

Source: International Union for Conservation of Nature (IUCN) · View assessment

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Image of Caves of Aggtelek Karst and Slovak Karst

© Jojo, en:Jojo_1, pl:Jojo, CC BY-SA 3.0 Resized from original. (This derivative is under the same CC BY-SA license.)

World Heritage Research

Discover scientific research and academic studies that deepen our understanding of Caves of Aggtelek Karst and Slovak Karst from its history and significance to its conservation, management, and contemporary challenges.

  • Radon monitoring in the Harmanecká Cave, Slovakia

    A study monitoring radon levels in Harmanecká Cave, Slovakia, revealed that annual average radon activity concentration inside the cave ranged from 930 to 2240 Bq/m³, significantly higher than the outdoor cavity measurement of 222.5 Bq/m³. Seasonal variations in radon levels were observed but showed no clear correlation with microclimate or meteorological parameters, suggesting that continuous measurements are necessary for a comprehensive assessment. The estimated annual effective dose for cave guides remained below the safety limit of 20 mSv. The research utilized Ramarn track detectors placed at multiple stations inside and outside the cave, with data collected over a year from December 2023 to November 2024.

    Smetanová, I., Pristašová, L., Haviarová, D., & Csicsay, K. (2026). Radon monitoring in the Harmanecká Cave, Slovakia. Contributions to Geophysics and Geodesy, 56(1), 25–38. https://doi.org/10.31577/congeo.2026.56.1.2

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  • Gravimetric Detection of Cave Space and Sinkhole Hazard with Growth Inversion: Valaská Village Case in Karst (Slovakia)

    A persistent sinkhole hazard exists in Valaská village, Slovakia, despite mitigation efforts, as revealed by microgravimetric analysis using the Growth inversion methodology. This study demonstrates that Growth inversion—a free-geometry inversion technique—is effective for detecting shallow cave spaces and assessing sinkhole risks in karst environments. The research highlights both the strengths and limitations of this approach, emphasizing the importance of parameter tuning to improve accuracy. Valaská's history of sinkholes, including a notable incident involving a horse in 1964, underscores the ongoing threat, which the gravimetric study confirms remains active.

    Bódi, J., Vajda, P., Zahorec, P., Putiška, R., Papčo, J., Pašteka, R., & Fernández, J. (2026). Gravimetric Detection of Cave Space and Sinkhole Hazard with Growth Inversion: Valaská Village Case in Karst (Slovakia). Geosciences, 16(5), 179. https://doi.org/10.3390/geosciences16050179

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  • Middle Pleistocene (>350 ka) glaciation in the Carpathians unveiled by quartz microtextures from cave sediments (Low Tatra Mountains, Slovakia)

    Researchers have uncovered direct evidence of Middle Pleistocene glaciation (>350,000 years ago) in the Western Carpathians, specifically within the UNESCO-listed Caves of Aggtelek Karst and Slovak Karst. By analyzing quartz grain microtextures from dated cave sediments in the Demänová Cave System (Low Tatra Mountains, Slovakia), the study provides the first conclusive proof of Chibanian glaciation in this region. Using scanning electron microscopy, the team identified glacigenic grains preserved in allochthonous cave clastic sediments that predate Marine Isotope Stage 10. Additionally, well-rounded quartz grains from Triassic rocks suggest glacial activity during MIS 6. This innovative approach is uniquely sensitive to early glacial imprints in karst terrains, where conventional geomorphic evidence may have been erased by subsequent ice advances. The method offers a novel way to detect otherwise missing records of glaciations, advancing our understanding of past climate dynamics in this region.

    Siemek, D., Szczygieł, J., Woronko, B., Littva, J., Bella, P., & Kłapyta, P. (2026). Middle Pleistocene (>350 ka) glaciation in the Carpathians unveiled by quartz microtextures from cave sediments (Low Tatra Mountains, Slovakia). Geology, 54(10), 972–977. https://doi.org/10.1130/g54825.1

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  • Shear-Wave Seismic Imaging using Small-Scale Broadband Electromagnetic Vibrators: A Case Study from Slovak Karst Mountains

    Researchers successfully employed small-scale broadband electromagnetic vibrators to map shear-wave seismic activity in the Slovak Karst Mountains, revealing potential new extensions of cave systems. The study tested modified ElViS VII and eVibe Lightning vibrators, both generating high-quality signals within a 4–120 Hz frequency band during a CTBTO On-Site Inspection field test. While the modified ElViS showed higher harmonic distortion, it achieved a 15 dB signal increase in reflection-dominated bands, producing a stacked seismic section with a notable anomaly suggesting further cave exploration. This approach demonstrates the viability of broadband near-surface S-wave seismic imaging for karst environments.

    Brodic, B., Koivisto, E., ElGabry, M., & Labak, P. (2026). Shear-Wave Seismic Imaging using Small-Scale Broadband Electromagnetic Vibrators: A Case Study from Slovak Karst Mountains. NSG 2026: 2nd Geohazards Assessment and Risk Mitigation Conference, 1–5. https://doi.org/10.3997/2214-4609.202620189

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  • Soil enzyme activities and moss biomonitoring as complementary bioindicators of environmental status and toxic and potentially toxic element contamination in a karst cave and its catchment: Brestovská Cave, Slovakia

    A new study on Brestovská Cave, Slovakia, reveals that soil enzyme activities and moss biomonitoring are effective complementary bioindicators for assessing environmental status and toxic/potentially toxic element (TPTE) contamination. The research found two distinct gradients: a natural gradient where lithophile elements remain below world-soil averages and enzyme activities decline towards the cave's aphotic interior due to oligotrophy, rather than contamination; and an anthropogenic gradient where cadmium consistently exceeds Slovak statutory limits but shows no clear external input signal, while selenium exhibits strong enrichment and variability, indicating localized external contamination. Mercury at the resurgence also signals local pollution. Despite moderate ecological risk (ERI = 212), screening-level health risks for visitors were deemed acceptable (HI ≤ 0.59; As-CR ≤ 8.3 × 10⁻⁶). The study highlights the importance of reference choice in interpreting TPTE data and underscores the utility of moss biomonitoring alongside soil enzyme analysis.

    Bobuľská, L., Demková, L., Beheshti, M., Višňovská, Z., Lošák, T., Jančo, I., & Árvay, J. (2026). Soil enzyme activities and moss biomonitoring as complementary bioindicators of environmental status and toxic and potentially toxic element contamination in a karst cave and its catchment: Brestovská Cave, Slovakia. Catena, 274, 110585. https://doi.org/10.1016/j.catena.2026.110585

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  • Accessible Caves in Slovakia as a Tool for Geoscience Education

    Slovakia's rich karst landscape, home to over 8,100 caves, offers unparalleled opportunities for geoscience education. These subterranean environments serve as natural laboratories for studying geological processes, hydrological cycles, climate change, and the history of life on Earth. Accessible caves provide a unique platform for both experts and the general public to explore these phenomena through educational activities and guided tours. This study characterizes Slovakia's accessible caves, assessing their current state, protection measures, utilization, and presentation methods. By leveraging these geological wonders, the research highlights their potential as valuable tools for enhancing public understanding of Earth sciences.

    Javorská, M., Palgutová, S., & Pramuková, K. (2025). ACCESSIBLE CAVES IN SLOVAKIA AS A TOOL FOR GEOSCIENCE EDUCATION. Proceedings of the 16th Conference Public Recreation and Landscape Protection - with Respect Hand in Hand…, 16, 11–14. https://doi.org/10.11118/978-80-7701-025-2-0011

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  • LiDAR-Based Morphometry of Dolines in Aggtelek Karst (Hungary) and Slovak Karst (Slovakia)

    LiDAR-based morphometry reveals that doline density in the Aggtelek Karst and Slovak Karst UNESCO World Heritage Sites is 25% higher when derived from high-resolution digital terrain models (DTMs) compared to traditional topographic maps. This study introduces a new parameter, k, which characterizes the 3D shape of dolines, indicating whether they resemble cylinders, bowls (calottes), cones, or funnels. Most dolines in the region exhibit transitional shapes between bowl and cone forms. The research also highlights that doline density is negligible on slopes steeper than 12° and that 75% of dolines are associated with Wetterstein Limestone. Additionally, the lognormal distribution effectively models the size distribution of doline areas.

    Telbisz, T., Mari, L., & Székely, B. (2024). LiDAR-Based Morphometry of Dolines in Aggtelek Karst (Hungary) and Slovak Karst (Slovakia). Remote Sensing, 16(5), 737. https://doi.org/10.3390/rs16050737

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Fossils preserve an extraordinary record of life on Earth. Embedded within ancient seabeds, sedimentary rocks, cave deposits, and former landscapes, they reveal how organisms evolved, adapted, and disappeared over billions of years. They provide the evidence that allows scientists to reconstruct ancient ecosystems, trace evolutionary change, and understand the major events that have shaped the living world.

Last updated: October 19, 2026

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