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Aggtelek and Slovak Karst

The Caves of the Aggtelek and Slovak Karst is a transboundary karst cave system, noted for its high concentration of caves and their great variety in cave types.

There are 712 caves in total. Features include the world's highest stalagmite and an ice filled abyss.

The following caves are part of the inscribed area:

- Baradla-Domica Cave System

- Béke-barlang Cave

- Kossuth-barlang Cave

- Meteor-barlang Cave

- Rákóczi 1.sz. barlang Cave

- Rákóczi 2.sz,.barlang Cave

- Rejtek-szomboly Chasm

- Szabadság-barlang Cave

- Vass Imre-barlang Cave

- Vecsem-bükki-szomboly Chasm

- Baradla-Domica Cave System

- Diviaèia Chasm

- Drienovská Cave

- Gombasecká Cave-Silicka Jadnica Ice Cave System

- Hrušovská Cave

- Jasovská Cave

- Krásnohorská Cave

- Ochtinská aragonitová Cave

- Obrovská Chasm

- System of the Skalistý potok Cave

- Snežná diera Cave

- Zvonivá diera Chasm

- Dobšinská Ice Cave

Map

Visit May 2008

En route from Banska Stiavnica to Kosice I passed the Slovak Karst area, half of this transboundary WHS near the border with Hungary. A number of caves open to visitors are located here, all well signposted off the main road. Some are still closed at this time of year (notably the Dobsinska Ice Cave). I decided to visit the Gombasecka cave, which is applauded in the Bradt guidebook as on of the most visually impressive.

I arrived at an almost empty parking area. The ticket booth seemed closed too, but when I appeared the window was opened. The entrance fee is 140SK (about 3 EUR) and you only get in with a guided tour. I had to wait an hour for that (Bradt didn't get the opening hours right).

At 1 pm it suddenly got very busy near the entrance. Tens of visitors arrived, mostly regional according to their car plates (Slovak, Czech, Polish, Hungarian). There were so many they even had to split the group in two 'smaller' groups of about 30.

The accessible part of this cave isn't very big, the whole tour takes about 40 minutes. Its key feature are the soda straws, very thin and hollow dripstones. It's certainly nice, but not different from other dripstone caves. I had to look hard for an accompanying picture where it doesn't look like that it has been taken at Carlsbad Caverns. But a visit to one of these caves certainly is a nice enough break in the long drive from West to East Slovakia.

Community Reviews


Hubert Scharnagl - March 2015

The cave system of the Aggtelek and Slovak Karst was inscribed mainly because of the high number of caves in a relatively small area and the variety of geological morphology, but less because of the outstanding value of the individual caves. At the time of inscription 712 caves were registered, 23 are listed in the nomination files (see above), today more than 1000 are known, and seven or eight of them are show caves and open to the public.

We spent one day for this WHS, we have chosen three caves that cover the diversity of the cave types: the Dobšinská Ice Cave, the Ochtinská Aragonite Cave, and the Gombasecká cave.

First, we visited the Dobšinská Ice Cave. Ice caves with year-round ice formations are relatively rare, there must be sub-zero temperatures throughout the year, at least in parts of the cave. The main attractions in the Dobšinská Cave are the huge ice block that fills almost the whole first part of the cave, and the Great Hall, where the ice is up to 26 metres thick and where you can also see ice columns and ice stalagmites. I have previously visited two ice caves in Austria, the Dachstein Ice Cave (WHS Hallstatt-Dachstein) and the Werfen Eisriesenwelt (no WHS, near Salzburg). I have to admit, that I was more impressed by the ice formations in the Werfen Cave.

Next we went to the Ochtinská Aragonite Cave (photo), definitely the highlight of our cave tour. Aragonite is a crystalline form of calcium carbonate, a very common mineral. But in the Ochtinska Cave it creates a wonderful variety of shapes: thin needles, spirals, branched tufts, cones and a lot more. It's really unique, very different from the usual stalactites and stalagmites. The cave consists of ten small halls, the most impressive is the Milky Way Hall. It was named after a long crack in the ceiling, decorated with milky white bundles of aragonite. We all had a stiff neck after the guided tour.

The Gombasecká Cave is a dripstone cave, the special feature are the extremely thin stalactites, only a few millimetres in diameter, but sometimes up to three metres long. But there are also the usual stalactites and stalagmites. Nice to visit, but not really outstanding.

We travelled by car, so it was easy to visit the three caves in one day. Dobšinská is about 45 minutes from Ochtinská, and from there it is only 20 minutes to Gombasecká. Each tour takes about 40 to 45 minutes; there are hourly tours in the summer season. It would be possible to visit even more caves, the Baradla-Domica cave complex is only 20 kilometres from Gombasecká, but three were more than enough for one day. The entrance fee was five to eight euros (in August 2014), and photo permit costs ten (Dobšinská and Ochtinská) or seven euros (Gombasecká), respectively

Of course it is difficult to assess the value of an extensive cave system by visiting only a few caves, but I think we got a glimpse of the diversity of the site. We enjoyed our cave tour, and at least the Aragonite Cave was a unique and impressive experience.


john booth - December 2012

I only managed to reach four of the listed caves, three in Slovakia and one in Hungary.

Dobsinska Ice Cave : similar to the Dachstein ice cave in Austria, but easier of access. Entry E6. Access by bus from Poprad-Tatry station.

Jasovska cave : featured splendid caramel coloured rock formations. Entry E5. Access by bus from Kosice.

Ochtinska cave : featured spaghetti-like stalactites. Entry E5. Access by bus from Kosice or Roznava, then 2km walk.

Kossuth Cave : found the entry, but was closed. Access by bus from Aggtelek-Josvafa station.


Christer Sundberg - September 2006

The only thing you really need to know about the Aggtelek Karst caves is that it is an absolutely fabulous place and a true masterwork of nature – just go there as soon as you can.

Once you’ve seen this place you feel like you want to return again and again and discover what’s behind the next cave and the next. The beauty of the shapes, forms and sizes of the stalactites and stalagmites is mind-blowing and it’s no wonder that many poets and painters have been inspired by its bizarre shapes and colours.

The caves are formed in 230 million year old Triassic limestone and about 2 million years ago, water started to get into the cracks, dissolving the limestone, widening the crevices and forming passages. Today there are over 1000 smaller and larger caves and you can visit the most spectacular ones on guided tours. I went for two tours and spent over four hours underground which was quite nice when the outside temperature was +35 and the caves holds a constant temperature of +9.

Aggtelek is not only caves but also a nature area and if you want to stay around for some time I can strongly recommend the Cseppkõ Hotel, run by the nice Mr Jorge, a former Hungarian border guard who knows the town and the area inside out.


Maarten J Vermeulen - March 2006

I visited the Dobsinska ladova jaskyna in 2001. Since 1995 I've been in Slovakia about 30 times.

Now I found a terrible negative comment on the main page of WHS of Paul Tanner of the UK about the Dobsinska ladova jaskyna (Dobsinska Ica Cave)

If you know the ice pillars are ALWAYS there in this cave unlike other caves then it is special enough to call it a WHS. Ths has got nothing to do with politics.

The entrance fee nowadays is SK 150,- which equals EUR 3,95 or old DM7,90. So 15 years down the line and taking into account inflation the entrance fee is much lower now.

My opinion: it is an interesting site to visit on a nice walking distance from the railway station as well.

Regards,

Maarten J Vermeulen

Holandsko


Solivagant - March 2006

I am afraid this is yet another example of a second rate “WHS “ which adds little to other similar sites already inscribed and which, one feels, has probably been chosen mainly for political reasons (As a transnational site – “it is IUCN’s opinion that this is the best and perhaps only prospect for a World Heritage site in Hungary and Slovakia). Its presence on the list typifies the gradual degradation of standards by UNESCO. The original evaluation is totally “underwhelming” in its enthusiasm for the site –

a. “CASK does not stand out on any particular natural feature. As one reviewer noted, other caves similar to those at Aggtelek exist elsewhere and, while the site is not considered unique, it is an excellent example. Although one of the better known cave areas in Europe it does not offer features in the “spectacular” category as are found in many other Karst areas”.

b. “CASK is very different from the other two existing World Heritage caves. Mammoth Cave is notable for its enormous length, large level passages and jagged domepits. Skocjan is famous for its awesome river canyons and textbook portrayal of karst hydrogeology. CASK is distinguished by its great variety of cave types and speleothems and the array of typical temperate zone karst features. CASK also contains 712 known caves, a very high concentration, but none of these by itself rates on world lists of the deepest/largest or most decorated.”

So don’t expect too much! But don’t get me wrong – if you are in the area, have a few spare hours and quite like visiting caves then by all means visit it but this isn’t a “world class” site. Parts of it were made World Biosphere Reserves in the late 1970s and that recognition should have been enough to assist appropriate conservation. To tell the truth, experiences around the world have convinced us that too many caves are opened primarily as money-making “visitor attractions” - at least this is all state owned!

In 1991 we visited the “Dobsinska Ice Cave” in what was then southern Czechoslovakia but this wasn’t included in the list of caves inscribed in 1995. WHS collectors should always keep an eye on “extensions” to existing sites however and, in 2000, the site was extended by adding just this cave and we could “count” the site! To quote - “The Committee approved the incorporation of the Dobsinská Ice Cave as part of the Caves of the Aggtelek Karst and Slovak Karst World Heritage site. Although this ice cave is a relatively small (6km2) and specialised feature, it does add variety to the existing site and its features relate to and complement the Caves of Aggtelek Karst and Slovak Karst.”

Well the site certainly needed it – indeed it was perhaps surprising that Dobsinská wasn’t included from the start as it is perhaps the most “noteworthy” of the caves in the area which are open for public visiting. Despite my generally negative review of it as a WHS it does contain a sight which, as far as I can remember, we haven’t seen in any of the many other caves we have visited around the world - all year round “Ice Pillars”. One of these is portrayed in my “photo” which shows of the front page of the brochure provided back in 1991 together with the entrance ticket. Note the rather steep (for those days) 10 Deutchmarks entrance fee – the Korun was unconvertible then and foreigners had to pay in hard currency! I wonder what its entrance price is now.


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Site Info

Full name: Caves of the Aggtelek and Slovak Karst

Site History

  • 2003 - Name change

    From "Caves of the Aggtelek Karst and Slovak Karst" to "Caves of Aggtelek Karst and Slovak Karst"
  •  
  • 2000 - Extended

    To include Dob
  •  
  • 1998 - Rejected

    As Slovak Paradis and Dobsinska Ice Cave: Does not meet WHS criteria - Add Dobsinska to Aggtelek and Paradis to Spissky Castle?
  •  
  • 1995 - Inscribed

    Reasons for inscription
  •  

Locations

The site has 7 locations.

  • Component including Aggtelek Hungary,
  • Component neighbouring Silica and Jasov Slovakia,
  • Component of Esztramos Hill Hungary,
  • Component of Koniar plateau (including Ochtinscká Aragonite Cave)
  • Component of Plešivec plateau
  • Component of Szendrő-Rudabánya Hill
  • Dobšinská Ice Cave

Connections

The site has 17 connections.

Constructions

Ecology

Geography

History

Timeline

  • Early Pleistocene Beginning some two million years ago, extensive and complex surface and underground erosion developed in this rock into classic forms of temperate climate karst.

WHS Hotspots

WHS on Other Lists

  • Natura 2000 in 2004, the Aggtelek National Park and the Slovensk´y kras National Park became part of the EU-wide network of protected the Natura 2000 sites.
  • Ramsar Wetlands Domica, 2001 / Baradla Cave System and related wetlands, 2001
  • World Biosphere Reserves Separate Biospheres in Hungary (Aggtelek (1979)) and Slovakia (Slovenski Kras (1977))

World Heritage Process