Baradla-Domica Cave System: Difference between revisions
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== The environment == |
== The environment == |
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Kiszögelésében northeastern Hungary, the Slovak border area along one of the country's most diverse [[karst]] os landscapes occupies. Across belonging to [[Northern Hungary]] Central Mountain range Aggtelek Karst (Aggteleki Mountains, Lower Hill) of the state border the Slovak Karst tal form a unified geological system, [[surface morphology]] and [[Hydrology]]. Before the withdrawal of the current boundaries of the two areas included in the literature [[Gömör-Torna karst]]. The karst was perfect for [[Triad]] period bedrock of (since the end of the third age) lasting about 5 million years of evolution as a result of a characteristic [[temperate]] [[mountain range]] i karst developed. The most striking characteristics: a large expanse of nearly 60 m in average height [[plateau]]s; the open [[karst relief]]s typical erosion of bowl-shaped pits and the [[doline]]s; the [[töbörsor]] V [[karst valley]] and [[Uvala]] and the steep, barren mountain slopes formed [[Karr (geology)|Karr]], [[karrmező]]s, which are the people's language [[Devil's plowing]] should be called. In some places the clogged töbrökben, [[gully]] in small dolinatavak water surface shimmers in karst and non-karst background colors border of [[blind valley]]s lined up with the locals ravaszlyukként, hell-hole, known as víznyelőkben disappear periodic streams. The region's spectacular forms of surface lying in the depths of smaller and larger caves, cave systems complement. Among the largest of the Baradla, which is longer than in Slovakia, together with the opening of the Domicával 25.5 km. The two forming a coherent whole cave in the multi-story cave development exemplifies one undeniable proof of Aggtelek and Slovak Karst hydrology of context. |
Kiszögelésében northeastern Hungary, the Slovak border area along one of the country's most diverse [[karst]] os landscapes occupies. Across belonging to [[Northern Hungary]] Central Mountain range Aggtelek Karst (Aggteleki Mountains, Lower Hill) of the state border the Slovak Karst tal form a unified geological system, [[surface morphology]] and [[Hydrology]]. Before the withdrawal of the current boundaries of the two areas included in the literature [[Gömör-Torna karst]]. The karst was perfect for [[Triad]] period bedrock of (since the end of the third age) lasting about 5 million years of evolution as a result of a characteristic [[temperate]] [[mountain range]] i karst developed. The most striking characteristics: a large expanse of nearly 60 m in average height [[plateau]]s; the open [[karst relief]]s typical erosion of bowl-shaped pits and the [[doline]]s; the [[töbörsor]] V [[karst valley]] and [[Uvala]] and the steep, barren mountain slopes formed [[Karr (geology)|Karr]], [[karrmező]]s, which are the people's language [[Devil's plowing]] should be called. In some places the clogged töbrökben, [[gully]] in small dolinatavak water surface shimmers in karst and non-karst background colors border of [[blind valley]]s lined up with the locals ravaszlyukként, hell-hole, known as víznyelőkben disappear periodic streams. The region's spectacular forms of surface lying in the depths of smaller and larger caves, cave systems complement. Among the largest of the Baradla, which is longer than in Slovakia, together with the opening of the Domicával 25.5 km. The two forming a coherent whole cave in the multi-story cave development exemplifies one undeniable proof of Aggtelek and Slovak Karst hydrology of context. |
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[[File:Okt 15.jpg|thumb|one cave trip]] |
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[[Category:Caves of Hungary]] |
[[Category:Caves of Hungary]] |
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Revision as of 12:31, 19 March 2016
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The baradla cave (formally Baradla Cave) Hungary researched the oldest, best known for centuries, visited stalactite caves. Cadastral Number: 5430-1. The Aggtelek Karst views on several entrances. Total length of the Slovak Republic was opened, it is a system component, 5.3 km long Domica cave with exceeding 25.5 km. Natural Entrance Aggtelek border of the village, at the foot of the cliff overlooking tall white with distance. The Jósvafő to the village lying, színlőkkel articulated, meandering main branch length of 7 km. The average 10 m wide and 7–8 m high rock tunnel, a huge restaurant widens in some places. The main branch of several shorter or longer side is connected. A significant part of the cave varied colors and shapes providing a unique spectacle stalactites to decorate. The Aggtelek village situated at the border of Acheron – Archer resulting víznyelőből and Domica coming from Styx Streams united today only water flowing through the main branch during floods. Víznyelőkön the dry season through the cave situated at a depth of 30–40 m Lower get caves. The cave is open from natural entrance to ancient times; there the Neolithic people could find shelter.
The first written mention originates from 1549. He graduated from Joseph Sartory – the first survey 1794. 1825 – only 1.8 km length was known. This section depicts Raisz Christian Gömör County by földmérője 1802 – was prepared map, which first appeared in print in the cave map. Vass Imre engineer 1825 – was penetrated in the previous endpoint Iron Gate waters, and revealed the cave about 5 km long main branch. The cave and the surface a description, and an accurate map. His work was published in Hungarian and German in 1831.
In order to facilitate the cave visit, the first to roll out 1806 was carried out. 1890 – artificial exit was established at the Red Lake. 1922 – the end point was the significance of the cave nearly a hundred years of Stage continuation of a new section 500 m have been identified, which 1927–28 in hand, Taro been Jósvafő. The Domica and Baradla Cave relationship 1932 – In the Styx Stream szifonjain penetrating Dr. Hubert Kessler managed to prove.
The Baradla, the Aggtelek Karst and Slovak Karst remaining caves with UNESCO 1995 He declared in the World Heritage part. The entire cave system and the catchment areas – with the Domicával – 2001 – was placed under the protection of internationally important wetlands fixing Ramsar Convention in scope. The Aggtelek National Park most appealing attractions all year round, closed without waiting for the visitors, who can choose from among several hiking trails.
The environment
Kiszögelésében northeastern Hungary, the Slovak border area along one of the country's most diverse karst os landscapes occupies. Across belonging to Northern Hungary Central Mountain range Aggtelek Karst (Aggteleki Mountains, Lower Hill) of the state border the Slovak Karst tal form a unified geological system, surface morphology and Hydrology. Before the withdrawal of the current boundaries of the two areas included in the literature Gömör-Torna karst. The karst was perfect for Triad period bedrock of (since the end of the third age) lasting about 5 million years of evolution as a result of a characteristic temperate mountain range i karst developed. The most striking characteristics: a large expanse of nearly 60 m in average height plateaus; the open karst reliefs typical erosion of bowl-shaped pits and the dolines; the töbörsor V karst valley and Uvala and the steep, barren mountain slopes formed Karr, karrmezős, which are the people's language Devil's plowing should be called. In some places the clogged töbrökben, gully in small dolinatavak water surface shimmers in karst and non-karst background colors border of blind valleys lined up with the locals ravaszlyukként, hell-hole, known as víznyelőkben disappear periodic streams. The region's spectacular forms of surface lying in the depths of smaller and larger caves, cave systems complement. Among the largest of the Baradla, which is longer than in Slovakia, together with the opening of the Domicával 25.5 km. The two forming a coherent whole cave in the multi-story cave development exemplifies one undeniable proof of Aggtelek and Slovak Karst hydrology of context.
