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Caves Of Aggtelek Karst And Slovak Karst
The Caves of Aggtelek Karst and Slovak Karst is a UNESCO World Heritage site consisting of 712 caves spread out over a total area of along the border of Hungary and Slovakia. Background This UNESCO World Heritage site includes seven components. They are Aggtelek, Szendrő-Rudabánya Hill, and Esztramoill in Hungary, and Dobšiná Ice Cave, Koniar plateau, Plešivec plateau, and neighbourhood of Silica and Jasov in Slovakia. Caves included are: * Baradla and Domica complex * Gombasek Cave *Silica Ice Cave *Dobšiná Ice Cave *Ochtinská Aragonite Cave * Jasovská Cave Baradla-Domica Cave complex is long with approximately one fourth of that on the Slovak side and the rest in Hungary. The first written mention of Baradla cave dates back to 1549 and from 1920 it serves as a tourist attraction. Ján Majko discovered Domica Cave (Slovak part of the complex) in 1926 and the tourist circuit opened to public in 1932 has more than . Cave was inhabited as far as 5000 BC and is an im ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Aggtelek Karst
Aggtelek Karst is a karst area in northern Hungary. The area is especially well known for its abundance of caves, which were recorded together with those in neighboring Slovakia in 1995 to the list of World Heritage Site under the name of the Caves of Aggtelek Karst and Slovak Karst. The Aggtelek National Park (Hungarian: ''Aggteleki Nemzeti Park'') is a national park in Northern Hungary, founded in 1985. It contains 198.92 km² (of which 39.22 km² are under increased protection). It has been part of the UNESCO World Heritage since 1995. The largest stalactite cave of Europe is situated in this area: the Baradla Cave The Baradla Domica cave system in Hungary is one of the longest researched, visited for centuries for its speleothems. As part of the Aggtelek Karst, the cave system extends more than and includes the Domica cave. The cave has a natural entranc ... (26 km long, of which 8 km is in Slovakia, known under the name of Domica). References {{commonscat, Agg ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Silica Ice Cave
Silicon dioxide, also known as silica, is an oxide of silicon with the chemical formula , most commonly found in nature as quartz and in various living organisms. In many parts of the world, silica is the major constituent of sand. Silica is one of the most complex and most abundant families of materials, existing as a compound of several minerals and as a synthetic product. Notable examples include fused quartz, fumed silica, silica gel, opal and aerogels. It is used in structural materials, microelectronics (as an electrical insulator), and as components in the food and pharmaceutical industries. Structure In the majority of silicates, the silicon atom shows tetrahedral coordination, with four oxygen atoms surrounding a central Si atomsee 3-D Unit Cell. Thus, SiO2 forms 3-dimensional network solids in which each silicon atom is covalently bonded in a tetrahedral manner to 4 oxygen atoms. In contrast, CO2 is a linear molecule. The starkly different structures of the dioxide ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Protected Areas Of The Western Carpathians
Protection is any measure taken to guard a thing against damage caused by outside forces. Protection can be provided to physical objects, including organisms, to systems, and to intangible things like civil and political rights. Although the mechanisms for providing protection vary widely, the basic meaning of the term remains the same. This is illustrated by an explanation found in a manual on electrical wiring: Some kind of protection is a characteristic of all life, as living things have evolved at least some protective mechanisms to counter damaging environmental phenomena, such as ultraviolet light. Biological membranes such as bark on trees and skin on animals offer protection from various threats, with skin playing a key role in protecting organisms against pathogens and excessive water loss. Additional structures like scales and hair offer further protection from the elements and from predators, with some animals having features such as spines or camouflage serv ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Caves Of Slovakia
A cave or cavern is a natural void in the ground, specifically a space large enough for a human to enter. Caves often form by the weathering of rock and often extend deep underground. The word ''cave'' can refer to smaller openings such as sea caves, rock shelters, and grottos, that extend a relatively short distance into the rock and they are called ''exogene'' caves. Caves which extend further underground than the opening is wide are called ''endogene'' caves. Speleology is the science of exploration and study of all aspects of caves and the cave environment. Visiting or exploring caves for recreation may be called ''caving'', ''potholing'', or ''spelunking''. Formation types The formation and development of caves is known as ''speleogenesis''; it can occur over the course of millions of years. Caves can range widely in size, and are formed by various geological processes. These may involve a combination of chemical processes, erosion by water, tectonic forces, microorganism ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Caves Of Hungary
A cave or cavern is a natural void in the ground, specifically a space large enough for a human to enter. Caves often form by the weathering of rock and often extend deep underground. The word ''cave'' can refer to smaller openings such as sea caves, rock shelters, and grottos, that extend a relatively short distance into the rock and they are called ''exogene'' caves. Caves which extend further underground than the opening is wide are called ''endogene'' caves. Speleology is the science of exploration and study of all aspects of caves and the cave environment. Visiting or exploring caves for recreation may be called ''caving'', ''potholing'', or ''spelunking''. Formation types The formation and development of caves is known as ''speleogenesis''; it can occur over the course of millions of years. Caves can range widely in size, and are formed by various geological processes. These may involve a combination of chemical processes, erosion by water, tectonic forces, microorganism ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Caves Of Aggtelek Karst And Slovak Karst
The Caves of Aggtelek Karst and Slovak Karst is a UNESCO World Heritage site consisting of 712 caves spread out over a total area of along the border of Hungary and Slovakia. Background This UNESCO World Heritage site includes seven components. They are Aggtelek, Szendrő-Rudabánya Hill, and Esztramoill in Hungary, and Dobšiná Ice Cave, Koniar plateau, Plešivec plateau, and neighbourhood of Silica and Jasov in Slovakia. Caves included are: * Baradla and Domica complex * Gombasek Cave *Silica Ice Cave *Dobšiná Ice Cave *Ochtinská Aragonite Cave * Jasovská Cave Baradla-Domica Cave complex is long with approximately one fourth of that on the Slovak side and the rest in Hungary. The first written mention of Baradla cave dates back to 1549 and from 1920 it serves as a tourist attraction. Ján Majko discovered Domica Cave (Slovak part of the complex) in 1926 and the tourist circuit opened to public in 1932 has more than . Cave was inhabited as far as 5000 BC and is an im ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Slovak Karst National Park
Slovak Karst National Park (''Národný park Slovenský kras'') is a national park in the Slovak Karst (''Slovenský kras'') mountain range in South East Slovakia. It lies in the Gelnica, Rožňava and Košice–okolie districts in the Košice region. The National Park covers an area of 346.11 km² (133.64 mi²) and its buffer zone covers 117.41 km² (45.33 mi²). The park was established on 1 March 2002, after being a protected landscape area since 1973. Slovak Karst is the first Slovak biosphere reserve since 1 March 1977, when it was included in the UNESCO's Programme on Man and the Biosphere. In 1995, 12 out of 700 caves in the park were recognized as a UNESCO World Heritage Site. See also *Caves of Aggtelek Karst and Slovak Karst UNESCO World Heritage site *Protected areas of Slovakia Protected areas of Slovakia are areas that need protection because of their environmental, historical or cultural value to the nation. Protected areas in Slovakia are managed ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
List Of Caves In Slovakia
There are more than 2,400 caves in Slovakia, of which more than 400 have been explored so far. New caves are being discovered constantly. Caves open to the public * caves included in the UNESCO World Heritage Sites list: **Dobšiná Ice Cave (''Dobšinská ľadová jaskyňa''), Slovak Paradise **Domica, Slovak Karst **Gombasek Cave (''Gombasecká jaskyňa''), Slovak Karst ** Jasovská Cave (''Jasovská jaskyňa''), Slovak Karst **Ochtinská Aragonite Cave (''Ochtinská aragonitová jaskyňa''), Slovak Karst * other public caves: **Belianska Cave, Tatras ** Bojnická hradná jaskyňa (literally Bojnice Castle Cave), Bojnice ** Brestovská Cave (''Brestovská jaskyňa''), Western Tatras ** Bystrianska Cave (''Bystrianska jaskyňa''), Low Tatras **Cave of Dead Bats (''Jaskyňa mŕtvych netopierov''), Low Tatras **out of the Demänová Caves ( long), Low Tatras: *** Demänovská jaskyňa Slobody (literally Demänová Cave of Freedom) *** Demänovská Ice Cave (''Demänovská ľadová ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hallstatt Culture
The Hallstatt culture was the predominant Western Europe, Western and Central European Archaeological culture, culture of Late Bronze Age Europe, Bronze Age (Hallstatt A, Hallstatt B) from the 12th to 8th centuries BC and Early Iron Age Europe (Hallstatt C, Hallstatt D) from the 8th to 6th centuries BC, developing out of the Urnfield culture of the 12th century BC (Bronze Age Europe, Late Bronze Age) and followed in much of its area by the La Tène culture. It is commonly associated with Proto-Celtic populations. Older assumptions of the early 20th century of Illyrians having been the bearers of especially the Eastern Hallstatt culture are indefensible and archeologically unsubstantiated. It is named for its type site, Hallstatt, a lakeside village in the Austrian Salzkammergut southeast of Salzburg, Austria, Salzburg, where there was a rich salt mine, and some 1,300 burials are known, many with fine artifacts. Material from Hallstatt has been classified into four periods, des ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Aragonite
Aragonite is a carbonate mineral, one of the three most common naturally occurring crystal forms of calcium carbonate, (the other forms being the minerals calcite and vaterite). It is formed by biological and physical processes, including precipitation from marine and freshwater environments. The crystal lattice of aragonite differs from that of calcite, resulting in a different crystal shape, an orthorhombic crystal system with acicular crystal. Repeated twinning results in pseudo-hexagonal forms. Aragonite may be columnar or fibrous, occasionally in branching helictitic forms called ''flos-ferri'' ("flowers of iron") from their association with the ores at the Carinthian iron mines. Occurrence The type location for aragonite is Molina de Aragón in the Province of Guadalajara in Castilla-La Mancha, Spain, for which it was named in 1797. Aragonite is found in this locality as cyclic twins inside gypsum and marls of the Keuper facies of the Triassic. This type of arago ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bükk Culture
The Bükk Mountains () are a section of the North Hungarian Mountains of the Inner Western Carpathians. Much of the area is included in the Bükk National Park. Geography Although Kékes, the highest point in Hungary, is not here but in the nearby Mátra Mountains, the average height of the Bükk Mountains–with more than 20 peaks higher than 900 m–exceeds that of Mátra. The highest point of Bükk is Kettős bérc (961 m), third highest main peak in Hungary after Kékes and Galyatető. There are 1115You can find information about Hungarian caves here: known caves in the mountain range, including Bányász-barlang (Miner cave, 274 m) and István-lápa (254 m), the deepest caves in Hungary, the archaeologically important Szeleta cave, the Cave Bath (a main tourist attraction of Miskolc-Tapolca), the Anna Cave, and the István Cave. 52 of the caves are protected because of their fauna and microclimate. The mountain range is also famous for its skiing facilities locat ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Archeological Site
An archaeological site is a place (or group of physical sites) in which evidence of past activity is preserved (either prehistoric or historic or contemporary), and which has been, or may be, investigated using the discipline of archaeology and represents a part of the archaeological record. Sites may range from those with few or no remains visible above ground, to buildings and other structures still in use. Beyond this, the definition and geographical extent of a "site" can vary widely, depending on the period studied and the theoretical approach of the archaeologist. Geographical extent It is almost invariably difficult to delimit a site. It is sometimes taken to indicate a settlement of some sort although the archaeologist must also define the limits of human activity around the settlement. Any episode of deposition such as a hoard or burial can form a site as well. Development-led archaeology undertaken as cultural resources management has the disadvantage (or the bene ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
