Bükk Wine Region
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Bükk Wine Region
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 located ...
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Sălaj County
Sălaj County () (also known as ''Land of Silvania'', ''silva, -ae'' means "forest") is a county ('' județ'') of Romania, located in the north-west of the country, in the historical regions of Crișana and Transylvania. It is bordered to the north by Satu Mare and Maramureș counties, to the west and south-west by Bihor County, and to the south-east by Cluj County. Zalău is the county seat, as well as its largest city. Etymology In Hungarian, it is known as ''Szilágy megye'', in Slovak as ''Salašská župa'', and in German as ''Kreis Zillenmarkt''. The county is named after the river Sălaj, which gets its name from Hungarian ''Szilágy'' "elm creek", composed from '' szil'', "elm" and '' ágy'' "riverbed". History Antiquity On 28 July 1978, a team of speleologists discovered in the cave of Cuciulat Paleolithic paintings about 12,000 years old, unique in Romania. Called the "Romanian Altamira", this cave features several red paintings of animals, including horses ...
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Szeletian
The Szeleta Culture is a transitional archaeological culture between the Middle Paleolithic and the Upper Palaeolithic, found in Austria, Moravia, northern Hungary, and southern Poland. It is dated 41,000 to 37,000 years before the present ( BP), and is named after Szeleta Cave in the Bükk Mountains, part of the North Hungarian Mountains. It was preceded by the Bohunician (48,000–40,000 BP), and is roughly contemporary with the Aurignacian (43,000–26,000 BP) in France, and the Uluzzian (45,000–37,000 BP) in Italy. It was succeeded by the Gravettian (33,000–21,000 BP). The initial excavation of the Szeletian cave was carried out from 1906 to 1913 by Ottocar Kadić. The idea of a distinctive Szeletian culture was advocated by the Czechoslovak archaeologist František Prošek (1922–1958). Neanderthals or modern humans It has been called the most original and also the most aboriginal Upper Palaeolithic culture in Central Europe. The findings are often interpreted in ...
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Mountain Ranges Of Hungary
A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited Summit (topography), summit area, and is usually higher than a hill, typically rising at least 300 metres (1,000 feet) above the surrounding land. A few mountains are Monadnock, isolated summits, but most occur in mountain ranges. Mountain formation, Mountains are formed through Tectonic plate, tectonic forces, erosion, or volcanism, which act on time scales of up to tens of millions of years. Once mountain building ceases, mountains are slowly leveled through the action of weathering, through Slump (geology), slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce Alpine climate, colder climates than at sea level at similar latitude. These colder climates strongly affect the Montane ecosystems, ecosys ...
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Alpine Skiing
Alpine skiing, or downhill skiing, is the pastime of sliding down snow-covered slopes on skis with fixed-heel bindings, unlike other types of skiing ( cross-country, Telemark, or ski jumping), which use skis with free-heel bindings. Whether for recreation or for sport, it is typically practiced at ski resorts, which provide such services as ski lifts, artificial snow making, snow grooming, restaurants, and ski patrol. "Off-piste" skiers—those skiing outside ski area boundaries—may employ snowmobiles, helicopters or snowcats to deliver them to the top of a slope. Back-country skiers may use specialized equipment with a free-heel mode, including 'sticky' skins on the bottoms of the skis to stop them sliding backwards during an ascent, then locking the heel and removing the skins for their descent. Alpine skiing has been an event at the Winter Olympic Games since 1936. A competition corresponding to modern slalom was introduced in Oslo in 1886. Participants and venues ...
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Microclimate
A microclimate (or micro-climate) is a local set of atmospheric conditions that differ from those in the surrounding areas, often with a slight difference but sometimes with a substantial one. The term may refer to areas as small as a few square meters or square feet (for example a garden bed or a cave) or as large as many square kilometers or square miles. Because climate is statistical, which implies spatial and temporal variation of the mean values of the describing parameters, within a region there can occur and persist over time sets of statistically distinct conditions, that is, microclimates. Microclimates can be found in most places but are most pronounced in topographically dynamic zones such as mountainous areas, islands, coastal areas. Microclimates exist, for example, near bodies of water which may cool the local atmosphere, or in heavy urban areas where brick, concrete, and asphalt absorb the sun's energy, heat up, and re-radiate that heat to the ambient air: t ...
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Fauna
Fauna is all of the animal life present in a particular region or time. The corresponding term for plants is ''flora'', and for fungi, it is '' funga''. Flora, fauna, funga and other forms of life are collectively referred to as '' biota''. Zoologists and paleontologists use ''fauna'' to refer to a typical collection of animals found in a specific time or place, e.g. the "Sonoran Desert fauna" or the "Burgess Shale fauna". Paleontologists sometimes refer to a sequence of faunal stages, which is a series of rocks all containing similar fossils. The study of animals of a particular region is called faunistics. Etymology ''Fauna'' comes from the name Fauna, a Roman goddess of earth and fertility, the Roman god Faunus, and the related forest spirits called Fauns. All three words are cognates of the name of the Greek god Pan, and ''panis'' is the Greek equivalent of fauna. ''Fauna'' is also the word for a book that catalogues the animals in such a manner. The term was first used b ...
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István Cave
The István Cave (''St. Stephen's Cave'') is a limestone cave in Miskolc-Lillafüred, Northern Hungary. The cave was formed in the Triassic period and is about 710 m long. It was discovered in 1913. According to local legend, a dog fell into a 15-metre deep shaft, which was the cave's only natural opening. People found the cave when they rescued the dog. Cavers began to explore the cave in 1927. Another entrance was made for the tourists, and in 1931 the cave was opened to the public. During World War II, the cave was damaged, with many of the stalagmites and stalactites were broken by people seeking refuge from air raids. The lighting was repaired only in 1955, and the cave was opened to the public again. The cave is still being explored, but only a part can be visited. Its deepest known area is named ''Hell''. The most beautiful dripstone structures are the ''Mammut's Mouth'', ''Fairyland'', ''Column Hall'' and ''Concert Hall''. Due to water filling the cave in 1958 and 1974, ...
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Anna Cave
The Anna Cave (also called ''Petőfi Cave'') is a natural limestone cave in Miskolc-Lillafüred, Hungary, near the waterfall. The cave was discovered in 1833, when opening a shaft in the limestone in order to provide the iron furnace at Hámor with water. It soon became a tourist attraction, even Sándor Petőfi visited it in 1847. However, in the second part of the century, when the iron furnaces were closed, the cave was forgotten. It was opened again in 1912. In 1927, when the Palace Hotel was built, new caverns were found. The entrance that's used today was constructed then. The cave has not only nice limestone structures, but also plant fossils. The cave can be visited all year round. See also * István Cave, a large dripstone cave Dripstone may refer to: *Hood mould or dripstone, an architectural feature for handling rain water * Dripstone, a type of speleothem (cave formation) that includes for example stalactites * Dripstone, a type of water filter made of porous ston ...
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Miskolc-Tapolca
Miskolctapolca or ''Miskolc-Tapolca'' (formerly ''Görömböly-Tapolca'', planned to be ''Tapolcafürdő'' after gaining independence from Miskolc, in colloquial speech known as ''Tapolca'') is a suburb of Miskolc, and is one of the most popular tourist towns of Hungary. Not to be confused with Tapolca town in Veszprém County. History The area has been inhabited since ancient times. The archaeological findings can be seen in the Ottó Herman Museum. Before the Hungarians conquered the area, it was inhabited by Slavic tribes. Its name comes from a Slavic word meaning bath and was first mentioned by Anonymus. Documents dating back to 1219 mention a Benedictine monastery in Tapolca; it stood until the 16th century, but during the Ottoman occupation of Hungary the monastery was attacked several times and the monks left. Tapolca remained without permanent residents until the 19th century, although it was used as a holiday resort already in the early 18th century. At this time it be ...
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Cave Bath
The Cave Bath ( hu, Barlangfürdő []<( hu, barlang [] ‘cave’+( hu, fürdő [] ‘bath’) is a hot spring, thermal bath in a natural cave in Miskolctapolca. The thermal water (temperature: 30°C/86°F) is reputed to reduce joint pain, and since it has a lower salt content than most thermal waters (around 1000 mg/liter), people can bathe in it for much longer, practically an unlimited amount of time. The Cave Bath can be visited all year long, except for January. The cave and the thermal spring have been known since ancient times, but Tapolca became a popular bathing place only after the Ottoman occupation of Hungary (16th-17th century). During this time the area bel ...
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