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Bükk
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 ...
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Heves (county)
Heves county ( hu, Heves megye, ) lies in northern Hungary, between the right bank of the river Tisza and the Mátra and Bükk mountains. It shares borders with the Hungarian counties Pest, Nógrád, Borsod-Abaúj-Zemplén and Jász-Nagykun-Szolnok. Eger is the county seat. Tourist sights * Lake Tisza * Bükk National Park * Bélapátfalva, abbey * Castle and City of Eger * Erdőtelek Arboretum * Feldebrő, 11th century Romanesque church * Gyöngyös, Mátra Museum * Hatvan, Grassalkovich mansion * Kisnána castle * Noszvaj, De la Motte mansion * Parád * Sirok castle * Szilvásvárad, Szalajka Valley * Szarvaskő, castle ruins Geography Heves county is a geographically diverse area; its northern part is mountainous (the Mátra and Bükk are the two highest mountain ranges in Hungary), while at south it includes a part of the Great Hungarian Plain. From south it is bordered by Lake Tisza, the largest artificial lake in Hungary. The average temperature is between 8 and 1 ...
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North Hungarian Mountains
The North Hungarian Mountains ( hu, Északi-középhegység), sometimes also referred to as the Northeast Hungarian Mountains, Northeast Mountains, North Hungarian Highlands, North Hungarian Mid-Mountains or North Hungarian Range, is the northern, mountainous part of Hungary. It forms a geographical unity with the Mátra-Slanec Area, the adjacent parts of Slovakia. It is a separate geomorphological area within the Western Carpathians. The mountains run along the northeastern border of Hungary as well as eastern parts of the Hungarian–Slovak border in broadband from the Danube Bend to the town of Prešov. Subdivisions The area consists of the following geomorphological units: * Börzsöny Regional Map Series of Hungary
( hu, Börzsöny +
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Bükk National Park
Bükk National Park ( hu, Bükki Nemzeti Park) is a national park in the Bükk Mountains of Northern Hungary, near Miskolc. It was founded in 1977 as the third national park in the country. It contains 431.3 km2 (of which 37.74 km2 is under increased protection). Mountainous and forested, Bükk is Hungary's largest national park and is situated in the northern mountains, between Szilvásvárad and Lillafüred. Bükk's important geological features include various karst formations within its limestone mountains - particularly caves (once inhabited by pre-historic people), swallow-holes, and ravines. The country's longest (4,000 metres) and deepest (245 metres) cave, Istvánlápa, is located in the park. Bükk National Park also contains ninety species of nesting birds, some considered endangered. The Vatican Climate Forest was to be located within the Park. KlimaFa ("Climate Trees") was started by a San Francisco promoter, Russ George, who promised a carbon offsetting pro ...
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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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Inner Western Carpathians
Divisions of the Carpathians are a categorization of the Carpathian mountains system. Below is a detailed overview of the major subdivisions and ranges of the Carpathian Mountains. The Carpathians are a "subsystem" of a bigger Alps-Himalaya System that stretches from western Europe all the way to southern Asia, and are further divided into "provinces" and "subprovinces". The last level of the division, i.e. the actual mountain ranges and basins, is usually classified as "units". The main divisions are shown in the map on the right. To generalize, there are three major provinces (regions): Western Carpathians, Eastern Carpathians, and the Southern Carpathians. Naming conventions The division is largely (with many exceptions) undisputed at the lowest level (except for the Ukrainian part), but various divisions are given for the higher levels, especially for the penultimate level. A geomorphological division has been used as much as the data was available; other new physio ...
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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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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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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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