Anna Cave
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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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Limestone
Limestone ( calcium carbonate ) is a type of carbonate sedimentary rock which is the main source of the material lime. It is composed mostly of the minerals calcite and aragonite, which are different crystal forms of . Limestone forms when these minerals precipitate out of water containing dissolved calcium. This can take place through both biological and nonbiological processes, though biological processes, such as the accumulation of corals and shells in the sea, have likely been more important for the last 540 million years. Limestone often contains fossils which provide scientists with information on ancient environments and on the evolution of life. About 20% to 25% of sedimentary rock is carbonate rock, and most of this is limestone. The remaining carbonate rock is mostly dolomite, a closely related rock, which contains a high percentage of the mineral dolomite, . ''Magnesian limestone'' is an obsolete and poorly-defined term used variously for dolomite, for limes ...
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Miskolc
Miskolc ( , , ; Czech language, Czech and sk, Miškovec; german: Mischkolz; yi, script=Latn, Mishkoltz; ro, Mișcolț) is a city in northeastern Hungary, known for its heavy industry. With a population of 161,265 (1 Jan 2014) Miskolc is the List of cities and towns in Hungary#Largest cities in Hungary, fourth largest city in Hungary (behind Budapest, Debrecen, and Szeged). It is also the county capital of Borsod-Abaúj-Zemplén and the Regions of Hungary, regional centre of Northern Hungary. Etymology The name derives from ''Miško'', Slavic languages, Slavic form of Michael (given name), Michael. ''Miškovec'' → ''Miskolc'' with the same development as ''Lipovec'' → ''Lipólc'', ''Lipóc''. The name is associated with the Miskolc (genus), Miskolc clan (also Miskóc or Myscouch, Slovak language, Slovak Miškovec, plural Miškovci) named after the settlement or vice versa. Earliest mentions are ''que nunc vocatur Miscoucy'' (around 1200), ''de Myschouch'' (1225), ''Ponyt ...
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Lillafüred
Lillafüred (Miskolc-Lillafüred) is a town in Borsod-Abaúj-Zemplén county, Hungary. Officially, it is a part of Miskolc, though it is almost 12 kilometres away from the city, in the Bükk Mountains. Lillafüred is a tourist resort. History Count András Bethlen, the minister of agriculture, decided in the 1890s to build a holiday resort near Lake Hámori. The resort was named after his niece, Erzsébet (nicknamed: "Lilla") Vay, who was the sister of the then-ispán, or count, of Borsod County, :hu:Vay Elemér, Elemér Vay. The Palace Hotel was built by István Bethlen. Tourist attractions Palace Hotel (Palotaszálló) The Palace Hotel was designed by Kálmán Lux and built between 1927 and 1930 in neo-Renaissance style. One of the hotel's restaurants is named after Matthias Corvinus of Hungary, King Matthias. Its stained glass windows show the castles of historical Hungary. The hotel is surrounded by a large park with rare plants. Hanging gardens The hanging gardens are ...
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Hungary
Hungary ( hu, Magyarország ) is a landlocked country in Central Europe. Spanning of the Carpathian Basin, it is bordered by Slovakia to the north, Ukraine to the northeast, Romania to the east and southeast, Serbia to the south, Croatia and Slovenia to the southwest, and Austria to the west. Hungary has a population of nearly 9 million, mostly ethnic Hungarians and a significant Romani minority. Hungarian, the official language, is the world's most widely spoken Uralic language and among the few non-Indo-European languages widely spoken in Europe. Budapest is the country's capital and largest city; other major urban areas include Debrecen, Szeged, Miskolc, Pécs, and Győr. The territory of present-day Hungary has for centuries been a crossroads for various peoples, including Celts, Romans, Germanic tribes, Huns, West Slavs and the Avars. The foundation of the Hungarian state was established in the late 9th century AD with the conquest of the Carpathian Basin by Hungar ...
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Sándor Petőfi
Sándor Petőfi ( []; né Petrovics; sk, Alexander Petrovič; sr, Александар Петровић; 1 January 1823 – most likely 31 July 1849) was a Hungarian poet of Serbian origin and liberal revolutionary. He is considered Hungary's national poet, and was one of the key figures of the Hungarian Revolution of 1848. He is the author of the ''Nemzeti dal'' (National Song), which is said to have inspired the revolution in the Kingdom of Hungary that grew into a war for independence from the Austrian Empire. It is most likely that he died in the Battle of Segesvár, one of the last battles of the war. Early life Petőfi was born on the New Year's morning of 1823, in the town of Kiskőrös, Kingdom of Hungary. The population of Kiskőrös was predominantly of Slovak origin as a consequence of the Habsburgs' reconstruction policy designed to settle, where possible, non-Hungarians in areas devastated during the Turkish wars. His birth certificate, in Latin, gives his name as ...
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Palace Hotel (Palotaszálló)
Palace Hotel may refer to: Film *Palace Hotel (film) Places Australia *Palace Hotel, Broken Hill, New South Wales, a pub *Palace Hotel, Childers, Queensland * Palace Hotel, Perth, Western Australia *Palace Hotel, Kalgoorlie, Western Australia China *Peace Hotel South Building, formerly Palace Hotel, Shanghai Denmark *Palace Hotel (Copenhagen) Egypt *Sofitel Winter Palace Hotel, Luxor Finland *Palace Hotel, Helsinki Hungary *Palace Hotel, Miskolc, Hungary Japan * Palace Hotel, Tokyo Poland *Palace, a hotel in Poland used by the Gestapo during the Nazi occupation, where Jadwiga Apostoł was brought Portugal *Buçaco Palace, Serra do Buçaco, Mealhada Romania *Athenee Palace Hilton Bucharest Hotel Russia * Palace Hotel, Rostov-on-Don Slovenia *Kempinski Palace Portorož, formerly Palace Hotel Switzerland *Badrutt's Palace Hotel, St. Moritz, Switzerland Turkey * Mardan Palace, Lara, Antalya United Kingdom *Palace Hotel, Bristol, a pub *Palace Hotel, Buxton * Palace Hotel, ...
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Plant Fossil
Paleobotany, which is also spelled as palaeobotany, is the branch of botany dealing with the recovery and identification of plant remains from geological contexts, and their use for the biological reconstruction of past environments (paleogeography), and the evolutionary history of plants, with a bearing upon the evolution of life in general. A synonym is paleophytology. It is a component of paleontology and paleobiology. The prefix ''palaeo-'' means "ancient, old", and is derived from the Greek adjective , . Paleobotany includes the study of terrestrial plant fossils, as well as the study of prehistoric marine photoautotrophs, such as photosynthetic algae, seaweeds or kelp. A closely related field is palynology, which is the study of fossilized and extant spores and pollen. Paleobotany is important in the reconstruction of ancient ecological systems and climate, known as paleoecology and paleoclimatology respectively; and is fundamental to the study of green plant development ...
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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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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 stone * Dripstone, New South Wales Dripstone is a locality in Dubbo Regional Council, New South Wales, Australia Australia, officially the Commonwealth of Australia, is a sovereign country comprising the mainland of the Australian continent, the island of Tasmania, an ...
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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 ...
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Limestone Caves
Limestone ( calcium carbonate ) is a type of carbonate sedimentary rock which is the main source of the material lime. It is composed mostly of the minerals calcite and aragonite, which are different crystal forms of . Limestone forms when these minerals precipitate out of water containing dissolved calcium. This can take place through both biological and nonbiological processes, though biological processes, such as the accumulation of corals and shells in the sea, have likely been more important for the last 540 million years. Limestone often contains fossils which provide scientists with information on ancient environments and on the evolution of life. About 20% to 25% of sedimentary rock is carbonate rock, and most of this is limestone. The remaining carbonate rock is mostly dolomite, a closely related rock, which contains a high percentage of the mineral dolomite, . ''Magnesian limestone'' is an obsolete and poorly-defined term used variously for dolomite, for limestone co ...
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