Gellért Hill
Gellért Hill (; ; ) is a high hill overlooking the Danube in Budapest, Hungary. It is located in the 1st and the 11th districts. The hill was named after Saint Gerard who was thrown to death from the hill. The famous Hotel Gellért and the Gellért Baths can be found in ''Gellért Square'' at the foot of the hill, next to Liberty Bridge. The Gellért Hill Cave is also located on the hill, facing the hotel and the Danube. At the top of the hill, the Citadella (''English: citadel'') can be found with a nice panoramic view of the city. Origin of the name The first recorded names of the hill in the Middle Ages were ''Kelen-hegy'', ''Pesti-hegy (English: Pest Hill)'' and ''Blocksberg''. Since the 15th century, it has been called (lit. ''the hill of St. Gerard''), in reference to the legend of the death of St. Gerard (), Bishop of Csanád. The bishop was assassinated by the pagans during the great pagan rebellion in 1046. He was allegedly put in a barrel and rolled d ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Danube
The Danube ( ; see also #Names and etymology, other names) is the List of rivers of Europe#Longest rivers, second-longest river in Europe, after the Volga in Russia. It flows through Central and Southeastern Europe, from the Black Forest south into the Black Sea. A large and historically important river, it was once a frontier of the Roman Empire. In the 21st century, it connects ten European countries, running through their territories or marking a border. Originating in Germany, the Danube flows southeast for , passing through or bordering Austria, Slovakia, Hungary, Croatia, Serbia, Romania, Bulgaria, Moldova, and Ukraine. Among the many List of cities and towns on the river Danube, cities on the river are four national capitals: Vienna, Bratislava, Budapest, and Belgrade. Its drainage basin amounts to and extends into nine more countries. The Danube's longest headstream, the Breg (river), Breg, rises in Furtwangen im Schwarzwald, while the river carries its name from its ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Paganism
Paganism (, later 'civilian') is a term first used in the fourth century by early Christians for people in the Roman Empire who practiced polytheism, or ethnic religions other than Christianity, Judaism, and Samaritanism. In the time of the Roman Empire, individuals fell into the pagan class either because they were increasingly rural and provincial relative to the Christian population, or because they were not '' milites Christi'' (soldiers of Christ).J. J. O'Donnell (1977)''Paganus'': Evolution and Use, ''Classical Folia'', 31: 163–69. Alternative terms used in Christian texts were '' hellene'', '' gentile'', and '' heathen''. Ritual sacrifice was an integral part of ancient Greco-Roman religion and was regarded as an indication of whether a person was pagan or Christian. Paganism has broadly connoted the "religion of the peasantry". During and after the Middle Ages, the term ''paganism'' was applied to any non-Christian religion, and the term presumed a belief in fal ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Hot Spring
A hot spring, hydrothermal spring, or geothermal spring is a Spring (hydrology), spring produced by the emergence of Geothermal activity, geothermally heated groundwater onto the surface of the Earth. The groundwater is heated either by shallow bodies of magma (molten rock) or by circulation through fault (geology), faults to hot rock deep in the Earth's crust. Hot spring water often contains large amounts of dissolved minerals. The chemistry of hot springs ranges from acid sulfate springs with a pH as low as 0.8, to alkaline chloride springs saturated with silica, to bicarbonate springs saturated with carbon dioxide and carbonate minerals. Some springs also contain abundant dissolved iron. The minerals brought to the surface in hot springs often feed communities of extremophiles, microorganisms adapted to extreme conditions, and it is possible that life on Earth had its origin in hot springs. Humans have made use of hot springs for bathing, relaxation, or medical therapy for th ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Tectonics
Tectonics ( via Latin ) are the processes that result in the structure and properties of the Earth's crust and its evolution through time. The field of ''planetary tectonics'' extends the concept to other planets and moons. These processes include those of orogeny, mountain-building, the growth and behavior of the strong, old cores of continents known as cratons, and the ways in which the relatively rigid tectonic plate, plates that constitute the Earth's outer shell interact with each other. Principles of tectonics also provide a framework for understanding the earthquake and volcanic belts that directly affect much of the global population. Tectonic studies are important as guides for economic geology, economic geologists searching for fossil fuels and ore deposits of metallic and nonmetallic resources. An understanding of tectonic principles can help geomorphology, geomorphologists to explain Erosion and tectonics, erosion patterns and other Earth-surface features. Ma ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Pleistocene
The Pleistocene ( ; referred to colloquially as the ''ice age, Ice Age'') is the geological epoch (geology), epoch that lasted from to 11,700 years ago, spanning the Earth's most recent period of repeated glaciations. Before a change was finally confirmed in 2009 by the International Union of Geological Sciences, the cutoff of the Pleistocene and the preceding Pliocene was regarded as being 1.806 million years Before Present (BP). Publications from earlier years may use either definition of the period. The end of the Pleistocene corresponds with the end of the last glacial period and also with the end of the Paleolithic age used in archaeology. The name is a combination of Ancient Greek () 'most' and (; Latinized as ) 'new'. The aridification and cooling trends of the preceding Neogene were continued in the Pleistocene. The climate was strongly variable depending on the glacial cycle, oscillating between cold Glacial period, glacial periods and warmer Interglacial, int ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Late Triassic
The Late Triassic is the third and final epoch (geology), epoch of the Triassic geologic time scale, Period in the geologic time scale, spanning the time between annum, Ma and Ma (million years ago). It is preceded by the Middle Triassic Epoch and followed by the Early Jurassic Epoch. The corresponding series (stratigraphy), series of rock beds is known as the Upper Triassic. The Late Triassic is divided into the Carnian, Norian and Rhaetian Geologic time scale, ages. Many of the first dinosaurs evolved during the Late Triassic, including ''Plateosaurus'', ''Coelophysis'', ''Herrerasaurus'', and ''Eoraptor''. The Triassic–Jurassic extinction event began during this epoch and is one of the five major mass extinction events of the Earth. Etymology The Triassic was named in 1834 by Friedrich August von Namoh, Friedrich von Alberti, after a succession of three distinct rock layers (Greek meaning 'triad') that are widespread in southern Germany: the lower Buntsandstein (colourful ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Main Dolomite
Main Dolomite (, , ) is a lithostratigraphic unit in the Alps of Europe. Formation was defined by K.W. Gümbel in 1857. Middle to Late Triassic sedimentary record in the Alpine realm is characterized by presence of various masses of dolomitic rock formations. In the Northern Calcareous Alps the dolomitic mass of Ladinian - Norian age is divided by the Carnian sandstones and shales of Lunz Formation to the Ladinian - Carnian Wetterstein Dolomite and Norian Main Dolomite.Tollmann, A., 1976: Analyse des klassischen nordalpinen Mesozoikums, Wien, Franz Deuticke, 580 pp. The Main Dolomite reaches higher thickness than underlying dolomites in Alps, therefore it is considered as more important "Main". Extent The formation is found in: * the Northern Limestone Alps and Southern Limestone Alps of the Limestone Alps, a mountain system of the western and Central Eastern Alps. * the Apennines in Italy * the Western Carpathians (Tatric, Fatric, Hronic, Silicic units) Description It ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Sashegy
Sashegy (aka Sas-hegy, ; lit. "Eagle Hill") is a hill and neighbourhood in Budapest, Hungary. It is a green, upper middle class area in Buda with expensive family homes. Administratively Sashegy is divided between the Újbuda, 11th and the Hegyvidék, 12th districts of Budapest. Maps * The streets on Google Map* Near view on Googl The borders of Sashegy are: Hegyalja út from Dayka Gábor utca - Kálló esperes utca - Hegyalja út - Budaörsi út - Brassó út - Dayka Gábor utca until Hegyalja út. Name The present-day name was given to the hill in 1847 when the geographical features of the Buda Hills were renamed by the initiative of Hungarian philologist Gábor Döbrentei. ''Sashegy'' is the translation of the former German name, ''Adlerberg''. According to a popular legend a parade was held on 2 September 1686 by the victorious Christian armies after capturing Buda Castle from the Ottoman Turks. During the parade eagles flew from the hill nearby towards the castle. Medie ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Buda Hills
The Buda Hills ( Hungarian: ''Budai-hegység'') are a low mountain range of numerous hills which dot the Buda side of Budapest, capital of Hungary. The most famous ones located within city limits are Gellért Hill, Castle Hill, Rózsadomb, , János Hill, and Eagle Hill. These hills consist of both nature and residential areas. Geology The Budaörs dolomite of Anisian-Carnian age (Triassic period) is the oldest formation which crops out in the Buda Hills. Younger Triassic succession is composed of cherty dolomite and limestone (basin facies), and dolomite combined with limestone (platform facies). The Triassic surface is composed of karstified carbonates, which are overlain by an Upper Eocene succession made of conglomerate beds. During the period from the terminal Cretaceous to Priabonian, the area was a karstic terrestrial environment displaying distinct relief differences. It was also the time when Triassic formations were eroded. The continental period (ended by t ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Pilgrimage
A pilgrimage is a travel, journey to a holy place, which can lead to a personal transformation, after which the pilgrim returns to their daily life. A pilgrim (from the Latin ''peregrinus'') is a traveler (literally one who has come from afar) who is on a journey to a holy place. Typically, this is a physical journey (often on foot) to some place of special significance to the adherent of a particular religious belief system. Background Pilgrimages frequently involve a journey or search of morality, moral or spirituality, spiritual significance. Typically, it is a journey to a shrine or other location of importance to a person's beliefs and faith, although sometimes it can be a metaphorical journey into someone's own beliefs. Many religions attach spiritual importance to particular places: the place of birth or death of founders or saints, or to the place of their "calling" or spiritual awakening, or of their connection (visual or verbal) with the divine, to locations where ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Bektashi
Bektashism (, ) is a tariqa, Sufi order of Islam that evolved in 13th-century western Anatolia and became widespread in the Ottoman Empire. It is named after the wali, ''walī'' "saint" Haji Bektash Veli, with adherents called Bektashis. The Bektashi community is currently led by Baba Mondi, the eighth Bektashi Dedebabate, ''Dedebaba'', whose seat is at the order’s World Headquarters of the Bektashi, headquarters in Tirana, Albania. The Bektashis were originally one of many Sufi orders within Sunni Islam. By the 16th century, the order had adopted some tenets of Twelver Shi'ism—including veneration of Ali, the cousin and son-in-law of the Prophets and messengers in Islam, Prophet Muhammad, and the Twelve Imams—as well as a variety of syncretic beliefs. The Bektashis acquired political importance in the 15th century when the order dominated the Janissary Corps. After the foundation of Turkey, the country's leader, Mustafa Kemal Atatürk, banned religious institutions t ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |