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Gellért Hill
Gellért Hill ( hu, Gellért-hegy; german: Blocksberg; la, Mons Sancti Gerhardi tr, Gürz İlyas Bayırı) 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 ''Szent Gellért hegye'' (lit. ''the hill of St. Gerard''), referring to the legend about the death of St. Gerard. The bishop was assassinated by the pagans duri ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Danube
The Danube ( ; ) is a river that was once a long-standing frontier of the Roman Empire and today connects 10 European countries, running through their territories or being a border. Originating in Germany, the Danube flows southeast for , passing through or bordering Austria, Slovakia, Hungary, Croatia, Serbia, Romania, Bulgaria, Moldova, and Ukraine before draining into the Black Sea. Its drainage basin extends into nine more countries. The largest cities on the river are Vienna, Budapest, Belgrade and Bratislava, all of which are the capitals of their respective countries; the Danube passes through four capital cities, more than any other river in the world. Five more capital cities lie in the Danube's basin: Bucharest, Sofia, Zagreb, Ljubljana and Sarajevo. The fourth-largest city in its basin is Munich, the capital of Bavaria, standing on the Isar River. The Danube is the second-longest river in Europe, after the Volga in Russia. It flows through much of Central and Sou ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Vata Pagan Uprising
The Vata pagan uprising () was a Hungarian rebellion which, in 1046, brought about the overthrow of King Peter Urseolo, the martyrdom of Bishop Gerard of Csanád and the reinstatement of the Árpád dynasty on the Hungarian throne. Background Christianity had been introduced in Hungary by the King Stephen I of Hungary. Upon his death in 1038, he was succeeded by his sororal nephew Peter Urseolo, a Venetian noble. Through tax increases, and Urseolo's involvement with foreign powers, he proved to be an unpopular ruler. The Hungarian peasants, still largely pagan, suspected he was intent on bringing Hungary into the fold of the Holy Roman Empire. In a rebellion in 1041, Stephen's brother-in-law Samuel Aba took control of the throne, overthrowing Urseolo. Urseolo fled to Bavaria, in exile allying himself with German king and Holy Roman Emperor Henry III. In the years that followed, Aba's reign weakened, likely due to opposition from the church, who disliked his catering to pa ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cave
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, microorgani ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hot Spring
A hot spring, hydrothermal spring, or geothermal spring is a spring produced by the emergence of 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 faults to hot rock deep in the Earth's crust. In either case, the ultimate source of the heat is radioactive decay of naturally occurring radioactive elements in the Earth's mantle, the layer beneath the 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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tectonics
Tectonics (; ) are the processes that control the structure and properties of the Earth's crust and its evolution through time. These include the processes of mountain building, the growth and behavior of the strong, old cores of continents known as cratons, and the ways in which the relatively rigid plates that constitute the Earth's outer shell interact with each other. 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 geologists searching for fossil fuels and ore deposits of metallic and nonmetallic resources. An understanding of tectonic principles is essential to geomorphologists to explain erosion patterns and other Earth surface features. Main types of tectonic regime Extensional tectonics Extensional tectonics is associated with the stretching and thinning of the crust or the lithosphere. This type of tectonics is found ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Pleistocene
The Pleistocene ( , often referred to as the ''Ice age'') is the geological Epoch (geology), epoch that lasted from about 2,580,000 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 grc, label=none, πλεῖστος, pleīstos, most and grc, label=none, καινός, kainós (latinized as ), 'new'. At the end of the preceding Pliocene, the previously isolated North and South American continents were joined by the Isthmus of Panama, causing Great American Interchang ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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'', 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 sandstone'')'', t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Main Dolomite
Main Dolomite (german: Hauptdolomit, hu, Fődolomit, it, Dolomia Principale) 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 (Ta ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sashegy
Sashegy (aka Sas-hegy, german: Adlerberg; 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 11th and the 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. Mediev ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 Trassic 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 the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Pilgrimage
A pilgrimage is a journey, often into an unknown or foreign place, where a person goes in search of new or expanded meaning about their self, others, nature, or a higher good, through the experience. It can lead to a personal transformation, after which the pilgrim returns to their daily life. Background Pilgrimages frequently involve a journey or search of moral or 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 miracles were performed or witnessed, or locations where a deity is said to live or be "housed", or any site that is seen to have special spiritual powers. S ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bektashi
The Bektashi Order; sq, Tarikati Bektashi; tr, Bektaşi or Bektashism is an Islamic Sufi mystic movement originating in the 13th-century. It is named after the Anatolian saint Haji Bektash Wali (d. 1271). The community is currently led by Baba Mondi, the eighth Bektashi Dedebaba and headquartered in Tirana, Albania. Bektashism began as a Shia Islamic Sufi order in Anatolia, during the Ottoman Empire. In 1876, a Salih Nijazi was appointed as the "''baba''" or leader by prominent Bektashi members. After the foundation of the Turkish Republic, Kemal Atatürk banned religious institutions that weren't part of the Directorate of Religious Affairs. After this, the community's headquarters relocated to Albania. The order became involved in Albanian politics, and some of its members, including Ismail Qemali, were major leaders of the Albanian National Awakening. Bektashis believe in the Twelve Imams, Fourteen Innocents and the modern-day Dedebabas. In addition to the spiritua ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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