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Grotta Del Cavallone
The Grotta del Cavallone, also known as the Grotta della Figlia di Jorio, is a cave located near Lama dei Peligni, in the province of Chieti, Abruzzo, Italy. It is open during the warmer months; an admission fee is charged. Overview The cave lies within the mountains of the Majella National Park, and is accessed via cable car. The cave is 10–20 meters wide and nearly the same height throughout, with numerous speleothems including stalagmites, flowstone, and rimstone pools. It has electric lighting with rough paths, concrete steps, and iron bridges. Gabriele D'Annunzio employed the cave in the first act of his tragedy "La figlia di Iorio". Gallery File:Cable Car Cavallone Cave IMG 0145.jpg, Arrive station of cable car - Grotta del Cavallone File:Grotta del Cavallone IMG 0176.jpg, Gate of the "Grotta del Cavallone" See also *List of caves *List of caves in Italy The following article shows a list of caves in Italy. Overview Main concentration of Italian caves ( it, grotte ...
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La Figlia Di Iorio
''La figlia di Iorio'' (''The Daughter of Iorio''), sometimes written as ''La figlia di Jorio'', is an opera in three acts by Alberto Franchetti to a libretto by Gabriele D'Annunzio. The libretto is a very close rendering of D'Annunzio's play of the same name. ''La figlia di Iorio'' premiered at La Scala on 29 March 1906, conducted by Leopoldo Mugnone. Although the play, which had premiered two years earlier, was considered one of D'Annunzio's greatest works, the opera did not achieve a comparable success and has been rarely performed since its day.An opera by Ildebrando Pizzetti with the same title, and again set to D'Annunzio's play, premiered at the Teatro San Carlo in Naples in 1954. Roles Synopsis The story is set in the small town in Abruzzo: Lama dei Peligni. Near the Grotta del Cavallone, lives a wealthy family in decline: the Sangro of Roio del Sangro. The father Lazaro di Roio is happy because his young son Aligi is getting married with a rich woman of the country. ...
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Stalagmite
A stalagmite (, ; from the Greek , from , "dropping, trickling") is a type of rock formation that rises from the floor of a cave due to the accumulation of material deposited on the floor from ceiling drippings. Stalagmites are typically composed of calcium carbonate, but may consist of lava, mud, peat, pitch, sand, sinter, and amberat (crystallized urine of pack rats). The corresponding formation hanging down from the ceiling of a cave is a stalactite. Mnemonics have been developed for which word refers to which type of formation; one is that ''stalactite'' has a C for "ceiling", and ''stalagmite'' has a G for "ground", another is that, as with ants in the pants, the mites go up and the tights (tites) come down. Formation and type Limestone stalagmites The most common stalagmites are speleothems, which usually form in limestone caves. Stalagmite formation occurs only under certain pH conditions within the cavern. They form through deposition of calcium carbonate ...
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Show Caves In Italy
Show or The Show may refer to: Competition, event, or artistic production * Agricultural show, associated with agriculture and animal husbandry * Animal show, a judged event in the hobby of animal fancy ** Cat show ** Dog show ** Horse show ** Specialty show, a dog show which reviews a single breed *Show, an artistic production, such as: ** Concert ** Radio show ** Talk show ** Television show ** Theatre production * Trade fair or trade show Arts, entertainment, and media Films * ''The Show'' (1922 film), starring Oliver Hardy * ''The Show'' (1927 film), directed by Tod Browning * ''The Show'' (1995 film), a hip hop documentary * ''The Show'' (2017 film), an American satirical drama * ''The Show'' (2020 film), a British mystery film Album * ''Show'' (The Cure album), 1993 * ''Show'' (The Jesus Lizard album), 1994 * ''The Show'' (album), a 2008 album by eMC Songs * "The Show" (Doug E. Fresh song) * "The Show" (Girls Aloud song) * "The Show" (Lenka song) * "The ...
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Landforms Of Abruzzo
A landform is a natural or anthropogenic land feature on the solid surface of the Earth or other planetary body. Landforms together make up a given terrain, and their arrangement in the landscape is known as topography. Landforms include hills, mountains, canyons, and valleys, as well as shoreline features such as bays, peninsulas, and seas, including submerged features such as mid-ocean ridges, volcanoes, and the great ocean basins. Physical characteristics Landforms are categorized by characteristic physical attributes such as elevation, slope, orientation, stratification, rock exposure and soil type. Gross physical features or landforms include intuitive elements such as berms, mounds, hills, ridges, cliffs, valleys, rivers, peninsulas, volcanoes, and numerous other structural and size-scaled (e.g. ponds vs. lakes, hills vs. mountains) elements including various kinds of inland and oceanic waterbodies and sub-surface features. Mountains, hills, plateaux, and plains are the fou ...
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Caves Of Italy
The following article shows a list of caves in Italy. Overview Main concentration of Italian caves ( it, grotte, singular: ''grotta'') is close to the Alps and the Apennine Mountains, principally due to karst. The main Italian tourist caves are Castellana and Frasassi. Other notable show caves are Pertosa, the Wind Cave, the Giant Cave, Castelcivita, Villanova, Toirano and Pastena. Caves The caves are listed by alphabetical order and there are shown the main tourist caves and other notable (e.g. archaeological or paleontological) underground voids. Notes and references See also *Grotto *List of caves External links Index of the show caves of ItalyPhotos of Italian caveson Flickr {{Authority control Italy Caves 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 ...
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List Of Caves In Italy
The following article shows a list of caves in Italy. Overview Main concentration of Italian caves ( it, grotte, singular: ''grotta'') is close to the Alps and the Apennine Mountains, principally due to karst. The main Italian tourist caves are Castellana and Frasassi. Other notable show caves are Pertosa, the Wind Cave, the Giant Cave, Castelcivita, Villanova, Toirano and Pastena. Caves The caves are listed by alphabetical order and there are shown the main tourist caves and other notable (e.g. archaeological or paleontological) underground voids. Notes and references See also * Grotto *List of caves External links Index of the show caves of ItalyPhotos of Italian caveson Flickr {{Authority control Italy Caves 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 ... ...
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List Of Caves
This is a list of caves of the world that have articles or that are properly cited. They are sorted by continent and then country. Caves which are in overseas territories on a different continent than the home country are sorted by the territory's continent and name. Africa File:Cango Caves, Western Cape (6253225986).jpg, The Cango caves in western cape. File:African cave paintings.jpg, African cave paintings. File:Lithic Industries at Blombos Cave, Southern Cape, South Africa (c. 105 – 90 Ka).jpg, Lithic Industries at Blombos Cave, Southern Cape, South Africa. File:Wonder Caves Praying Mary.JPG, Wonder Caves Praying Mary. Algeria * Aïn Taïba * Anou Achra Lemoun * Anou Boussouil * Anou Ifflis * Anou Timedouine * Gueldaman caves * Ghar Boumâaza * Grotte de Cervantes * Kef Al Kaous * Rivière De La Tafna Botswana * Gcwihaba * Rhino Cave Cameroon * Gouffre de Mbilibekon * Grottes de Linté * Grotte de Loung * Grotte de Mfouda * Grotte Fovu
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Rimstone
Rimstone, also called gours, is a type of speleothem (cave formation) in the form of a stone dam. Rimstone is made up of calcite and other minerals that build up in cave pools. The formation created, which looks like stairs, often extends into flowstone above or below the original rimstone. Often, rimstone is covered with small, micro-gours on horizontal surfaces. Rimstone basins may form terraces that extend over hundreds of feet, with single basins known up to 200 feet long from Tham Xe Biang Fai in Laos. Formation Rimstone dams form where there is some gradient, and hence flow, over the edge of a pool. Crystallization begins to occur at the air/water/rock interface. The turbulence caused by flow over the edge of the building dam may contribute to the outgassing or loss of carbon dioxide from water, and result in precipitation of mineral on this edge. When dams form under running water, they tend to be higher when the passage is steeper. Shallow-gradient dams tend to be lower a ...
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Flowstone
Flowstones are sheetlike deposits of calcite or other carbonate minerals, formed where water flows down the walls or along the floors of a cave. They are typically found in "solution caves", in limestone, where they are the most common speleothem. However, they may form in any type of cave where water enters that has picked up dissolved minerals. Flowstones are formed via the degassing of vadose percolation waters. Flowstone may also form on manmade structures as a result of calcium hydroxide being leached from concrete, lime or mortar. These secondary deposits created outside the cave environment, which mimic the shapes and forms of speleothems, are classified as "calthemites" and are associated with concrete degradation.Smith, G.K., (2016). “Calcite Straw Stalactites Growing From Concrete Structures”, Cave and Karst Science, Vol.43, No.1, P.4-10, (April 2016), British Cave Research Association, ISSN 1356-191X. Formation Flowing films of water that move along floors or do ...
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Speleothems
A speleothem (; ) is a geological formation by mineral deposition (geology), deposits that accumulate over time in natural caves. Speleothems most commonly form in calcareous caves due to carbonate dissolution reactions. They can take a variety of forms, depending on their depositional history and environment. Their chemical composition, gradual growth, and preservation in caves make them useful paleoclimatology, paleoclimatic proxies. Chemical and physical characteristics More than 300 variations of cave mineral deposits have been identified. The vast majority of speleothems are calcareous, composed of calcium carbonate (CaCO3) minerals (calcite or aragonite). Less commonly, speleothems are made of calcium sulfate (gypsum or mirabilite) or opal. Speleothems of pure calcium carbonate or calcium sulfate are translucent and colorless. The presence of iron oxide or copper provides a reddish brown color. The presence of manganese oxide can create darker colors such as black or dark b ...
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Lama Dei Peligni
Lama dei Peligni is a ''comune'' and town in the Province of Chieti in the Abruzzo region of Italy with 1,155 inhabitants. It is also part of the Aventino-Medio Sangro mountain community and the municipal territory is included in the Majella National Park. The town, known to naturalists as the country of chamois, is located in a florofaunal area of particular interest. History The territory has been inhabited since prehistoric, as amply testified by a series of rock paintings found in the caves of the area and from the remains of a village from the Neolithic period. In Contrada Fonterossi, right in the vicinity of the Neolithic site, the so-called " Uomo della Maiella" was found at the beginning of the 20th century, human remains of a prehistoric burial dating back to 7000–5000 BC. Name origin The toponym is of pre-Latin derivation, coming from the word ''lama''which literally meant 'counterbore', that is, 'land where water stagnates'; the addition referring to the Italic peo ...
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