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Vallone Dei Mulini
Vallone dei Mulini or Valle dei Mulini (known in English as Valley of the Mills) is a historic valley in Sorrento, Italy. History The flour mills, built from stone as far back as the 13th century. Its name derived from its beginning function: to grind grain. The valley originates from the release of waters into a tufa plain about 37,000 years ago, following the eruption of the Campi Flegrei. A sawmill was providing sawn wood. It was in operation until the beginning of the tenth century. In 1866, Piazza Tasso was established, and it caused the mill and the surrounding sea to be isolated. The building was closed and abandoned in the 1940s. Geography It is located behind Piazza Tasso. The valley is carved by two rivers: Casarlano-Cesarano and S. Antonino. This also means that the humidity is very high. Characteristics It is considered one of the most enchanting views of the Sorrento Peninsula. It is known for its variety and unique plants. These plants settle within ferns. Poss ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sorrento, Italy
Sorrento (, ; nap, Surriento ; la, Surrentum) is a town overlooking the Bay of Naples in Southern Italy. A popular tourist destination, Sorrento is located on the Sorrentine Peninsula at the south-eastern terminus of the Circumvesuviana rail line, within easy access from Naples and Pompei. The town is widely known for its small ceramics, lacework and marquetry (woodwork) shops. The Sorrentine Peninsula has views of Naples, Vesuvius and the Isle of Capri. The Amalfi Drive, connecting Sorrento and Amalfi, is a narrow road along the high cliffs above the Tyrrhenian Sea. Ferries and hydrofoils connect the town to Naples, Amalfi, Positano, Capri and Ischia. Limoncello, a digestif made from lemon rinds, alcohol, water and sugar, is produced in Sorrento along with citrus fruit, wine, nuts and olives. History Origins The Roman name for Sorrento was . From the 8th century BC the area had the presence of a community of indigenous villages, which was a crossing point for Etruscan ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Valley
A valley is an elongated low area often running between Hill, hills or Mountain, mountains, which will typically contain a river or stream running from one end to the other. Most valleys are formed by erosion of the land surface by rivers or streams over a very long period. Some valleys are formed through erosion by glacier, glacial ice. These glaciers may remain present in valleys in high mountains or polar areas. At lower latitudes and altitudes, these glaciation, glacially formed valleys may have been created or enlarged during ice ages but now are ice-free and occupied by streams or rivers. In desert areas, valleys may be entirely dry or carry a watercourse only rarely. In karst, areas of limestone bedrock, dry valleys may also result from drainage now taking place cave, underground rather than at the surface. Rift valleys arise principally from tectonics, earth movements, rather than erosion. Many different types of valleys are described by geographers, using terms th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tufa
Tufa is a variety of limestone formed when carbonate minerals precipitate out of water in unheated rivers or lakes. Geothermally heated hot springs sometimes produce similar (but less porous) carbonate deposits, which are known as travertine. Tufa is sometimes referred to as (meteogene) travertine. It should not be confused with hot spring (thermogene) travertine. Tufa, which is calcareous, should also not be confused with tuff, a porous volcanic rock with a similar etymology that is sometimes also called "tufa". Classification and features Modern and fossil tufa deposits abound with wetland plants; as such, many tufa deposits are characterised by their large macrobiological component, and are highly porous. Tufa forms either in fluvial channels or in lacustrine environments. Ford and Pedley (1996) provide a review of tufa systems worldwide. Fluvial deposits Deposits can be classified by their depositional environment (or otherwise by vegetation or petrographically). Pedle ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Campi Flegrei
The Phlegraean Fields ( it, Campi Flegrei ; nap, Campe Flegree, from Ancient Greek 'to burn') is a large region of supervolcanic calderas situated to the west of Naples, Italy. It was declared a regional park in 2003. The area of the caldera consists of 24 craters and volcanic edifices; most of them lie under water. Hydrothermal activity can be observed at Lucrino, Agnano and the town of Pozzuoli. There are also effusive gaseous manifestations in the Solfatara crater, the mythological home of the Roman god of fire, Vulcan. This area is monitored by the Vesuvius Observatory. It is considered a supervolcano. The area also features bradyseismic phenomena, which are most evident at the Macellum of Pozzuoli (misidentified as a temple of Serapis): bands of boreholes left by marine molluscs on marble columns show that the level of the site in relation to sea level has varied. Geological phases Three geological phases or periods are recognised and distinguished. * The First P ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Piazza Tasso, Sorrento
Piazza Tasso is a central place and square in Sorrento in the south of Italy. The square is named after the poet Torquato Tasso (1544–1595). In the main square, well known as Largo of the Caste, is the yellow-painted Baroque Carmelite Church del Carmine, holding within its interior a painting by Onofrio Avellino of the Virgin Mary with Saint Simon Stock and angels.Best of SorrentoChiesa del Carmine Sorrento accessed 26 September 2022 On the square stands a statue of S. Antonino Abbate. The shopping street Via San Cesareo leads off the square to the west. Also near Piazza Tasso is the Palazzo Correale, now also a museum, Museum Correale Museum Correale (Italian: ''Museo Correale di Terranova'') is a museum in Sorrento in the south of Italy. The museum is situated in a patrician villa, surrounded by a citrus grove, with a terrace of Belvedere that overlooks the Gulf of Naples. Th .... References External links Piazza TassoImagesImages Statue of S. Antonino Abbate {{coord, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sorrento Peninsula
The Sorrento Peninsula or Sorrentine Peninsula is a peninsula located in southern Italy which separates the Gulf of Naples to the north from the Gulf of Salerno to the south. Geography Overview The peninsula is named after its main town, Sorrento, which is located on the north (Gulf of Naples) coast. The Amalfi Coast is located on the southern side. The Lattari Mountains form the geographical backbone of the peninsula. The island of Capri lies off the western tip of the peninsula in the Tyrrhenian Sea. The whole area is an important tourist destination. Tuesday, 17 January 2017 Municipalities 9 comunes of the peninsula are in the territory of the province of Naples and 12 comunes are in the province of Salerno. Transportation Airports The nearest airports are: * Naples International (NAP) * Salerno Costa d'Amalfi (QSR) See also *Amalfi Coast *Capri *Gulf of Naples *Gulf of Salerno *Monti Lattari *Punta Campanella Lighthouse *Sant'Agata sui Due Golfi *Sirenuse *Souther ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tuff
Tuff is a type of rock made of volcanic ash ejected from a vent during a volcanic eruption. Following ejection and deposition, the ash is lithified into a solid rock. Rock that contains greater than 75% ash is considered tuff, while rock containing 25% to 75% ash is described as tuffaceous (for example, ''tuffaceous sandstone''). Tuff composed of sandy volcanic material can be referred to as volcanic sandstone. Tuff is a relatively soft rock, so it has been used for construction since ancient times. Because it is common in Italy, the Romans used it often for construction. The Rapa Nui people used it to make most of the ''moai'' statues on Easter Island. Tuff can be classified as either igneous or sedimentary rock. It is usually studied in the context of igneous petrology, although it is sometimes described using sedimentological terms. Tuff is often erroneously called tufa in guidebooks and in television programmes. Volcanic ash The material that is expelled in a volcanic ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Valleys Of Italy
A valley is an elongated low area often running between Hill, hills or Mountain, mountains, which will typically contain a river or stream running from one end to the other. Most valleys are formed by erosion of the land surface by rivers or streams over a very long period. Some valleys are formed through erosion by glacier, glacial ice. These glaciers may remain present in valleys in high mountains or polar areas. At lower latitudes and altitudes, these glaciation, glacially formed valleys may have been created or enlarged during ice ages but now are ice-free and occupied by streams or rivers. In desert areas, valleys may be entirely dry or carry a watercourse only rarely. In karst, areas of limestone bedrock, dry valleys may also result from drainage now taking place cave, underground rather than at the surface. Rift valleys arise principally from tectonics, earth movements, rather than erosion. Many different types of valleys are described by geographers, using terms th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
