Algemesí is a municipality in the comarca of Ribera Alta in the Valencian Community, Spain. The town of Algemesí is one of the major centres for the production of citruses in Spain, several cooperatives are based there; this is due to the mild climate and good irrigation coming from the Xuquer river, which passes through the city. Every September is celebrated the Festivity of “la Mare de Déu de la Salut”, declared as Intangible Cultural Heritage by UNESCO in 2011; the traditional Valencian dance called Muixeranga is a part of the festivity. The Museum os the Parties of Algemesí, venue of the network of museums of the Valencian Council looks for the consolidation of a major research center about the party. There some files are stored for the public consultation by photographic media with the most relevant aspects of the popular festivity. Among the expositive elements are “los misterios y martirios”, la “muixeranga”, “els bastonets”, “el ball de la carxofa i arquets”, “les pastoretes”, “el bolero”, “els tornejants”,“els volants”,“la Mare de Deu de la Salut” y la música.
La Mare de Déu de la Salut Festival” The Festivity of “la Mare de Déu de la Salut” presents a series of traditions which from 1247 through to 1905, were transmitted from generation to generation until they came to form what can now be considered a homage to cultural tradition. This event takes place in the historical parts of the city of Algemesí on the 7th and 8 September each year. Of special note is the great participation and involvement of the townsfolk of all ages in the event, through the many associations formed to meet the needs of the traditions and ritual acts that make up the festivity; the guilds, from which the age-old dances were born, underwent many changes with the industrial revolution in the late 19th Century, providing their members with a window onto other social and professional environments. These days, the ritual acts and traditions which call for a specific number of participants all have waiting lists. Positions on these lists are hereditary; the number of people joining in the dances which are open to any number of participants is growing constantly.
RECOGNITIONS UNESCO has recognized the ritual and community participation dimension of the Valencian celebration Our Lady of Health as part of the "intangible heritage of humanity". Event of Intangible Cultural Interest. Generalitat Valenciana, it is recorded in the Register of Assets of Cultural Interest of the Spanish Ministry of Culture, under code R-I-54-0000151-00000. Festivity of Touristic Interest. Spanish Ministry of Industry and Commerce. Spanish treasure of intangible cultural heritage. In 2009 the festivity received accreditation from the IBOCC as one of the 10 Treasures of Spain’s Intangible Cultural Heritage. Accredited as one of the 7 Valencian marvels. In 2008, the festivity received accreditation as one of the 7 Valencian marvels, in the section “Cultural events and intangible heritage”. Taurine week: Every year in late September in the town is built a wood rectangular bullring where the Fair of calves (the oldest and most important bullfighting and bullfighting on horse; the bullfighting ring is divided into 4 “cadafals” that come to auction and its cost is the basis of the budget of the Party and evening performances.
The bullring is a unique construction: each 9 September the “peñas” as are known the associations built the bullring just as it was done in 1943, with wood and strings as raw materials. Each “peña” built its own “cadafal>” parallel to the façade of the Major Square, so all the 29 “cadafals” form the rectangular square. The exhibition consists on eight runs and afternoon bullfightings on horseback; the schedule is as follows: during the morning they have the “correbous” from the pens to the square. After lunch, at the square of Salvador Castell, where the “peñas” have their booths. In the afternoon, more runs and they have dinner and nightly entertainment in the bullfightring Algemesí is twinned with: Riom, France Gangneung, South Korea
Sueca is a city in eastern Spain in the Valencian Community. It is situated on the left bank of the river Xúquer; the town of Sueca is separated from the Mediterranean Sea 11 kilometres to the east by the Serra de Cullera, though the municipality possesses 7 km of Mediterranean coastline. Some of the architecture shows Moorish roots—the flat roofs, view-turrets, horseshoe arches—and the area has an irrigation system dating from Moorish times. Rice processing is the principal industry, though oranges are exported. Mareny de Barraquetes Évreux, France Palafrugell, Spain Map and pictures of Sueca This article incorporates text from a publication now in the public domain: Chisholm, Hugh, ed.. "Sueca". Encyclopædia Britannica. 26. Cambridge University Press. P. 21
Valencia València, on the east coast of Spain, is the capital of the autonomous community of Valencia and the third-largest city in Spain after Madrid and Barcelona, with around 800,000 inhabitants in the administrative centre. Its urban area extends beyond the administrative city limits with a population of around 1.6 million people. Valencia is Spain's third largest metropolitan area, with a population ranging from 1.7 to 2.5 million depending on how the metropolitan area is defined. The Port of Valencia is the 5th busiest container port in Europe and the busiest container port on the Mediterranean Sea; the city is ranked at Beta-global city in World Cities Research Network. Valencia is integrated into an industrial area on the Costa del Azahar. Valencia was founded as a Roman colony by the consul Decimus Junius Brutus Callaicus in 138 BC, called Valentia Edetanorum. In 714 Moroccan and Arab Moors occupied the city, introducing their language and customs. Valencia was the capital of the Taifa of Valencia.
In 1238 the Christian king James I of Aragon conquered the city and divided the land among the nobles who helped him conquer it, as witnessed in the Llibre del Repartiment. He created a new law for the city, the Furs of Valencia, which were extended to the rest of the Kingdom of Valencia. In the 18th century Philip V of Spain abolished the privileges as punishment to the kingdom of Valencia for aligning with the Habsburg side in the War of the Spanish Succession. Valencia was the capital of Spain when Joseph Bonaparte moved the Court there in the summer of 1812, it served as capital between 1936 and 1937, during the Second Spanish Republic. The city is situated on the banks of the Turia, on the east coast of the Iberian Peninsula, fronting the Gulf of Valencia on the Mediterranean Sea, its historic centre is one of the largest in Spain, with 169 ha. Due to its long history, this is a city with numerous popular celebrations and traditions, such as the Fallas, which were declared as Fiestas of National Tourist Interest of Spain in 1965 and Intangible cultural heritage by UNESCO in November 2016.
From 1991 to 2015, Rita Barberá Nolla was the mayor of the city, yet in 2015, Joan Ribó from Coalició Compromís, became mayor. The original Latin name of the city was Valentia, meaning "strength", or "valour", the city being named according to the Roman practice of recognising the valour of former Roman soldiers after a war; the Roman historian Livy explains that the founding of Valentia in the 2nd century BC was due to the settling of the Roman soldiers who fought against an Iberian rebel, Viriatus. During the rule of the Muslim kingdoms in Spain, it had the nickname Medina at-Tarab according to one transliteration, or Medina at-Turab according to another, since it was located on the banks of the River Turia, it is not clear if the term Balansiyya was reserved for the entire Taifa of Valencia or designated the city. By gradual sound changes, Valentia has in Castilian and València in Valencian. In Valencian, the grave accent ⟨è⟩ /ɛ/ contrasts with the acute accent ⟨é⟩ /e/—but the word València is an exception to this rule.
It is spelled according to Catalan etymology. Valencia stands on the banks of the Turia River, located on the eastern coast of the Iberian Peninsula and the western part of the Mediterranean Sea, fronting the Gulf of Valencia. At its founding by the Romans, it stood on a river island in 6.4 kilometres from the sea. The Albufera, a freshwater lagoon and estuary about 11 km south of the city, is one of the largest lakes in Spain; the City Council bought the lake from the Crown of Spain for 1,072,980 pesetas in 1911, today it forms the main portion of the Parc Natural de l'Albufera, with a surface area of 21,120 hectares. In 1976, because of its cultural and ecological value, the Generalitat Valenciana declared it a natural park. Valencia has a subtropical Mediterranean climate with short mild winters and long and dry summers, its average annual temperature is 18.4 °C. In the coldest month, the maximum temperature during the day ranges from 14 to 21 °C, the minimum temperature at night ranges from 5 to 11 °C.
In the warmest month – August, the maximum temperature during the day ranges from 28–34 °C, about 22 to 23 °C at night. Similar temperatures to those experienced in the northern part of Europe in summer last about 8 months, from April to November. March is transitional, the temperature exceeds 20 °C, with an average temperature of 19.3 °C during the day and 10.0 °C at night. December and February are the coldest months, with average temperatures around 17 °C during the day and 8 °C at night. Valencia has one of the mildest winters in Europe, owing to its southern location on the Mediterranean Sea and the Foehn phenomenon; the January average is comparable to temperatures expected for May and September in the major cities of northern Europe. Sunshine duration hours are 2,696 per year, from 15
A lagoon is a shallow body of water separated from a larger body of water by barrier islands or reefs. Lagoons are divided into coastal lagoons and atoll lagoons, they have been identified as occurring on mixed-sand and gravel coastlines. There is an overlap between bodies of water classified as coastal lagoons and bodies of water classified as estuaries. Lagoons are common coastal features around many parts of the world. Lagoons are shallow elongated bodies of water separated from a larger body of water by a shallow or exposed shoal, coral reef, or similar feature; some authorities include fresh water bodies in the definition of "lagoon", while others explicitly restrict "lagoon" to bodies of water with some degree of salinity. The distinction between "lagoon" and "estuary" varies between authorities. Richard A. Davis Jr. restricts "lagoon" to bodies of water with little or no fresh water inflow, little or no tidal flow, calls any bay that receives a regular flow of fresh water an "estuary". Davis does state that the terms "lagoon" and "estuary" are "often loosely applied in scientific literature."
Timothy M. Kusky characterizes lagoons as being elongated parallel to the coast, while estuaries are drowned river valleys, elongated perpendicular to the coast; when used within the context of a distinctive portion of coral reef ecosystems, the term "lagoon" is synonymous with the term "back reef" or "backreef", more used by coral reef scientists to refer to the same area. Coastal lagoons are classified as inland bodies of water. Many lagoons do not include "lagoon" in their common names. Albemarle and Pamlico sounds in North Carolina, Great South Bay between Long Island and the barrier beaches of Fire Island in New York, Isle of Wight Bay, which separates Ocean City, Maryland from the rest of Worcester County, Banana River in Florida, Lake Illawarra in New South Wales, Montrose Basin in Scotland, Broad Water in Wales have all been classified as lagoons, despite their names. In England, The Fleet at Chesil Beach has been described as a lagoon. In Latin America, the term laguna in Spanish, which lagoon translates to, may be used for a small fresh water lake in a similar way a creek is considered a small river.
However, sometimes it is popularly used to describe a full-sized lake, such as Laguna Catemaco in Mexico, the third largest lake by area in the country. The brackish water lagoon may be thus explicitly identified as a "coastal lagoon". In Portuguese the same usage is found: lagoa may be a body of shallow sea water, or a small freshwater lake not linked to the sea. Lagoon is derived from the Italian laguna, which refers to the waters around Venice, the Lagoon of Venice. Laguna is attested in English by at least 1612, had been Anglicized to "lagune" by 1673. In 1697 William Dampier referred to a "Lake of Salt water" on the coast of Mexico. Captain James Cook described an island "of Oval form with a Lagoon in the middle" in 1769. Atoll lagoons form as coral reefs grow upwards while the islands that the reefs surround subside, until only the reefs remain above sea level. Unlike the lagoons that form shoreward of fringing reefs, atoll lagoons contain some deep portions. Coastal lagoons form along sloping coasts where barrier islands or reefs can develop off-shore, the sea-level is rising relative to the land along the shore.
Coastal lagoons do not form along steep or rocky coasts, or if the range of tides is more than 4 metres. Due to the gentle slope of the coast, coastal lagoons are shallow, they are sensitive to changes in sea level due to global warming. A relative drop in sea level may leave a lagoon dry, while a rise in sea level may let the sea breach or destroy barrier islands, leave reefs too deep under water to protect the lagoon. Coastal lagoons are young and dynamic, may be short-lived in geological terms. Coastal lagoons are common. In the United States, lagoons are found along more than 75 percent of the Gulf coasts. Coastal lagoons are connected to the open ocean by inlets between barrier islands; the number and size of the inlets, precipitation and inflow of fresh water all affect the nature of the lagoon. Lagoons with little or no interchange with the open ocean, little or no inflow of fresh water, high evaporation rates, such as Lake St. Lucia, in South Africa, may become saline. Lagoons with no connection to the open ocean and significant inflow of fresh water, such as the Lake Worth Lagoon in Florida in the middle of the 19th century, may be fresh.
On the other hand, lagoons with many wide inlets, such as the Wadden Sea, have strong tidal currents and mixing. Coastal lagoons tend to accumulate sediments from inflowing rivers, from runoff from the shores of the lagoon, from sediment carried into the lagoon through inlets by the tide. Large quantities of sediment may be be deposited in a lagoon when storm waves overwash barrier islands. Mangroves and marsh plants can facilitate the accumulation of sediment in a lagoon. Benthic organisms may destabilize sediments. River-mouth lagoons on mixed sand and gravel beaches form at the river-coast interface where a braided, although sometimes meandering, river interacts with a coastal environment, affected by longshore drift; the lagoons which form on the MSG coastlines are common on the east coast of the South Island of New Zealand and have long been referred to as hapua by the Māori. This classification differentiates hapua from similar lagoons located on the N
El Saler is a village in Valencia, Spain. It is part of the municipality of Valencia
A wetland is a distinct ecosystem, inundated by water, either permanently or seasonally, where oxygen-free processes prevail. The primary factor that distinguishes wetlands from other land forms or water bodies is the characteristic vegetation of aquatic plants, adapted to the unique hydric soil. Wetlands play a number of functions, including water purification, water storage, processing of carbon and other nutrients, stabilization of shorelines, support of plants and animals. Wetlands are considered the most biologically diverse of all ecosystems, serving as home to a wide range of plant and animal life. Whether any individual wetland performs these functions, the degree to which it performs them, depends on characteristics of that wetland and the lands and waters near it. Methods for assessing these functions, wetland ecological health, general wetland condition have been developed in many regions and have contributed to wetland conservation by raising public awareness of the functions and the ecosystem services some wetlands provide.
Wetlands occur on every continent. The main wetland types are swamp, marsh and fen. Many peatlands are wetlands; the water in wetlands is either brackish, or saltwater. Wetlands can be non-tidal; the largest wetlands include the Amazon River basin, the West Siberian Plain, the Pantanal in South America, the Sundarbans in the Ganges-Brahmaputra delta. The UN Millennium Ecosystem Assessment determined that environmental degradation is more prominent within wetland systems than any other ecosystem on Earth. Constructed wetlands are used to treat municipal and industrial wastewater as well as stormwater runoff, they may play a role in water-sensitive urban design. A patch of land that develops pools of water after a rain storm would not be considered a "wetland" though the land is wet. Wetlands have unique characteristics: they are distinguished from other water bodies or landforms based on their water level and on the types of plants that live within them. Wetlands are characterized as having a water table that stands at or near the land surface for a long enough period each year to support aquatic plants.
A more concise definition is a community composed of hydric soil and hydrophytes. Wetlands have been described as ecotones, providing a transition between dry land and water bodies. Mitsch and Gosselink write that wetlands exist "...at the interface between terrestrial ecosystems and aquatic systems, making them inherently different from each other, yet dependent on both."In environmental decision-making, there are subsets of definitions that are agreed upon to make regulatory and policy decisions. A wetland is "an ecosystem that arises when inundation by water produces soils dominated by anaerobic and aerobic processes, which, in turn, forces the biota rooted plants, to adapt to flooding." There are four main kinds of wetlands – marsh, swamp and fen. Some experts recognize wet meadows and aquatic ecosystems as additional wetland types; the largest wetlands in the world include the swamp forests of the Amazon and the peatlands of Siberia. Under the Ramsar international wetland conservation treaty, wetlands are defined as follows: Article 1.1: "...wetlands are areas of marsh, peatland or water, whether natural or artificial, permanent or temporary, with water, static or flowing, brackish or salt, including areas of marine water the depth of which at low tide does not exceed six metres."
Article 2.1: " may incorporate riparian and coastal zones adjacent to the wetlands, islands or bodies of marine water deeper than six metres at low tide lying within the wetlands." Although the general definition given above applies around the world, each county and region tends to have its own definition for legal purposes. In the United States, wetlands are defined as "those areas that are inundated or saturated by surface or groundwater at a frequency and duration sufficient to support, that under normal circumstances do support, a prevalence of vegetation adapted for life in saturated soil conditions. Wetlands include swamps, marshes and similar areas"; this definition has been used in the enforcement of the Clean Water Act. Some US states, such as Massachusetts and New York, have separate definitions that may differ from the federal government's. In the United States Code, the term wetland is defined "as land that has a predominance of hydric soils, is inundated or saturated by surface or groundwater at a frequency and duration sufficient to support a prevalence of hydrophytic vegetation adapted for life in saturated soil conditions and under normal circumstances supports a prevalence of such vegetation."
Related to this legal definitions, the term "normal circumstances" are conditions expected to occur during the wet portion of the growing season under normal climatic conditions, in the absence of significant disturbance. It is not uncommon for a wetland to be dry for long portions of the growing season. Wetlands can be dry during the dry season and abnormally dry periods during the wet season, but under normal environmental conditions the soils in a wetland will be saturated to the surface or inundated such that the soils become anaerobic, those conditions will persist through the wet portion of the growing season; the most important factor producing wetlands is flooding. The duration of flooding or prolonged soil saturation by groundwater determines whether the resulting wetland has aquatic, marsh or swamp vegetation