The Devesa the Beach Seaward Dune System Dune Slacks Inland Dune System the Banks of the Albufera the Devesa: Actions

Total Page:16

File Type:pdf, Size:1020Kb

The Devesa the Beach Seaward Dune System Dune Slacks Inland Dune System the Banks of the Albufera the Devesa: Actions The Devesa The beach Seaward dune system Dune slacks Inland dune system The banks of The Albufera The Devesa: actions From the 13th century to the end of the 19th century, when This is a system made up of 3 This system is formed by Between the seaward and These are the oldest dunes The sandy loam soil, in contact Since the decision was taken, almost 30 years ago, to recover they became the property of the State, the Devesa and the Al- sub-units that are closely inter- the dunes that are clos- the inland dune systems, which have much denser with the water, supports hy- the landscape and natural value of the Devesa, numerous ac- bufera belonged to the Crown, and their use was restricted. related, the submerged zone, the est to the beach. Here the there are a series of inter- plant cover. In the closest drophilous vegetation (reeds and tions have been carried out with this end in view. Since 1927, both areas have belonged to Valencia City Coun- foreshore and the backshore. The wind forms little depres- dunar depressions, or dune area to the seaward dune cane) that is known locally as One of the first measures adopted was the creation of a nurs- cil. In 1965, at the height of the Spanish tourist boom, a proc- submerged zone is the area with sions known as abrasion slacks, that are known lo- system which is still af- carrizal. ery of autoctonous plants to recover and repopulate the de- ess of urban development began which seriously altered the the greatest biodiversity; the posi- hollows. cally as mallades. These fected by the sea wind, is This ecosystem is the habitat for graded areas. Simultaneously the space was reorganized and ecosystems; the coastal dune sytem was almost completely de- A “ball” of posidonia remains formed donia meadows, nowadays very have impermeable soil the jaguarzal, open scrub- Saltmarsh mallow The harsh environmental a rich and varied fauna. Of spe- (Kosteletzkya pentacarpos) the most intensive recreational uses were concentrated in the stroyed to make way for the construction of a sea promenade, by the action of the sea reduced, which provide a habitat which means that pools land characterized by the Sea holly (Eryngium maritimum) conditions that character- Dune slack in autumn Open vegetation area cial importance are the migratory most damaged areas, while recreational use was limited, and The Devesa forms part of the Albufera Nature Reserve. It is the roads, car park, and housing (only the Muntanyar de La Rambla for algae, molluscs and fishes, are form in rainy periods. When the presence of the black rock rose, ize this ecosystem (strong sun- birds that use it for both food and access restricted, in the better preserved areas which were best conserved area of the dune system that made up the spit or and the Muntanyar de El Pujol areas survived). The dune slacks of especial importance. water evaporates as the tempera- with many sandy open spaces. In light, the constant sea wind, and shelter. These birds include the of greater natural value (La Creu, Muntanyar de la Rambla, sand bar which formed a barrier in the old Gulf of Valencia that (or depressions between dunes) known as mallades were filled ture rises, salt incrustations form the more inland sections where The foreshore, which is bathed by the mobility of the sand) make it reed warbler, the streaked fan- Muntanyar de El Pujol, Reserva de La Punta and the whole created the Albufera lagoon. The Albufera, which was previ- in with sand and repopulated with eucalyptus, and the inland on the surface. In this ecosystem the sea has a lesser influence, is seawater, has no vegetation, and necessary for the plants and ani- tail warbler, and the bearded tit, south sector of the Devesa). ously salt water and was used to provide salt for the city of Va- dune system was broken up by the construction of roads, car the vegetation grows in concentric the Mediterranean coastal maquia the backshore is dry and charac- mals of this habitat to adopt spe- which use the fine reed stems to lencia, has been a freshwater lagoon since the 17th century. parks, tower blocks and other infrastructure. circles depending on the degree of scrubland which is characterized Furthermore there have been numerous interventions aimed terized by plants that are adapted cial strategies in order to survive. weave their nests. Other frequent salinity: in the central area where by the great density, diversity and Martinet (Nycticorax nycticorax) at the recovery of the different environments affected by the Although it is not large (10km long by 1km wide) a range of It is important to emphasise that the degree of damage caused Seashell (Rubicardium sp.) to saline conditions. Both envi- Sand stock (Malcolmia littorea) Plants have flexible or horizontal Common Snipe (Gallinago gallinago) Dense vegetation made up of lianas visitors are the little grebe and the salinity is very high, there is and creepers extension of the plant cover. There process of urban development: climate and edaphic factors combine in this area to support by this urban development was different in the north and south ronments contain a wide range stems (stolons) so as not to be bro- the great crested grebe, which no vegetation, around this zone are various different plant strata in In the seaward dune system area roads, car parks and unused a diversity of flora, fauna and landscapes that give it an im- sections of the Devesa. The north of the Devesa (which extends of invertebrate fauna, which feeds ken by the wind, extensive roots build floating nests that are hid- the salt marsh vegetation grows, this ecosystems: moss (mosses and infrastructure have been eliminated along with the whole of portant, and internationally recognized, environmental value. to the Gola de El Pujol – the Pujol irrigation canal) was de- on the detritus provided by the to anchor them in the sand, leaves den among the vegetation by principally marsh samphire, and lichens), herbaceous, shrub, creep- the old promenade. The fore dunes of the Devesa have been (More than 400 different plant species have been identified in stroyed; infrastructure and housing was built. In the south (from sea. that are small or covered in little the banks, the mallard duck and in the outer area where the salin- ers and in the majority of cases completely reconstructed and the transitional dune system, the Devesa). the Gola de El Pujol to the Gola del Perellonet – the Perrellonet hairs to avoid dehydration, or several species of egret, such as ity is lowest there are rushes and trees, above all the Aleppo pine just behind them, has been completely recovered in the irrigation canal) was also destroyed and infrastructure was built fleshy leaves that can store water. the little bittern, the martinet and There are 5 different environments: Red seaweed Cottonweed (Otanthus maritimus) grasses. (Pinus halepensis). south sector. (LIFE-Enebro Project). but no housing. Currently, the southern part is better conserved Ruddy Darter Dragonfly the purple heron. There are also Grey heron (Ardea cinerea) Beach Many of the animals that live (Sympetrum sanguineum) Heather (Erica multiflora) and enjoys a greater degree of protection. Among the invertebrates, the most This environment is preferred by many small mammals such as the At the same time, the dune slacks have been recovered by The seaward dune system in this habitat have biological abundant are, together with small the majority of the predators to greater white-toothed shrew, the returning the sand to its original location; the seaward dune Dune slacks (depressions between dunes) The process of urban development almost destroyed the De- rhythms involving twilight or noc- crustaceans and snails, insects that rest during the day. The common white-toothed pygmy shrew, the system. The inland dune system vesa as a natural space, but at the end of the 1970s the process turnal activity to avoid the high spend all or part of their life cycle or small spotted genet, the fox and brown rat and the southern water Furthermore, many of the roads and car parks and infrastruc- The banks of the Albufera of development was stopped and in 1980 the Valencia City daytime sand temperatures. They in the pools of water (water bee- the long-eared owl wait for twilight vole. ture that had been constructed in the inland dune system Council created the Devesa-Albufera Technical Office which remain buried during the day tles, dragonflies, water bugs…). hidden in the dense vegetation, be- have been reduced or eliminated, thus achieving little by was responsible for the management, conservation and recov- Seashell (Chlamys sp.) Oviparous sharks lay eggs and Sand Viper’s Gloss (Echium sabulicola) like the dung beetle, or attached leave hatching to destiny. The Among the vertebrates the Iberian fore going out to look for prey. little the integration of the recovered areas with the rest of ery of the space. to the leaves of plants, such as Water beetle (Ditiscus sp.) Myrtle (Myrtus communis) Red-crested duck (Netta rufina) eggs have a thick rubbery case green frog and the water snake some snails, and in the evening the environment. From that moment a series of measures were initiated that or shell. In general the eggs are are the most common. This area laid in pairs. The embryos are they come out or climb down to The feathers of an is frequented by meadow birds All the actions are always accompanied by extensive informa- aimed at the conservation of the least affected areas and the nourished by the egg yolk. feed. Some other animals such as adult flamingo tion campaigns, together with a range of educational and cul- acceleration of the natural regeneration of the most affected with long beaks that allow them range from pink the red-tailed spiny-footed lizard, tural, with the aim of promoting the natural value of the area, areas.
Recommended publications
  • Sistema Acuifero De La Plana De Valencia
    COMPORTAMIENTO DE LOS ACUÍFEROS ANTE ACTUACIONES DE SEQUÍA PARA USO AGRÍCOLA EN LA CUENCA DEL JÚCAR SEXTO INFORME PERIÓDICO MES DE OCTUBRE Noviembre 2006 COMPORTAMIENTO DE LOS ACUÍFEROS ANTE LAS ACTUACIONES DE SEQUÍA PARA USO AGRÍCOLA EN LA CUENCA DEL JÚCAR SEXTO INFORME PERIÓDICO MES DE OCTUBRE Noviembre 2006 El proyecto cuyos resultados se exponen en este informe se inscribe dentro del Convenio de Asistencia Técnica subscrito entre la Confederación Hidrográfica del Júcar y el Instituto Geológico y Minero de España, y ha sido realizado por el siguiente equipo técnico: Dirección y supervisión D. Bruno J. Ballesteros Navarro (IGME) Equipo de trabajo D. José María Pernía Llera (IGME) D. José Antonio Domínguez Sánchez (IGME) Dña. Olga García Menéndez (IGME) Dña. Elisabeth Díaz Losada (IGME) D. José María Esnaola Navarro (Colaborador) Dña. Teresa Espinós Bernal (IGME) D. Horacio Higueras García (IGME) ÍNDICE 1. INTRODUCCIÓN............................................................................................................ 1 2. OBJETIVOS DEL INFORME ....................................................................................... 2 3. METODOLOGÍA EMPLEADA .................................................................................... 3 4. MARCO GEOGRÁFICO DE LAS UNIDADES HIDROGEOLÓGICAS ................ 4 5. ACUÍFEROS CONTROLADOS Y DATOS UTILIZADOS ....................................... 6 6. RED ESPECÍFICA DE SEQUÍA PARA EL CONTROL DE ACUÍFEROS. CARACTERÍSTICAS E INCIDENCIAS.............................................................................
    [Show full text]
  • El Regadío Tradicional De La Ribera Alta Del Xúquer Capítulo 1
    II EL REGADÍO TRADICIONAL DE LA RIBERA ALTA DEL XÚQUER CAPÍTULO 1 EL REGADÍO EN LA RIBERA ALTA DEL Como singularidad estructural, el Xúquer no ocupa el punto más bajo de su valle, de este sector del gran llano de inundación que es XÚQUER. EL MARGEN DERECHO la Ribera, sino que igual que hemos visto en la Ribera Baixa discurre a mayor altitud que las tierras inmediatas. Ello se debe a la mayor Antonio Furió Diego sedimentación de materiales en el propio cauce del río o en sus márge- Luis Pablo Martínez nes que en las tierras inundables, ya que son más frecuentes los momentos en que el río va lleno que los momentos en que se desborda. El llano de Departament d'Història Medieval inundación adquiere así una forma convexa en la que el Xúquer ocupa la Universitat de València parte más alta y el barranco de Barxeta, que discurre en buena medida en paralelo hasta converger con él, la más honda. En dos de los cortes Dos ríos, un barranco y una calzada transversales practicados por Vicent Ferrer, la superficie baja de los 24 La Ribera del Xúquer, lo hemos dicho ya en otro capítulo de m y 27 m sobre el nivel del mar, al lado del río, a los 19 y 20, respectivamente, este mismo libro, es a la vez una y diversa. Una unidad física, determinada junto al barranco. Es en esta superficie convexa, entre el Xúquer y el por el relieve y la hidrografía, y una unidad humana, conformada por Barxeta, con una pendiente de entre cinco y siete metros, donde se ha siglos de historia compartida.
    [Show full text]
  • Spanish National Committee of Geodesy and Geophysics
    SPANISH NATIONAL COMMITTEE OF GEODESY AND GEOPHYSICS NATIONAL REPORT 1999-2002 Presented to the XXIII General Assembly of the International Union of Geodesy and Geophysics Sapporo, Japan July 2003 Introduction Members of the Spanish National Committee Association Reports INTRODUCTION This report has been elaborated by the Comisión Española de Geodesia y Geofísica (CEGG), which is the International Union of Geodesy and Geophysics (IUGG) adhering organization. CEGG administer the Spanish National Committee for the IUGG, whose current membership is presented below. The main goal of this report is to summarize the research activities on Geodesy and Geophysics carried out in Spain during the years 1999-2002. This activities are presented in the form of reports elaborated by the Associations. However, other activities has been carried out by the CEGG during the last four years as, for example, the joint organization of two Spanish-Portuguese 1 Assemblies on Geodesy and Geophysics: the first one held in Lagos (Portugal) in 2000, and the second held in Valencia (Spain) in 2002. These Joint Assemblies proved very fruitful in establishing scientific cooperations for the study of the Iberian area. MEMBERS OF THE SPANISH NATIONAL COMMITTEE OF GEODESY AND GEOPHYSICS The current membership of CEGG is: President: Albero Sereno Álvarez Director General del Instituto Geográfico Nacional General Ibáñez de Ibero, 3 28003 Madrid Tf: 34-91-5979410 Fax: 34-91-5979753 e-mail: [email protected] Vice-President: Ricardo Vieira Díaz Consejo Superior de Investigaciones
    [Show full text]
  • Seasonal Circulation Over the Catalan Innershelf (Northwest
    JOURNAL OF GEOPHYSICAL RESEARCH: OCEANS, VOL. 118, 1–14, doi:10.1002/jgrc.20403, 2013 Seasonal circulation over the Catalan inner-shelf (northwest Mediterranean Sea) Manel Grifoll,1,2 Alfredo L. Aretxabaleta,3 Josep L. Pelegrı,4 Manuel Espino,1,2 John C. Warner,3 and Agustın Sanchez-Arcilla1,2 Received 5 February 2013; revised 12 September 2013; accepted 18 September 2013. [1] This study characterizes the seasonal cycle of the Catalan inner-shelf circulation using observations and complementary numerical results. The relation between seasonal circulation and forcing mechanisms is explored through the depth-averaged momentum balance, for the period between May 2010 and April 2011, when velocity observations were partially available. The monthly-mean along-shelf flow is mainly controlled by the along- shelf pressure gradient and by surface and bottom stresses. During summer, fall, and winter, the along-shelf momentum balance is dominated by the barotropic pressure gradient and local winds. During spring, both wind stress and pressure gradient act in the same direction and are compensated by bottom stress. In the cross-shelf direction the dominant forces are in geostrophic balance, consistent with dynamic altimetry data. Citation: Grifoll, M., A. L. Aretxabaleta, J. L. Pelegrı, M. Espino, J. C. Warner, and A. Sanchez-Arcilla (2013), Seasonal circulation over the Catalan inner-shelf (northwest Mediterranean Sea), J. Geophys. Res. Oceans, 118, doi:10.1002/jgrc.20403. 1. Introduction northwest Europe and the low pressure of Mediterranean cyclones over the Gulf of Lion (located north of the Catalan [2] The Catalan Sea (CS), located in the Northwest Med- Sea).
    [Show full text]
  • Hydrodynamics Over the Gulf of Valencia Continental Slope and Their Role in Sediment Transport
    Deep-Sea Research I 95 (2015) 54–66 Contents lists available at ScienceDirect Deep-Sea Research I journal homepage: www.elsevier.com/locate/dsri Hydrodynamics over the Gulf of Valencia continental slope and their role in sediment transport M. Ribó a,n, P. Puig a, H. van Haren b a Institut de Ciències del Mar, ICM-CSIC, Barcelona, Spain b Royal Netherlands Institute for Sea Research, NIOZ, Texel, The Netherlands article info abstract Article history: Circulation patterns and sediment dynamics were studied over the Gulf of Valencia (GoV) continental Received 2 June 2014 slope during spring and winter 2011–2012. Two moorings were deployed at two locations; at 450 m Received in revised form depth from February to May 2011, and at 572 m depth from October 2011 to February 2012. At both 8 October 2014 mooring sites, observations were made of currents, temperature and near-bottom turbidity within the Accepted 13 October 2014 lowermost 80 m above the seafloor. The temperature measurements allowed distinction of the different Available online 23 October 2014 water masses and their temporal evolution. The fluctuations of the boundary between the Western Keywords: Mediterranean Deep Water (WMDW) and the Levantine Intermediate Water (LIW) masses were Hydrodynamics monitored, and several intrusions of Western Mediterranean Intermediate Water (WIW) were observed, Sediment transport generally coinciding with changes in current direction. At both mooring sites, the currents generally Gulf of Valencia maintained low velocities o10 cm sÀ1, with several pulses of magnitude increases 420 cm sÀ1, and Continental slope À1 Western Mediterranean few reaching up to 35 cm s , associated with mesoscale eddies and topographic waves.
    [Show full text]
  • LA RIBERA ALTA.Indd
    ESTUDIOS COMARCALES DE LA PROVINCIA DE VALENCIA ESTUDIS COMARCALS DE LA PROVÍNCIA DE VALÈNCIA Dirección y Coordinación Técnica/ Autoría/Autoria Direcció i coordinació tècnica Josep Banyuls Juan Antonio Pascual Jorge Hermosilla Pla Departament d’Economia Aplicada Departament de Geografia Joan Carles Membrado-Tena Emilio Barba José Manuel Pastor Càtedra ESTEVAL Institut Cavanilles de Biodiversitat Departament d’Anàlisi Econòmica i Biologia Evolutiva Juan Piqueras Equipo técnico / Equip tècnic: ESTEPA Ernest Cano Departament de Geografia Departament d’Economia Aplicada Cartografía / Cartografia: Josep Vicent Pitxer José Vicente Aparicio Joaquín Farinós Departament d’Economia Aplicada Departament de Geografia Ghaleb Fansa Agustín Rovira Estadística / Estadística: Juan Ramón Gallego Departament de Comercialització Departament d’Economia Aplicada i Investigació de Mercats Miguel Antequera Jose Vicente Aparicio Irene Gil Amat Sánchez Departament de Comercialització Departament d’Economia Aplicada Ghaleb Fansa i Investigació de Mercats Sandra Mayordomo Javier Serrano Andrés Gomis Departament de Geografia Colaboración técnica / Col·laboració tècnica Col·laborador Carles Simó Carme Piqueras Emilio Iranzo Departament de Sociologia i Antropologia Social Departament de Geografia Ángel Soler Diseño y Maquetación / Disseny i Maquetació José Luis Jiménez Departament d’Estructura Econòmica Begoña Broseta Departament de Prehistòria, Arqueologia Alícia Villar i Historia Antiga Departament de Sociologia i Antropologia Social Traducción / Traducció Isidre
    [Show full text]
  • El Parc Natural De L'albufera. Un Paisaje Cultural Cargado De Historia
    bienes, paisajes e itinerarios El parc natural de l’Albufera. Un paisaje cultural cargado de historia José Segarra Ferrando | parc natural de l’Albufera, Conselleria de Infraestructuras, Territorio y Medio Ambiente, Generalitat Valenciana Bosco Dies Jambrino | parc natural de l’Albufera, Oficina de gestión técnica. Conselleria de Infraestructuras, Territorio y Medio Ambiente, Generalitat Valenciana URL de la contribución <www.iaph.es/revistaph/index.php/revistaph/article/view/3478> RESUMEN Los humedales representan ámbitos territoriales que cuentan con una serie de peculiaridades que los hacen especialmente valiosos. Además de tratarse de espacios de una elevada biodiversidad, la presencia humana en ellos ha perfilado modelos de vida, usos y sociedades especialmente singulares. El parque natural de l’Albufera, en Valencia, representa uno de esos humedales, con una larga tradición de presencia humana que le otorga un rico patrimonio cultural, resultado de esta prolongada convivencia. Un humedal que, a pesar de su elevada antropización y alteración, sigue siendo uno de los espacios naturales más importantes y representativos del estado español. El presente artículo pretende dar una rápida mirada de la evolución de este espacio en el tiempo, desde los primeros pobladores hasta el momento actual, y cómo se han ido perfilando y gestando estructuras sociales, modelos de vida, prácticas culturales, usos y costumbres, estrechamente vinculados al medio palustre que, en la mayoría de los casos, han llegado hasta nuestros días. Con la declaración de este extenso territorio como parque natural desde 1986, se ha pretendido proteger, no sólo la rica biodiversidad que acoge esta zona húmeda, sino también el variado patrimonio cultural, material e inmaterial, que ha rodeado y todavía hoy aún conserva, uno de los imaginarios más representativos de la sociedad valenciana.
    [Show full text]
  • Plan General Municipal Excm. Ajuntament De Sueca
    PLAN GENERAL MUNICIPAL EXCM. AJUNTAMENT DE SUECA DOCUMENTO DE ORDENACION -Planeamiento y Gestión- Marzo 2.001 PLAN GENERAL MUNICIPAL EXCM. AJUNTAMENT DE SUECA DOCUMENTO DE ORDENACION -Normas Urbanísticas- Marzo 2.001 PLAN GENERAL MUNICIPAL EXCM. AJUNTAMENT DE SUECA DOCUMENTO DE ORDENACION -Directrices- Marzo 2.001 PLAN GENERAL MUNICIPAL EXCM. AJUNTAMENT DE SUECA DOCUMENTO DE ORDENACION -Memoria Justificativa- Marzo 2.001 PLAN GENERAL MUNICIPAL EXCM. AJUNTAMENT DE SUECA DOCUMENTO DE ORDENACION -Catálogo- Marzo 2.001 PLAN GENERAL MUNICIPAL EXCM. AJUNTAMENT DE SUECA DOCUMENTO DE ORDENACION MEMORIAS Marzo 2.001 PLAN GENERAL MUNICIPAL EXCM. AJUNTAMENT DE SUECA DOCUMENTO DE ORDENACION PLANOS Marzo 2.001 AJUNTAMENT DE SUECA. PLA GENERAL MUNICIPAL EQUIPO REDACTOR JUAN JOSÉ HERNÁNDEZ BARQUERO ARQUITECTO-URBANISTA DIRECTOR DEL EQUIPO GUILLERMO MONFORT SALVADOR ARQUITECTO-URBANISTA COORDINADOR DEL EQUIPO ANTONI LLUCH CORELL ABOGADO A.S.T. INGENIEROS / JOSÉ Mª ARRAIZ INGENIEROS GERARDO URIOS PARDO BIÓLOGO Mª DOLORES PITARCH GARRIDO GEÓGRAFA ELISABETH CLAUDIA DELIOS ESPAÑA GEÓGRAFA ANDRÉS ARTAL TUR ECONOMISTA JUAN JOSÉ LÓPEZ HERNANDO ECONOMISTA ALEJANDRO LACUESTA ROCA ESTUDIANTE ARQUITECTURA EMILIO CONEJERO CAMPS ESTUDIANTE ARQUITECTURA EUGENIO VERDEJO BOIX DELINEACIÓN ESTHER HERNÁNDEZ GALLEGO DELINEACIÓN FERNANDO LACUESTA SOLER DELINEACIÓN RAQUEL SUAY PAYÁ DELINEACIÓN MEMORIA. 1 AJUNTAMENT DE SUECA. PLA GENERAL MUNICIPAL 2 MEMORIA. AJUNTAMENT DE SUECA. PLA GENERAL MUNICIPAL 0.- INTRODUCCIÓN MEMORIA. 3 AJUNTAMENT DE SUECA. PLA GENERAL MUNICIPAL 0.1.-EL PLANEAMIENTO MUNICIPAL El planeamiento urbano del municipio de Sueca está históricamente plagado de planes frustrados o inacabados. Primero fue el “Plano Geométrico de la Villa de Sueca” trazado en agosto de 1.860 por D. Fulgencio Vercher, después el de Buenaventura Ferrando en 1.920, el de Julián Ferrando en 1.955, en 1.966 fue Lavernia, después G.O.D.B.
    [Show full text]
  • Presentacion Seduccion V3
    Seducción Ambiental Un geoportal IDE para la participación pública en gestión de espacios naturales Javier Jiménez Romo Ayuntamiento de Valencia Salvador Bayarri Romar IVER T.I. S.A. Contenido • El parque natural de l’Albufera de Valencia • El proyecto Seducción Ambiental • Ejemplos de portales • Arquitectura del sistema • El papel de gvSIG • El portal web Parque Natural de l’Albufera de Valencia • A 10 kilómetros de Valencia. • 21.000 hectáreas. • Espacio protegido a nivel: – Nacional: Parque Natural – Comunitario: Red Natura 2000 – Internacional: Humedal RAMSAR • 4 ecosistemas Parque Natural de l’Albufera de Valencia EL LAGO Parque Natural de l’Albufera de Valencia LOS ARROZALES Parque Natural de l’Albufera de Valencia LOS ARROZALES Parque Natural de l’Albufera de Valencia LA DEVESA Parque Natural de l’Albufera de Valencia LAS PLAYAS Parque Natural de l’Albufera de Valencia 13 municipios Albal Albalat de la Ribera Alfafar Algemesí Beniparrell Catarroja Cullera Massanassa Sedaví Silla Sollana Sueca Valencia Parque Natural de l’Albufera de Valencia 13 municipios Albal Albalat de la Ribera Alfafar Algemesí Beniparrell Catarroja Cullera Massanassa Sedaví Silla Sollana Sueca Valencia Parque Natural de l’Albufera de Valencia 13 municipios Albal Albalat de la Ribera Alfafar Algemesí Beniparrell Catarroja Cullera Massanassa Sedaví Silla Sollana Sueca Valencia Parque Natural de l’Albufera de Valencia Problemas a resolver – Cercanía a Valencia… pero desconocimiento por parte de la ciudadanía. – Valiosos ecosistemas… que requieren de restricciones de usos. – Diversos municipios… que implican muchas administraciones competentes y desorientación. El proyecto Seducción Ambiental Proyecto financiado por el programa UE LIFE+ (2007-2013) Aproximación a las soluciones: – Cercanía a Valencia… Más allá de la concienciación medioambiental, seducir con los valores de l’Albufera.
    [Show full text]
  • Al DOC. III OBJETIVOS Y ESTRATEGIAS ANEXO
    ANEXO al DOC. III OBJETIVOS Y ESTRATEGIAS ANEXO $E CONFORMIDAD CON LO ESTABLECIDO EN LOS ARTÓCULOS Listado de fichas del anexo. DELA,EY DEDEJUNIO DE/RDENACIØN DEL 4ERRITORIO Y 0ROTECCIØN DEL 0AISAJE LOS PLANES DE ACCIØN TERRITORIAL DE NATURALEZA SECTORIAL PUEDEN s ALBAL s '/$%,,! s 15!24$%0/",%4 MODIFICAR DIRECTAMENTE OTROS PLANES DE ACCIØN s ALAQUÀS s -!.)3%3 s 2!&%,"5.9/, TERRITORIAL O PLANES URBANÓSTICOS APROBADOS %N ESTOSSUPUESTOSDEBENCONTENERUNANEXOENELSE s !,"!,!4$%,33/2%,,3 s -!33!,&!33!2 s 2/#!&/24 ESPECIFIQUEN LAS MEJORAS EN LA ORDENACIØN QUE SE s !,"/2!9! s -!33!-!'2%,, s 3%$!6) PROPONENYLASRAZONESQUELASJUSTIFIQUEN s !,"5)8%#( s -!33!.!33! s SILLA 4ALYCOMOSEESTABLECEENELPRESENTEDOCUMENTODE s !,#°33%2 s -%,)!.! s 4!6%2.%3",!.15%3 OBJETIVOSYESTRATEGIAS EL0LANDE!CCIØN4ERRITORIALDE s !,$!)! s MISLATA s 4/22%.4 LA(UERTA QUEAFECTAACUARENTAYCUATROMUNICIPIOS s !,&!&!2 s -/.#!$! s 6!,%.#)!,A!LBUFERA TIENEPOROBJETOLAORDENACIØNYREGULACIØNDEPARTE DELSUELONOURBANIZABLEINCLUIDOENELÉMBITOESTRICTO s !,&!2!$%,0!42)!2#! s -53%2/3 s 6!,%.#)!(UERTADE#AMPANARY!RCODE-ONCADA s !,-°33%2! s ,!0/",!&!2.!,3 s 6!,%.#)!(UERTADE6ERAYDE2OVELLA %L PRESENTE ANEXO TIENE POR FINALIDAD RECOGER LAS s "/.2%0¿3)-)2!-"%,, s ,,/#./5$%,!#/2/.! s 6!,%.#)!#ASESDE"ÌRCENA -AHUELLAY2AFALELLY6ISTABELLA MODIFICACIONES DE PLANEAMIENTO INTRODUCIDAS EN EL PLANEAMIENTODELOSMUNICIPIOSAFECTADOS!SÓPUES s "%.%4Â33%2 s 0!)0/24! s 6).!,%3! RECOGEDEFORMAINDIVIDUALIZADAPARACADAMUNICIPIO s "%.)0!22%,, s 0!4%2.! s 8)2)6%,,! LACLASIFICACIØNYZONIFICACIØNQUEESTABLECEPARAEL s "52*!33/4 s 0)#!.9! SUELO NO URBANIZABLE PROTEGIDO NATURAL %6. O DE HUERTA ( $ENTRO DE LAS ÉREAS DE PROTECCIØN DE s #!4!22/*! s 0)#!33%.4 HUERTASEPREVÏUNAZONIFICACIØN ENFUNCIØNDELOS s %-0%2!$/2 s 05£/, OBJETIVOSDECALIDADPRETENDIDOSESTABLECIENDOTRES s &/)/3 s 05)' NIVELES (UERTA DE PROTECCIØN ESPECIAL ( (UERTA DE PROTECCIØN ESPECIAL ( Y (UERTA DE PROTECCIØN AGRÓCOLA(%LRÏGIMENDEUSOSYACTIVIDADESPARA Contenido de cada ficha del anexo.
    [Show full text]
  • F:\DATOS\AA Paloma\Mapa Albufera\Mapa Turístico ALBUFERA
    Parc Natural de l'Albufera Surface: 21.120 ha. Year of Declaration / Année de déclaration: 1986 www.parquesnaturales.gva.es/albufera València Centre d'interprétation Interpretation centre Musée Museum V-30 Riu Túria Picanya Lieu d'intérêt Interesting place Sedaví Paiporta Benetússer Platja de Pinedo Aire de repos Alfafar Pinedo Resting area CV-500 Massanassa V-31 Port CV-401 Catarroja Barranc de Xiva Platja del Saler Hermitage Albal Port de Parking Catarroja Port El Saler del Saler Beniparrell Platja de la Garrofera Source d'eau Ruta3 Natural spring Alcàsser Point d'observation des oiseaux Bird watching point Silla Port de Platja de la Brava Silla Tancat La Devesa Itineraries de la Pipa Itinéraires La Mata del Rei Punta Llebeig Gola del Pujol i Mirador Platja de la Malladeta Estany del Pujol Punta de Sant Pere Mata de l' A L B U F E R A Sant Roc C.I. Racó de l’Olla La Mata del Fang Platja de la Devesa La Mata de la Manseguerota La Mata de L’Antina Parador El Saler A-7 AP-7 Gola del Perellonet Ruta 4 El Palmar Torre Mirador Port El Perellonet i Tancat de Mília del Palmar Platja del Recatí MAR Ruta 2 Soll Almussafes MEDITERRANI Benifaió PARC NATURAL Gola del Perelló Sollana El Perelló L’ALBUFERA Port Platja del Perelló Tancat de del Perelló L’Illa Platja de les Palmeres Les Palmeres Ullal de A-38 Baldoví Mareny de Platja del Rei Gola del Rei Barraquetes Platja deBega de Mar Muntanyeta dels Sants CV-502 AP-7 Llacuna del CV-500 Samaruc Mareny de Platja del Mareny de Sant Llorenç Vilxes Mareny de Sant Llorenç Albalat de Bassa de Platja del Dosser la Ribera Sueca Sant Llorenç Riu Xúquer Polinyá de Xúquer Riola Gola de Sant Museo del Arroz Llorenç Algemesí A-38 (961 731 586) Benicull Fortaleny N-332 Cullera Places of interest of the Natural Park of l'Albufera: Lieux d’intérêts du Parc Naturel Port d'El Saler: Petit port situé à moins de 5 kms de Valencia, durant une longue période il était le seul lien Port of El Saler: Small port placed ve kilometres from València.
    [Show full text]
  • El Tancat De La Pipa Recupera Els Ecosistemes
    Núm. 31, primer semestre 2011 www.fhortasud.org El Tancat de la Pipa recupera els ecosistemes de l’Albufera Resultats de les eleccions municipals a l’Horta Sud Entrevista a l’escriptora Carme Miquel Fumerals, testimonis de la Revolució Industrial a l’Horta Sud Arquitectura al Torrent del canvi del segle XIX al XX Les torres islàmiques de l’Horta Sud La cançó en valencià, gèneres tradicionals i moderns sumari la fundació paisatges de l’horta sud Enfortint les associacions, El Tancat de la Pipa recupera incrementant la participació, els hàbitats naturals del Parc Natural millorant la democràcia 4 de l’Albufera 18 Julio Huerta FranceSc Martínez Activitats del Museu Comarcal “Josep Ferrís March” 6 patrimoni de l’horta sud adrià beSó Fumerals, testimonis de la revolució Industrial a l’Horta Sud 23 sociocomunitari adrià beSó L’Horta Sud té el seu propi himne 8 L’arquitectura a la ciutat de Torrent FátiMa KoudSi en el canvi del segle XIX al XX (1893-1935) 26 Programes de creació d’ocupació toMáS roSSelló JaunzaráS de la Mancomunitat de l’Horta Sud 9 FátiMa KoudSi arqueologia de l’horta sud La cançó en valencià, repertoris tradicionals i moderns 11 El paisatge històric de l’Horta Sud FranceSc Martínez a l’època islàmica. Visibilitat i sistema defensiu de les torres islàmiques 32 actualitat comarcal adrià pitarcH Les eleccions de maig de 2011 consoliden l’hegemonia del PP passat i present a l’Horta Sud 13 Antic Ajuntament d’Albal 36 toMàS SancHiS gent d’ací Entrevista a Carme Miquel i Diego 16 quaderns de l’horta, núm 7 FátiMa KoudSi suplement de la revista papers de l’horta Núm.
    [Show full text]