944 resultados para Vilallonga, Mariàngela -- Viatges -- Girona


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Ressenya del llibre de Josep Clara 'El Partit únic : la Falange i el Movimiento a Girona, 1935-1977', publicat pel Cercle d'Estudis Històrics i Socials l'any 1999. En aquest llibre es tracta un dels aspectes centrals del regim (antiparlamentari) franquista: l'existència d'un partit únic oficial (la Falange), configurat com a Movimiento Nacional, i la seva concreció en la demarcació provincial de Girona

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El projecte tracta de la realització de proves de càrrega al Claustre de la Catedral de Girona per tal de conèixer la càrrega que suporten les columnes de pedra del claustre. Un cop coneguda aquesta càrrega, es podrà decidir si son aptes o no per al canvi d’ús previst a la planta superior i es podrà aportar una resposta definitiva a una de les dues hipòtesis plantejades: si es forma o no arc de descàrrega a les columnes del Claustre. D’altre banda, es realitzarà una proposta de tractament de les columnes del Claustre que consistirà a escollir les que hauran de ser reparades i les que hauran de ser substituïdes, en base a una sèrie de càlculs numèrics

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Las Jornadas de SIG Libre de Girona empezaron su andadura en el año 2007, organizadas por el SIGTE (Servicio de Sistemas de Información Geográfica y Teledetección) de la Universitat de Girona, y con un comité científico de 11 personas. Los patrocinadores eran dos, y los colaboradores cinco, con tan sólo una empresa del área de la geomática entre ellos. En 2011, a pesar de la crisis, el número de patrocinadores y colaboradores ascendió a 14. El número de comunicaciones o charlas pasó de 42 en 2007 a 47 en 2011. A pesar de que los números de las Jornadas no reflejan un crecimiento cuantitativo exponencial, cualitativamente las Jornadas de Girona se han convertido en un referente hispano en el sector no sólo del SIG Libre, sino de la Tecnologías de Información Geográfica en general. Podemos considerar a este evento un punto consolidado para el encuentro de empresas, administraciones, investigadores, profesionales y ciudadanos en general que dedican parte de su tiempo a trabajar y disfrutar con la cartografía, la ciencia y la tecnología geográfica. En consecuencia puede ser un buen espejo donde observar la evolución del sector SIG en España. Partiendo de esta hipótesis, esta comunicación presenta un análisis SIG acerca de la procedencia y el contenido de Jornadas de SIG Libre de Girona desde el año 2007 al 2011, presentando información interesante para comprender mejor el progreso de este estratégico sector en España en particular, y en el ámbito de habla castellana en general, e invitando a la reflexión sobre si un evento como estas jornadas puede servir para monitorizar el estado del SIG en un determinado territorio

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The Onyar River basin is situated in the depression of la Selva. His origins are related to tectonic activity during Neogen in this region. In his evolution, we note a slowly and continuous downfall which directs the morphodinamical behaviour. In this sense, the drainage network has a directional trend towards the north, as consecuence of fault systems, and specially the N-S oriented one. A fault of this system has an important influence in the basin morphology, directs the drainage towards the north and avoids a closely drainage in the basin

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This paper makes a contribution to the knowledge of the coastal fringe morphology of the ‘Macizo de Begur’. A lithological study, macro and microscopic, has been carried out of a variety of a series of metamorphic, plutonic, phyllonianic and effusive rocks

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Two unknown volcanic outcrops in the Alt Emporda (Girona) are described in this paper . We present their exact situation and a description of their occurrence and their mineralogical and petrological characteristics. Bothhave been classified as alkali-olivine basalts and they probably extruded during the Neogen period

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Two decay rates are distinguished in the discharge hydrograph of the Onyar River, using Maillet's formula. In this way, we can know which Kina of influence is made by geomorphology and rainfall distribution on fluvial processes

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It is a contribution to the study of the terraces of the river Ter along its mid-course in the town of Girona, since that is the last speace where it is still possible to observe four of these terraces with clear characteristics of climatical deposition. Itsmorphological peculiarities are described as well as the morphometrical and lithological parameters of its pebbles. These terraces are compared with others which have been studied in other areas of the regions and conclusions are drawn concerning deposition, source àrea and chronology

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This study makes clear the existence of a paleogenical red basal level (Pontils Fm.) in the Vilablareix àrea, under the mio-pliocenical cover of the Girona plain, enlargening the surface known go far of that level

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The behaviour of 21 natural springs in a granític massif is studied in this survey. Geomorphological features of the zone are described as well as water circulation and rising 25 parametres of each of them are analysed ans conclusions are withdrawn regarding geological conditions of rising, course, chemism and potability

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The Bac Grillera nappe (Prepirenean of Girona) shows a stratigraphic section composed of two unconformi ty-bounded units. The lower unit is composed by rethian (marly limestones) and liassic (brechoid marly limestones and limestones). The upper unit (sandstones and marly limestones) belongs to the upper Cretaceous (Campanian)

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With the aim of radiocarbon dating Llora travertines, chemical and isotopic data of strearn water and present travertines have been analyzed. The purpose is to determine the radiocarbon activity of present travertines in order to assign an initial radiocarbon activity to the old ones. Applying this methodology we conclude that travertines are from Holocen age around 4.000 years BP

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The University of Girona held the XXVI Young Geographers meeting in september 2003. The event, entitled «Talking geograpies», involved Spanish students and qualified geographers with the aim of discussing the varied perspectives of geography in the field of town and country planning

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ln this paper we describe a stratigraphic column of the Cretaceous of the Montgrí. This description is based on several partial stratigraphic cross sections as well as on the lithological character of the different levels and their faunal content, specially megafossils

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From several small stratigraphic sections, we have reconstituted the Liassic interval of the Girona Province (NE Spain). We have been able to identify paleontologically the Carixian (Jamesoni, Ibex, and perhaps, Davoei zones), the Lower Domerian (Stockesi zone), and the Middle Toarcian (possibily Variabilis zone, as well as Thouarsense and Insigne zones). The Lower Toarcian (Serpentinus zone) is represented by fossil remains no ‘in situ’. The lowest Toarcián (Tenuicos-tatum zone) as well as the Middle and Upper Domerian (Margaritatus and Spinatum zones respectively, are probably represented by stratigraphic gaps