996 resultados para Pedralta (Girona, Catalonia)
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Sobre les relacions i intercanvis artístics entre Girona i el Rosselló a la segona meitat del segle XV
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Article que estudia els cementiris antics i altomedievals de la ciutat de Girona ubicats a l'entorn immediat de la ciutat, a la riba esquerra del riu Onyar i intra muros
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Article sobre l'edifici de 'La Pabordia' de Girona, un casal medieval amb torre. Es fa una reflexió i un estudi sobre l'estructura de l'edifici, les tècniques constructives emprades en cada fase i la relació existent entre els seus diversos àmbits i cossos, tenint en compte la documentació planimètrica, la informació gràfica a través de fotografies, i la consulta puntual de documentació medieval
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Descripció del jaciment arqueològic del 'Roc de la Melca', en la vall de Sant Aniol de Finestres (Girona). Es descriuen la indústria lítica i els problemes que presenta la cronologia del 'Roc de la Melca'
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Article que descriu com era el Palau Episcopal de Girona a mitjans del segle XV a través de dos documents antics sobre reparacions realitzades al palau, un del 1437 i un altre del 1460
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L’any 2011 s’ha graduat la primera promoció dels estudis d’Arquitectura de la UdG. Tot i la crisi que afecta la construcció, cada curs un bon nombre d’estudiants tria aquesta especialitat. Els responsables del grau, però, consideren que és un bon moment per donar un nou enfocament a la matèria
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This article is an essay aiming at the definition of the urban district of Girona, having as a base the analysis of the intensities and directional tendencies of labour mobility fluxes in it. Several cathegories will be signaled inside this area which wil enable us to differenciate a number of crowns of municipalities according to their respective links with Girona town. A reflection set forth by Francesco Indovina on the concept of diffused town will be the first step in the attempt to typify this area. Thus, the existence of a diffused city core of which would be Girona town will be argued, an issue this one which is to be analysed in future studies
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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)