Èmfasi contrareformista en els retaules de la seu de Girona

La catedral de Girona conserva un bon mostrari de retaules barrocs, ubicats en les capelles laterals de l'àmplia nau gòtica, fet que permet conèixer i detectar l'ambient artístic desenvolupat a la ciutat en el primer terç del segle XVIII. Entrant per la porta dels peus de la gran nau trobem, a banda i banda, els retaules de l'Anunciació i de la Immaculada Concepció; a la banda dreta, tot seguint la direcció vers l'altar, observem els retaules de sant Miquel i el dels sants Iu i Honorat; enfront, més a prop de la girola, s'hi troba el retaule de sant Narcís; i ja plenament en el deambulatori, el dels Dolors

Els Naturals i el rei natural en la Catalunya de la Guerra dels Segadors: a propòsit d´un sermó de Gaspar Sala (1641)

La guerra dels Segadors (1640-1652/59) va ser també una guerra d'idees o arguments polítics. A diferència, però, d'altres conflictes anteriors (com ara l'anomenada guerra civil catalana de mitjan segle xv), aquests arguments antagònics conegueren (al Principat i fins i tot mes enllà) una difusió sense precedents; sobretot pel fet que s'expressaren tot sovint per la via impresa

Sobre la identitat dels Matiners a les comarques del N.E. de Catalunya

This study attempts to throw some light on the identity of the Matiners of the regions of north-eastern Catalonia by analizing a notebook which was a register of rebels. This notebook gives the age, geographical origin and profession of the rebels. The War of the matiners (1846-49) was a Catalan rebellion framed within the context of popular opposition to the regime of the moderates, and in the midst of a general crisis. Themen who formed the groups of ((trabucaires)) were particulary young (the problemof recriting must not be forgotten), and came from the country, the crafts, and industry, and were militarized above all in the interior regions

Solicitud de verificación de la titulación. Grado en Ingeniería de Sistemas Electrónicos por la Universitat Politècnica de Catalunya ‐ ETSETB

Solicitud de verificación de la titulaciónGrado en Ingeniería de Sistemas Electrónicos por la Universitat Politècnica de Catalunya ‐ ETSETB según el protocolo VERIFICA de la Agencia Nacional de Evaluación de la Calidad y Acreditación.

Solicitud de verificación de la titulación. Grado en Ingeniería Telemática por la Universitat Politècnica de Catalunya ‐ ETSETB

Solicitud de verificación de la titulaciónGrado en Ingeniería Telemática por la Universitat Politècnica de Catalunya ‐ ETSETBsegún el protocolo VERIFICA de la Agencia Nacional de Evaluación de la Calidad y Acreditación.

Solicitud de verificación de la titulación. Grado en Ingeniería de Sistemas de Telecomunicación por la Universitat Politècnica de Catalunya ‐ ETSETB

Solicitud de verificación de la titulaciónGrado en Ingeniería de Sistemas de Telecomunicación por la Universitat Politècnica de Catalunya ‐ ETSETBsegún el protocolo VERIFICA de la Agencia Nacional de Evaluación de la Calidad y Acreditación.

Aportació al coneixement de la dinàmica fluvial en la conca del riu Onyar (Girona)

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

Anàlisi geomètrica del Diaclasat de les Guilleries en el sector de la Vall del Ter entre els embassaments del Pasteral i Susqueda (Girona)

The Guilleries are a small and mountainous area located in the north-westem part of the Catalonian Coastal Ranges where metamorphic and igneous Paleozoic rocks are exposed. After the main hercynian folding this area was affected by a brittle deformation that is mainly manifested by the intrusion of a very large number of dykes of granodiorite and the development of a complex joint system. Trends of dykes indicate that their intrusion was related to a SE-NW extension, whose estimated value is 40% on an average. This extension seems to stand, although without any associated igneous event, with the development of NE-SW directed joints which make the main set. Five families more were developed later, onegently-dipping and fou upright; the latter trending roughly SE-NW, ENE-WSW, ESE-WNW and N-S. AU the joint sets appear in the metasedimentary Paleozoic rocks and in the hercynian intrusive bodies. Concerning the ages, joints that belong to the NE-SW and SE-NW directed sets and also those slightly dipping have been attributed to the late-hercynian times and all the other are considered to be later

Aportaciones al conocimiento de la geología de Bac Grillera (prepirineo, Girona)

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)

Avaluació dels recursos d'àrids disponibles en medis fluvials mitjançant tècniques geofisiques. Aplicació a la cubeta de Celrà (Riu Ter, Ne Catalunya)

The depth of the water table and the clay content are determinant factors for the exploitability of natural aggregates, such as the alluvial sands and gravels found on the fluvial domain of the Ter River. In this preliminary study, carried out in the Celri basin, we conclude that these variables can be determined by means of geophysical methods and recornmends the use of such methods in studies of regional character

Morfolitología de las terrazas del Ter en Girona

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

Presencia del paleogeno bajo los sedimentos neogénicos de Vilablareix (Girona)

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

Las fuentes naturales del término municipal de Sant Feliu de Guíxols (Girona)

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

Participació de les aigües subterrànies en la gènesi d'ambients palustres continentals: el cas dels prats de Sant Sebastià (Caldes de Malavella, Girona)

The area known as 'prats de Sant Sebastià' is in Caldes de Malavella. It is part of the wetlands located in the south-eastern end of the Selva Basin. Several areas with unusually high conductivity (EC up to 24,500 uS/cm) have been identified in this place. This fact allows highly specialised and comparatively rare botanical species to grow in this area. These saline soils follow a north-south line-up. The geophysical data, obtained with a field conductivemeter (EM 31), show that this superficial line-up continues in the subsoil. In addition to this, the conductivity cartography, made for an electromagnetic exploration depth of 6 meters, shows that the width of the region where these salinity anomalies take place increases in depth. When included in the hidrogeological context of this sector of the Selva Basin, these data bring new elements for the study of the genesis and working of these marshy environments.The model that future research will have to confirm, maintains that the groundwater discharges coming from the underlying hydrogeothermal aquifer are a conditioning factor of the aforementioned phenomenon. This ascending flow of highly mineralised waters (TDS of about 3,500 mg/l) can produce and keep stable the soil salinity

El paleozoic del massís de Begur (Girona)

The Paleozoic materials of Massís de Begur are described from a stratigraphical point of view. We distinguish two units: the lower one, present phillites with carbonate layers ofcambro-ordovician age. The upper one is composed by volcanic rocks, carbonate schistsand black slates, bring from caradocian and ashgillian age