Girona entre l'Islam i Carlemany: una ciutat de frontera (759-801)

Tradicionalment s'ha considerat l'ocupació de Girona pels francs (any 785) com el moment "fundacional" de la ciutat medieval, en paral·lel a la consideració que ha merescut l'època de Carlemany (final del segle VIII i principi del IX) com una època formativa en la història de Catalunya. Però tenim raons per pensar que aquells moments no significaren un gran terrabastall enuna ciutat que, des de començament del segle VIII, jugava un paper polític i militar significatiu en els esdeveniments de l'anomenada Marca Superior, el territori musulmà proper a les terres del regne franc. Més endavant, un cop incorporada a l'imperi carolingi, Girona mantingué la seva condició de ciutat capital de frontera o marca, fins a la conquesta de Barcelona l'any 801. Volem historiar, en la mesura del possible, aquesta etapa d'uns quaranta anys -entre 759 i 801- quan la ciutat visqué en primera línia i, també, protagonitzà les vicissituds de l'enfrontament entre dos dels grans estats d'aquell moment: la monarquia franca dels carolingis i l'emirat omeia A'al-Andalús. Els moviments d'anada i tomada dels seus exèrcits van situar Girona en primera línia de combat en aquells anys, fins a la definitiva consolidació del poder franc a principis del segle IX

El Camí de Sant Jaume en la provincia de Girona

En primer lugar se identifican las distintas rutas del Camí de Sant Jaume en la provincia de Girona con el objetivo de determinar cuáles han sido las principales rutas que los peregrinos han utilizado para su peregrinación hacia Santiago de Compostela dentro de la provincia de Girona. En segundo lugar se establecen los elementos que determinan que un itinerario concreto esté comprendido en el Camino de Santiago para lo cual se analizan las rutas y se buscan los componentes que tienen una relación directa con la peregrinación a Santiago de Compostela, bien por ser elementos descriptivos del Santo, bien por ser elementos que a lo largo de la historia se han atribuido a los peregrinos que peregrina a Santiago de Compostela. En tercer lugar se analiza el recorrido del Camí de Sant Jaume elegido por la Generalitat de Catalunya, se examinan los servicios que ofrece y las carencias o insuficiencias que posee. Finalmente se establece la confección de propuestas de mejora y las acciones pertinentes para corregir las debilidades que en su caso puedan tener estos itinerarios

Les Espècies vegetals introduïdes d’ús ornamental als enjardinaments públics dels sectors de l’esquerra del Ter a la ciutat de Girona

Estudi de les plantes ornamentals conreades al sector esquerra de les ribes del Ter al seu pas per Girona, incidint en les espècies no autòctones i elaboració d’una cartografia digital dels arbres i arbusts de la zona de Sant Ponç (Girona)

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

Característiques geomorfològiques de la Pedralta (Baix Empordà, Girona)

Descripció de les característiques geomorfològiques de La Pedralta, entre els municipis de Santa Cristina d'Aro i de Sant Feliu de Guíxols

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)

Las formas graníticas de los macizos de les Gavarres i de Begur (Girona)

In the present paper the granite landforms of the Les Gavarres and Begur massifs (Girona) are described. Also the relationship between this landforms and the lithology are analysed

The geophysical electromagnetic prospecting in the spatial location of the travertine deposits of the Banyoles Depression (Girona)

The results of the application of the geophysical electromagnetic prospection methods in the resolution of the problems of the spatial location of the travertine quaternary formations of the Banyoles depression are presented

La Pedralta, un ejemplo de patrimonio geológico de Girona

Pedralta is a very large rocking stone shaped in monzonitic granite. Its volume and weight are approximately 34 m3 and 90 Tm. The fall of such block has supposed the loss of a worthy geotipe

Aportaciones al conocimiento del Cretácico del macizo del Montgrí (Girona)

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 characterof the different levels and their faunal content, specially megafossils

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