938 resultados para Marine fauna -- Catalonia -- Costa Brava


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Several marine deposits in the southern Costa Brava shoreline have been studied. They appear at different heights above and below the present sea level. Three groups are defined in relation to their origin: conglomerate levels at the bottom of the cliffs, not-cemented emerged beaches and cemented submerged beaches. The age of the emerged beaches has been accurately determined by means of the ceramic content and radiocarbon dating. Chronological succession of the deposits and their stratigraphic and paleontological characteristics allow to define a sequence of the sea level changes during the latest stages of the versiliane transgression in the studied area

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Article que descriu els organismes animals del litoral gironí

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Este artículo tiene por finalidad analizar las medidas de adaptación al riesgo de inundación que se han realizado en el ámbito de la Costa Brava, con especial incidencia en el papel que han tenido las obras de infraestructura hidráulica en la prevención de avenidas. Se intenta comprobar hasta que punto la percepción local dominante sobre las obras hidráulicas como una de las formas más eficientes pera la prevención de inundaciones se contradice con las nuevas tendencias tanto en relación a los costes ecológicos de la construcción de estos dispositivos hidráulicos como al planeamiento urbanístico y fluvial, en general

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Repàs de com ha estat representada la Costa Brava, com a escenari d’exteriors, al món del cinema amb diverses localitzacions tant des d’una perspectiva metodològica documental com des d’una perspectiva metodològica simbòlica

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Visió de la realitat econòmica de la Costa Brava 20 anys després del Debat Costa Brava de 1976, sobretot centrat en l’activitat turística

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Ressenya del llibre El paisatge humà de la Costa Brava. L’obra es presenta en dos volums. El primer l’ocupen dos blocs: “El medi i els homes” i “L’elaboració del paisatge humà i dels gèneres de vida”; el segon és un bloc referit a l’impacte territorial i socio-econòmic del turisme. Es tracta d’una obra que resulta útil per saber per què la Costa Brava és avui com és

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La vida al medi marí de la Costa Brava

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The first section of this paper summarises the most relevant charateristics of the contemporary tourist model, also called postfordist or postmodernist. In the second part the traditional tourist model developed in the Costa Brava in the past decades, is reviewed. Emphasising the saturation of tourist facilities on the coast line, expansive urban growth, thanks to a tolerant administration, poor complementary supply and concentrated demand in few markets and the proximity of Barcelona conurbation, stressed by second homes. In the third section, some strategies developed in recent years to readapt the Costa Brava to the new tendencies in tourism, are presented. Incorporation of the inland to the tourist product, new planning policics, lessening urban densities and height, and a change in mind in favour of protected natural areas, diversification of demand with new markets, specially form Eastern Europe (although this might be considered as a continuation of the traditional tourist model) and the emergence of local strategies oriented towards the creation of new tourist products based upon natural and cultural resources

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Ressenya de l' obra d'en Josep Duran i Carpintero, 'Itineraris geológics per la Costa Brava' i editada pel Consorci de la Costa Brava l'any 1989. El llibre inclou 8 itineraris per la Costa Brava, cadascun d' ells amb una fitxa tècnica amb informació pel docent o visitant, una descripció geològica i activitats i qüestions per a l'alumne

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The geometry of Riera de Tossa (Costa Brava, Catalonia) Pleistocene paleovalley has been studied by two geophysical prospecting methods: vertical electric sounding (VES-DC) and seismic refraction. The results show the existence of a sudden slope change of the thalweg that permits to differentiate two sections where erosion processes operated in unequal intensity. Based on geological and geomorphological available data, it can be inferred that this slope rupture is caused by the litological control imposed by the alineation of resistant materials, which limited the headward erosion extend of the creek during the Upper Pleistocene

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