555 resultados para Viticulture -- Catalonia


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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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Ressenya del llibre 'La Vall de Llémena' d' Albert Pujadas i Pigem, editat per la Diputació de Girona dins la col·lecció 'Els Espais Naturals de les Comarques Gironines' i publicat l'any 1995 i en el que s'ofereix un material didàctic-educatiu als professors d'ensenyament secundari

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Ressenya del llibre 'Itinerari geològic de Banyoles : descoberta del funcionament del sistema lacustre' de David Brusi, Joan Bach i Miquel Sanz, editat per l' Ajuntament de Banyoles i Eumo Editorial l'any 1990

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Descripció del volcà anomenat 'Palou' a 1Km. al Sud d' Amer

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Descripció del sistema càrstic de Sant Martí de Llémena

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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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Due to the edition of the new Atles comarcal de Catalunya by the Institut Cartogràfic de Catalunya in digital format, we look at the structure of their contents and the dynamics of its use. Likewise, it is detailed which methodology was utilized to perform it. Finally, some reflections on the innovations that this new product entails in textual and cartographic areas are proposed, especially related to the current socioeconomic context and new employed technologies

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La present comunicació pretén ressenyar l’aportació dels Atles comarcals de Catalunya al coneixement del nostre territori com una obra no només de caire acadèmic sinó també divulgatiu i aplicat. En primer lloc, es constata la filiació de l’obra al llegat de la geografia clàssica catalana i a les aportacions tradicionals —monografies i les obres generals― que han disseccionat el país des de l’òptica comarcal. En segon lloc, es detalla el seu procés de concepció i elaboració. Finalment, es destaquen les innovacions que el nou format CD-Rom i les possibilitats d’interacció cartogràfica amb servidors externs suposen en el sentit d’innovació respecte de les aportacions anteriors

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Here we describe a series of recognized morainic deposits in the "Macizo del Port del Comte", which are the southern-most example of the eastern pre Pyrenees

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Catalan volcanic field, in Iberian Peninsula Northeast, has been made during Neogene and Quaternary. It is made up Empordà, la Selva and la Garrotxa Zones, the best volcanic morphology is in the last one because is the most recent. In this paper we explain the volcanic rocks general characteristics, what eruption activity generate it and the final volcanic edifice morphology. Finally, we propose some crops to visit

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In this paper we make a litostratigraphical study on the Miocene of the 'Vallés occidental' (Barcelona, Spain) which embraces a part of the 'Depresion Media' of the intermediary tectonic grave between the 'Cadena Litoral' and 'Prelitoral' of the 'Sistema Mediterráneo'. At the same time we undertake an analysis of the bassin

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A series of circumstances which converge in a little valley in the province of Girona, result in a peculiar type of morphogenetic evolution and a quite singular mechanical instability of its buttons. Very recent tectonic movements as well as dissolution phenomena of its subsoil due to pressurized underground water have played an important role in the morphogenesis. Such conditions have resulted in a fast morphological evolution which a progressive lowering of the valley floor as well as peculiar morphological features which favour the existence of numerous pits caused by sudden collapses distributed in altitude and time

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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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There is in this work a description of sedimentological characters of the medium Eocene sandstone level from Sarriá de Ter (Gerona province Spain) and an interpretation of their genesis and situation in the regional paleogeography. The conclusion is that these sandstones form a deltaic channel(delta front). To wards the E and NE the become fluvial deposits, to wards the W, Plana de Vic, they become clay and silstones considered as a prodelta

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Starting from the discovery of a cheek-booth Dinotherium giganteum KAUP in the river Oñar in Gerona we can consider that the Miocene formations of La Selva expand up to this area