992 resultados para Vives, Joan Lluís, 1492-1540-Retratos-Grabado


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Com tants altres personatges de la nostra història, el pare de FrancescFontanella i Garraver –el jurisconsult olotí Joan Pere Fontanella–ha estat objecte durant dècades d’un encadenament de notíciesbiogràfiques on s’han reiterat dades no sempre filtrades científicament.Això ha abocat diverses generacions a acumular imprecisions sobre ell,fins i tot a distorsionar-ne la significació ideològica i política, sovinten clau d’un patriotisme ardorós. Volem contribuir, sense cap ànimd’esmena, a esclarir i difondre algunes informacions sobre les sevesvida i obra i el seu pensament jurídic i polític. I considerem adientfer-ho en un marc que ratione loci convida a ventilar els forts lligamsque l’advocat mantingué amb la ciutat de Girona i ratione materiaeobliga a subratllar el seu vessant protector dels parents i pròxims i,més a l’engròs, la seva vocació per analitzar amb el dret a la mà elcomplexíssim món de les relacions familiars.

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Comunicació presentada a les Jornades d'Estudi Sobre el Municipi Abans de la Nova Planta (1716), celebrades a La Fatarella (Tarragona) el 19 i 20 d'abril de 2008.

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Article que descriu la planta poligonàcea, Polyganum Romanum, present a la zona de l' Empordà

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When did overseas trade start to matter for living standards? Traditional real-wage indices suggest that living standards in Europe stagnated before 1800. In this paper, we argue thatwelfare rose substantially, but surreptitiously, because of an influx of new goods as a result ofoverseas trade. Colonial luxuries such as tea, coffee, and sugar transformed European diets afterthe discovery of America and the rounding of the Cape of Good Hope. These goods became household items in many countries by the end of the 18th century. We use three different methodsto calculate welfare gains based on price data and the rate of adoption of these new colonialgoods. Our results suggest that by 1800, the average Englishman would have been willing to forego 10% or more of his income in order to maintain access to sugar and tea alone. These findings are robust to a wide range of alternative assumptions, data series, and valuation methods.

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En aquest article es presenta el relat de les històries personals de deu joves geògrafs i geògrafes centrades en la seva formació acadèmica i en les respectives experiències i trajectòries en el món laboral. No pretén ser una mostra representativa de l’actual panorama professional al nostre país, sinó, tan sols, fer arribar al lector deu trajectòries individuals que tenen com a fil conductor l’intent d’assolir l’exercici professional i estable de la geografia

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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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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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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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In this paper we show some sedimentological characteristics of Assilina beds from Armancies Fm. (middle Eocene) and their lateral equivalents that let us to remark some aspects of their genesis. We arrive to the conclusion that, in occidental sector (Bagá-Campdevanol), ‘las barras de Assilinas’ from the Armancies Fm. are grain flow channels, first sedimented at W of Terrades and after slided, from E to W in a turbidite basin, without any coarse clastic