739 resultados para Catedral de Burgos


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At head of title: Asociación de arquitectos de Cataluña.

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"Oracion fùnebre pronunciada por el presbitero don Felix Varela, catedratico de filosofia en el Real Colegio de San Carlos de la Habana": p. [7]-15.

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This study analyzes Carmen de Burgos' European travel literature, and focuses on two themes: education and travel literature as a literary genre. An examination of her travel literature reveals two essential elements related to her view of education. The first is the influence that the European educational system had on her way of thinking, particularly with respect to the idea of tolerance, the practice of hygiene, and the important role of nature in education. The second is the development of her view of education as the foundation for the emancipation of women in Spain. Carmen de Burgos espoused the view that the reform of the Spanish educational system was the primary and foundational goal to further social, political and economic progress of women in Spain at the end of the 19th and beginning of the 20th Century. ^ In the second part of this dissertation I support the theory that her travel literature was her main source to convey to Spanish women the need for social change. I do this by analyzing four properties that are considered characteristic of women's travel literature: (1) the woman as a hero, (2) scientific authority of women, (3) feminine style, and (4) feminine content. I argue that Carmen de Burgos's travel literature uses these properties to facilitate her access to women audiences and to assure that this audience regarded her as an authoritative voice. ^

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The Pico de Navas landslide was a large-magnitude rotational movement, affecting 50x106m3 of hard to soft rocks. The objectives of this study were: (1) to characterize the landslide in terms of geology, geomorphological features and geotechnical parameters; and (2) to obtain an adequate geomechanical model to comprehensively explain its rupture, considering topographic, hydro-geological and geomechanical conditions. The rupture surface crossed, from top to bottom: (a) more than 200 m of limestone and clay units of the Upper Cretaceous, affected by faults; and (b) the Albian unit of Utrillas facies composed of silty sand with clay (Kaolinite) of the Lower Cretaceous. This sand played an important role in the basal failure of the slide due to the influence of fine particles (silt and clay), which comprised on average more than 70% of the sand, and the high content presence of kaolinite (>40%) in some beds. Its geotechnical parameters are: unit weight (δ) = 19-23 KN/m3; friction angle (φ) = 13º-38º and cohesion (c) = 10-48 KN/m2. Its microstructure consists of accumulations of kaolinite crystals stuck to terrigenous grains, making clayey peds. We hypothesize that the presence of these aggregates was the internal cause of fluidification of this layer once wet. Besides the faulted structure of the massif, other conditioning factors of the movement were: the large load of the upper limestone layers; high water table levels; high water pore pressure; and the loss of strength due to wet conditions. The 3D simulation of the stability conditions concurs with our hypothesis. The landslide occurred in the Recent or Middle Holocene, certainly before at least 500 BC and possibly during a wet climate period. Today, it appears to be inactive. This study helps to understand the frequent slope instabilities all along the Iberian Range when facies Utrillas is present.

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En el presente trabajo se analiza primeramente el proceso de fundación, a fines del siglo XV, del colegio de San Gregorio de Valladolid por parte del obispo dominico, consejero y confesor real Alonso de Burgos; el colegio, de patronato real y centrado en los estudios de teología, estaba reservado exclusivamente para frailes predicadores observantes. A continuación, y como parte más amplia y fundamental del estudio, se analizan los primeros estatutos que tuvo el colegio, otorgados por su fundador, ofreciéndose finalmente, en apéndice documental, su transcripción completa.

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In this paper we analyze the set of Bronze Age bone tools recovered at the archaeological site of El Portalón of Cueva Mayor in the Sierra de Atapuerca (Burgos). The Bronze Age cultural period is the best represented in the cavity and its study has forced us to unify the different excavation and stratigraphical criteria undertaken from the earliest archaeological excavations developed by J.M. Apellániz during the 70s until the excavations of the current research team (EIA) since 2000. We propose here for the first time a relationship between the initial system of “beds” used by Apellániz and our recent sedimentary sequence that recognizes eleven stratigraphic levels radiometrically dated from the late Upper Pleistocene to the Middle Age. Within the bone industry assemblage we recognize a large variety of utensils and ornamental elements, with native and allochthonous features, that make evident a regional as well as long distance relationships of these populations of the interior of the Iberian Peninsula during the recent Prehistory.