983 resultados para Navas de Tolosa, Batalla de, 1212


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This work was left incomplete by the author, wanting the projected v. 3 and the end of v. 2.

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Mode of access: Internet.

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"Representada por primera vez en el teatro del Príncipe la noche del 24 de diciembre de 1856" -port.-

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Mode of access: Internet.

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Thesis (doctoral)--Kaiser-Wilhelms-Universitat Strassburg i. E.

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De acuerdo a lo que se ha dado en llamar "historia del sentido" (Assmann, 2005), cada sociedad posee una forma cultural que le es inherente y es precisamente en ella donde adquieren sentido los acontecimientos y procesos históricos, comprensibles sólo a través de los discursos producidos. Los relieves y las inscripciones de la Batalla de Kadesh, durante el reinado de Ramsés II (1279-1213 a.C.) constituyen un claro ejemplo de rememoración y manifestación de esos discursos. En este trabajo, nos proponemos analizarlos como ejemplos de procesos constructivos de la "memoria cultural" (Assmann, 2008), tomando como categorías de análisis los postulados de la semiótica de Umberto Eco (1994 (1973); 2013 (1968)) y del análisis de la imagen de Martine Joly (2012 (1993)). Como premisa básica, consideraremos a los relieves y las inscripciones que los acompañaban como una unidad total narrativa, como discursos que se completan y complementan, para ser eficaces.

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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.