7 resultados para Literatura española s.XVIII estudio

em Universitat de Girona, Spain


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Ressenya de l' edició de Ramon Díaz i Villalonga sobre l' obra literària de l'escriptor mallorquí Albert Burguny i Castellò (1707-1770)

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Presentació de les webs de: Enciclopèdia Stanford de Filososofia, Sociedad Española para el estudio de la Ansiedad y el Estrés (SEAS) i Revista Electrònica de Motivació i Emoció (REME)

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El empleo de la filmografía como fuente de transmisión de conocimientos no es per se novedoso. En realidad, los conocimientos más especializados a los que parece se dirigen los estudios de la ESO y del Bachiller, que sustituyen al conocimiento general tan estilado en otras épocas, dificulta que un porcentaje elevado de alumnos universitarios hayan leído las piezas esenciales de la literatura española y comparada, y tengan el hábito de consultar, sino diariamente, con cierta frecuencia, el periódico. Es difícil, pues, buscar un ejemplo que les resulte familiar acudiendo a la literatura y a la prensa escrita. A ello se suma el impulso imparable de la televisión y, más recientemente, el acceso cómodo a través de Internet a películas prácticamente de estreno o a trailers de las mismas. El cine está más próximo al alumno, a la época que le toca vivir, y en él se encuentran múltiples referencias que permiten aproximar la materia que se debe explicar a la realidad del receptor de la información

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The amorphous silica (opal-A) speleothems associated to the open structural system of granitic rocks where the slow circulation of runoff is produced are mainly the result of the biological degradation of the rock. These speleothems are found in many different geographic, climatic and geological environments though always associated to granitoids. They show two different morphologies: cylindrical or long bodies and laminar or layered forms. They are internally formed by a mass of clasts and spheres of opal-Awith a porous texture that evolves to compact and massive due to the reiteration of the re-dissolution/re-precipitation of the amorphous opal by the water that circulates through it after each rainfall period. A final characteristic of each growth stage (end of rainy period) is the development of whiskers of minerals, normally gypsum, on the water output points of the speleothems. The dimensions of the speleothems are millimetric (length and/or thickness). In this paper their morphology and mineralogy are described based on their study by SEM, XRD and XRF, and there is established a new and more complete genetic hypothesis than the one that exists up to now to understand their formation

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The paludal deposits presented here belong to a geomorphological unit identified between Palafrugell Corridor and the littoral plains of Ter River (Baix Ter), associated to a carbonate-rich spring system. The sections show a distintic clay level, mixed with black silts, very rich in snail remains. The malacological assemblage contained stillwaters species (Bithynia leachii, Galba truncatula, Pisidium milium, Radix peregra) along with damp species (Monacha cartusiana, Oxyloma elegans, Succinea putris, Succinella oblonga, Vallonia pulchella, Vertigo sp.). Some open-dry species are also present (Cernuella virgata, Eobania vermiculata, Pomatias elegans, Rumina decollata) revailing a mosaic-like landscape. Radiocarbon dates place this level ca. 7.000BPwithin the Holocene sequence of the Baix Ter basin. Colluvial deposits on top of these paludal levels have a typical open-dry malacological assemblage (Cernuella virgata, Cochlicella acuta, Eobania vermiculata, Pomatias elegans, Rumina decollata, Trochoidea elegans) the same assemblage that inhabits the Empordà littoral plains nowadays

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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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Estudi de conjunt de la figura i l'obra de fra Agustí Eura i a l'edició crítica de la seva poesia completa. La tesi està publicada en 2 obres impreses. Les referències es localitzen a Qüern 5, refs. 1298 i 1301