721 resultados para 982


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Un episodio del retorno de los argonautas, en el Libro IV de Apolonio, inserta bruscamente un escenario homérico. Desde la isla de Eea, donde han sido purificados por Circe, son conducidos bajo la protección de Hera hasta Corcira -Esqueria en Odisea-, en una veloz travesía que ve sucederse sin riesgos los otrora peligrosos escollos de la ruta de Odiseo. La idea de hacer coincidir a los argonautas con los feacios homéricos aparece solo claramente en los poetas helenísticos. Calímaco parece haber dedicado especial atención a la escala feacia, en terminus similares -peso no idénticos- a los de Apolonio',y Filitas menciona unas hadas de Medea y Jason en el palacio de Alcinoa'. Testimonios anteriores asocian asimismo a Medea, Jason y sus hijos con Corcina...

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Generación de nuevos programas académicos que resulten adecuados para la realidad del país y se constituyan en fuentes de soluciones y desarrollos innovadores para el avance y crecimiento de la nación colombiana. programa de Doctorado en Economía

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u.a. Frankfurter Zeitung; Politik; Bildnis Schopenhauer;

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The Cenozoic volcanic activity on Iceland has been recorded in North Atlantic sediments drilled during several Ocean Drilling Program (ODP)/Deep Sea Drilling Project legs (Legs 104, 151, 152, 162, and 163). Leg 162 (North Atlantic-Arctic Gateways II) recovered ash layers at Sites 982, 985, and 907 (Jansen, Raymo, Blum, et al., 1996, doi:10.2973/odp.proc.ir.162.1996). The revisited Site 907 was first drilled during Leg 151, and the ash from this site has been described in detail by Lacasse et al. (1996, doi:10.2973/odp.proc.sr.151.122.1996) and Werner et al. (1996, doi:10.2973/odp.proc.sr.151.123.1996). Site 982 is located within the Hatton-Rockall Basin on the Rockall Plateau, which is situated west of the British Isles. Site 985 is located northeast of Iceland at the foot of the eastern slope of the Iceland Plateau, adjacent to the Norwegian Basin. Here we report chemical analyses of Neogene tephra layers from Holes 982A, 983B, 982C, 985A, and 985B. The sedimentary sequence at Site 982 spans the lower Miocene-Holocene; Site 985 recovered sediments spanning the upper Oligocene-Holocene. Twenty-two distinct ash layers and ash-bearing sediments were sampled in Holes 982A-982C (Cores 162-982A-16H through 24H, 162-982B-14H through 56X, and 162-982C-15H through 27H), and 59 ash layers were sampled in Holes 985A and 985B (Cores 162-985A-11H through 59X, and 162-985B-11H through 14H). Almost 50% of the sampled ash is strongly altered (predominantly from Site 985). A cluster of altered thin layers in the lower Pliocene of Site 985 (top of Unit III) is remarkable.