998 resultados para Napoleon Bonaparte


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Boberach: Behandelt werden Alexander Freiherr von Soiron, Jakob Venedey, Oskar von Wydenbrugk, Gottlieb Christian Schüler, Heinrich Freiherr von Gagern, Ernst Moritz Arndt, Carl Theodor Welcker, Friedrich Ludwig Jahn, Franz Schuselka, Friedrich Siegmund Jucho, Johann Gustav Moritz Heckscher, Felix Fürst von Lichnowsky, Friedrich Christoph Dahlmann, Anton Ritter von Schmerling, Franz Raveaux, Heinrich Simon, Johann Jacoby, Robert Blum, Johann Erzherzog von Österreich, Louis Cavaignac, Friedrich Hecker, Friedrich von Wrangel, Joseph Wenzel Graf Radetzky, Joseph Freiherr Jellachich von Buszin, Hermann Rollett, Alphonse de Lamartine, Georg Jung, Louis Napoleon, Ernst Alfred Fürst zu Windischgrätz, Ferdinand Freiligrath, Ludwig Kossuth, Emanuel Geibel

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Eugen Neureuther

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Fanny Januschek, Napoleon III, Frankfurt

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Berufspläne, Der wahre Jakob, Politische Bemerkungen, Ferdinand Freiligrath, Napoleon III, Amerikanische Presse, Frankfurter Latern

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Fil: Bonaparte, Adrián. Universidad Nacional de La Plata. Facultad de Humanidades y Ciencias de la Educación; Argentina.

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Fil: Bonaparte, Adrián. Universidad Nacional de La Plata. Facultad de Humanidades y Ciencias de la Educación; Argentina.

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Fil: Bonaparte, Adrián. Universidad Nacional de La Plata. Facultad de Humanidades y Ciencias de la Educación; Argentina.

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One of the essential problems of oceanic tectonics is estimation of the influence of plumes of the deep hot mantle on processes in the axial spreading zone. Areas of two giant (St. Helena and Tristan da Cunha) plumes in the Mid-Atlantic Ridge (MAR) rift zone (South Atlantic) are characterized by the effusion of basalts that differ from typical depleted riftogenic tholeiites by anomalously high contents of lithophile components and specific isotopic compositions. Moreover, the rift valley floor with basalt effusion is significantly uplifted above the adjacent sectors of the rift. The formation of the St. Helena Seamount located 400 km east of the MAR axis is related to magmatism that is active to this day. St. Helena Island is a member of the structural ensemble of large volcanic seamounts (Bonaparte, Bagration, and Kutuzov). Like St. Helena Island, each seamount incorporates a series of smaller rises of different morphologies and dimensions. Thus, a system of subparallel series of NE-trending (~45°) rises extend from the seamount ensemble to the African continent. According to the plate tectonics concept, the seamount series represent hotspots related to a deep mantle plume that can be projected onto the present-day St. Helena Island area (St. Helena plume). At the same time, the inferred topographic map based on satellite altimetry data shows that the seamount series also extend along the opposite southwestern direction (~225°) toward the axial MAR and even intersect the latter structure. This fact cannot be explained by the hotspot hypothesis, which suggests stationary positions of plumes relative to the mobile oceanic plate. In the course of Cruise 10 of the R/V Akademik Ioffe (2002), detailed geological and geophysical investigations were carried out at the junction of one structural series with the MAR rift zone located near the Martin Vaz Fracture Zone (Martin Vaz test area, 19°-20° S). The present communication is devoted to the study of lithology, geochemistry, and isotopy of basalts dredged at the test area.

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During the Peninsular War, Napoleon's and Wellington's armies were aware of the lack of precision in the maps of Spain and its provinces that appeared in Tomas Lopez \s Geographical Atlas of Spain. The errors were due to the non-topographical surveying method he used which he had learned from his teacher Jean Baptiste Bourguignon D 'Anville. To map all of the Spanish provinces, Tomas Lopez divided them into circles of three leagues in diameter (16,718 m), taking a particular town as the centre. He asked the town's priest to draw a map of the territory and to complete a questionnaire that Tomas Lopez sent to him. The priest was to return the two documents after he had completed them. Subsequently, at his desk, Tomas Lopez used the maps and reports as well as other graphic and written sources from various locations to make an outline of each map. Next, he made a mosaic that served as a pattern for drawing the final provincial map. We will see the way that this method was applied in two concrete cases: the villages ofChavaler and Monteagudo, situated in the Spanish province of Soria, and verify their degree of accuracy. We will use the maps drawn by the priests in 1767, the final map of the province which was published in 1804 by Tomás López, and a current map of the province showing the angular and linear errors in Lopez \s map.

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Contiene: Carta que dirige Williams Piit al Emperador Napoleon