913 resultados para AK22-1928


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Mode of access: Internet.

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One fundamental question raised by the philosophical works of Maurice Blondel, which were published over a long life, is that of the relation between his early masterpiece L’Action (1893) and the volume of the same name—more precisely, its second tome L’Action humaine et les conditions de son aboutissement (1937)—forming part of the Trilogy of his later years (La Pensée; L’Être et les êtres; L’Action). The treatment of the nature of international relations in the work of 1937 is more developed than that found in L’Action of 1893. For understanding the development of Blondel’s thought on this matter, the key text is "Patrie et Humanité", a paper prepared for the 1928 annual meeting, held in Paris, of the Catholic Semaine sociale movement. It brings out the affinity between his understanding of international relations and that represented by such established thinkers in the canon of international thought as Vitoria and Suarez (in the case of the latter, despite some radical difference in respect of metaphysics). Not surprisingly from the standpoint of the genesis of Blondel’s philosophy, there is also a certain affinity between his view of the importance of justice for international affairs and that of Leibniz (notably in the preface of the Codex Juris Gentium, 1693). Various specialists treating of Blondel’s philosophy have drawn attention to parallels between the phenomenology of the will in L’Action of 1893 and Hegel’s Phänomenologie des Geistes. However, as regards the two philosophers’ understanding of the nature of international relations, there is a considerable gulf, and some of the difference may be related to the Hegelian idea of the Christian Church as found, at least implicitly, in the Grundlinien der Philosophie des Rechts (1821).

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During the period in question, large ice drifts transported incalculable numbers of icebergs, ice fields and ice floes from the Antarctica into the South Atlantic, confronting long-journeying sailing ships on the Cape Horn route with considerable danger. As is still the case today, the ice drifts generally tended in a northeasterly direction. Thus it can be assumed that the ice masses occuring near Cape Horn and in the South Atlantic originated in Graham Land and the South Shetland Islands, while those found in the Pacific will have come from Victoria Land. The masses drifting to Cape Horn, Isla de los Estados, the Falkland Islands and occasionally as far as the Tristan da Cunha Group are transported by the West Wind Drift and Falkland Current, diverted by the Brazil Current. The Bouvet and Agulhas Currents have little influence here. The great ice masses repeatedly reached points beyond the "outermost drift ice boundery" calculated in the course of the years, to continue on in the direction of the equator. The number of sailing ships which fell victim to the ice drifts while rounding Cape Horn can only be surmised; they simply disappeared without a trace in the expanses of the South Atlantic. Until the end of the 1900s the dangers presented by ice were less serious for westward-bound ships than for the "homeward-bounders" travelling from West to East. Following the turn of the century, however, the risk for "onwardbounders" increased significantly. Whether the ice drifts actually grew in might or whether the more frequent and more detailed reports led to this impression, could never be ascertained by the German Hydrographie Office. In the forty-one years between 1868 and 1908, ten light, ten medium and nine heavy ice years were counted, and only twelve years in which no reports of ice were submitted to the German Hydrographie Office. "One of the most terrible dangers threatening ships on their return from the Pacific Ocean," the pilot book for the Atlantic Ocean warns, "is the encounter with ice, to be expected south of the 50th parallel (approx.) in the Pacific and south of the 40th parallel (approx.) in the South Atlantic." Following the ice drift of 1854-55, thought to be the first ever recorded, the increasing numbers of sailing ships rounding Cape Horn were frequently confronted with drifts of varying sizes or with single icebergs. Then from 1892-94, a colossal ice drift crossed the path of the sailships in three stages. Several sailing ships collided with the icebergs and could be counted lucky if they survived with heavy damage to the bow and the fo regear. The reports on those which vanished for ever in the ice masses are hardly of investigative value. The English suffered particularly badly in the ice-plagued waters; their captains apparently sailed courses that led more freqently through drifts than did the sailing instructions of the German Hydrographic Office. Thus, among others, Capt. Jarvis' DUNTRUNE, also the STANMORE, ARTHURSTONE and LORD RANOCH as well as the French GALATHEE and CASHMERE all collided with icebergs. The crew of the AETHELBERTH panicked after a collision and took to their lifeboats. It was only after the ship detached itself from the iceberg it had rammed that the men returned to it and continued their journey. The TEMPLEMORE, on the other hand, had to be abandoned for good. Of the German sailing ships, the FLOTOW is to be mentioned here, and in the third phase of the drift the American SAN JOAQUIN lost a large proportion of its rigging. In the 20th century ice drifts continued to cross the courses of the Cape Horn ships. 1906 and 1908 were recorded as particularly heavy ice years. In 1908-09 both the FALKLANDBANK and the TOXTETH fell prey to ice, or so it was assumed during the subsequent Maritime Board proceedings. For the most part the German sailing ships were spared greater damages by sea. Their captains sent detailed ice reports to the German Hydrographic Office, which gratefully welcomed the information and partially incorporated it in the third and final edition of the "Pilot Book for the Atlantic Ocean." From the end of 1926 until the beginning of 1928, the last of the large sailing ships were once again confronted with "tremendous masses of icebergs and ice drifts." Reports of this period originated above all on the P-Liners PADUA, PAMIR, PASSAT, PEKING, PINNAS, PRIWALL and the ships of Gustav Erikson's fleet. The fate of the training sailship ADMIRAL KARPFANGER in connection with the ice in early 1938 was never clearly determined by the Maritime Board proceedings. Collision with an iceberg, however, is thought to be the most likely cause of accident. Today freight sailing ships no longer cross the oceans. The Cape Horn route is relatively insignificant for engine-powered ships and icebergs can be spotted in plenty of time by modern navigation technology ... The large ice drifts are no longer a menace, but only a marginal note in the final chapter of the history of transoceanic sailing.

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El objetivo del artículo es analizar algunos aspectos de los orígenes de la “política cultural” estadounidense en Argentina. La atención se concentrará en el pasaje desde las declaraciones del presidente Hoover, que contribuyeron a favorecer un clima útil y propicio a la intensificación de los intercambios, a los primeros pasos concretos realizados en el periodo de la presidencia de Roosevelt. Se tratará, en particular, de individualizar las características de la cooperación establecida entre organismos estadounidenses y argentinos para favorecer la proyección cultural estadounidense en el país y el intercambio cultural entre Estados Unidos y Argentina, donde se iba intensificando la difusión de un sentimiento anti-imperialista, y que era entonces objetivo de formas de propaganda particularmente agresivas por parte de los regímenes totalitarios.

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Vom Kaukasus bis in den Pamir und vom Tien-Shan zurück nach Moskau, St. Petersburg und Kiew: Die Geschichte der sowjetischen Bergsteiger und ihrer Formen von Gemeinschaft gewährt zum einen neue Einblicke in die Kultur-, Alltags- und Sozialgeschichte der stalinistischen Sowjetunion und in die Lebenswelten eines Teils der intellektuellen Elite, zum andern in die unterschiedliche Symbolik und Funktion dieser nichtrussischen Bergperipherien für das Selbstverständnis des multinationalen sowjetischen Herrschaftsgebiets. Das Machtzentrum Moskau ist dabei geographisch oft weit entfernt und doch stets präsent – ob in der politischen Symbolik vertikaler Berghierarchien (so am Pik Stalin mitten im Pamir) oder in den Repressionen des 'Grossen Terrors', der auch die Alpinisten traf. Die Studie stellt die Bergsteiger als erfolgreiche Akteure in eigener Sache ins Zentrum und eröffnet so eine Perspektive auf die Ebene zwischen Individuum und Staatsmacht im Stalinismus. Sie zeigt, wie die staatlichen Monopolorganisationen im Bereich des Sports und der Freizeit nicht nur der Kontrolle und Sozialisierung ins Sowjetsystem dienten, sondern auch als Ausgangspunkt für eigene Aktivitäten und manchmal sogar als halböffentliche Nischen des Rückzugs und der Kritik genutzt werden konnten. Der zeitliche Bogen spannt sich von den zwanziger bis zu den ausgehenden fünfziger Jahren des 20. Jahrhunderts. Ein ausführliches Einleitungskapitel bietet ausserdem einen Einblick in die Entstehung des russländischen Bergsteigens vor der Revolution.

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The present note deals with the functions and activities done by the Institute of oceanography of Indochina during 1927-1928.

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The present note deals with the functions and activities done by the Institute of oceanography of Indochina during 1928-1929.

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Su meta de Consuelo Meyer fue hacer de la Facultad de Economía una de las mejores en su género no solo en México sino en Latinoamérica “y creo – decía al hacer un balance - que lo conseguí”.