1000 resultados para Jeroni, sant, ca. 342-420
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Two reminiscences from the Cicero's speeches against Catiline in the letters of St Jerome and St Augustine.
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Mode of access: Internet.
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Mode of access: Internet.
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Mode of access: Internet.
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Mode of access: Internet.
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In this paper we study the presence of elements related to Roman games in the work of the bishop Paulinus of Nola (355-431 AD). References to shows in his work are not as abundant as they occurs among his contemporaries. Nevertheless, many of these references possess a great importance for us. Certainly, they are similar to other allusions made by his contemporaries; however they express the opinion of one of the most famous and prestigious bishops of the Late Antiquity about these popular exhibitions. In his writings we can see his criticism of the waste of wealth in the organization of the Roman games, and also the use of a metaphorical language with ludical reminiscences whose origins go back to Paul of Tarsu
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El primer tercio del siglo V representó un momento muy convulso en la historia del Imperio Romano. Algunas zonas, como la Galia, se vieron inmersas en una crisis provocada principalmente por las devastaciones que poblaciones bárbaras estaban llevando a cabo, desde inicios de la centuria, en casi todo su territorio. El foedus pactado por el Imperio con los visigodos, por el cual éstos se establecían en Aquitania (418), lejos de representar una solución no hizo sino aumentar los problemas de convivencia entre galorromanos y germanos. El pesimismo cundió entre la población autóctona: la teología eusebiana que presentaba al Dios cristiano como garante de los bienes materiales a través de su culto ―siguiendo la tradicional ideología del do ut des― había fallado, y muchas conciencias cristianas se hundieron en la angustia al preg
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Deposits of coral-bearing, marine shell conglomerate exposed at elevations higher than 20 m above present-day mean sea level (MSL) in Bermuda and the Bahamas have previously been interpreted as relict intertidal deposits formed during marine isotope stage (MIS) I I, ca. 360-420 ka before present. On the strength of this evidence, a sea level highstand more than 20 m higher than present-day MSL was inferred for the MIS I I interglacial, despite a lack of clear supporting evidence in the oxygen-isotope records of deep-sea sediment cores. We have critically re-examined the elevated marine deposits in Bermuda, and find their geological setting, sedimentary relations, and microfaunal assemblages to be inconsistent with intertidal deposition over an extended period. Rather, these deposits, which comprise a poorly sorted mixture of reef, lagoon and shoreline sediments, appear to have been carried tens of meters inside karst caves, presumably by large waves, at some time earlier than ca. 310-360 ka before present (MIS 9-11). We hypothesize that these deposits are the result of a large tsunami during the mid-Pleistocene, in which Bermuda was impacted by a wave set that carried sediments from the surrounding reef platform and nearshore waters over the eolianite atoll. Likely causes for such a megatsunami are the flank collapse of an Atlantic island volcano, such as the roughly synchronous Julan or Orotava submarine landslides in the Canary Islands, or a giant submarine landslide on the Atlantic continental margin. (c) 2006 Elsevier B.V. All rights reserved.
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Mode of access: Internet.
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Mode of access: Internet.
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Mode of access: Internet.
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Mode of access: Internet.
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Datos tomados de ICCU y de CCFR.