984 resultados para rose bengal
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Despite its being the first testimony of Chaucer’s genius, the interest of modern criticism in the Romaunt has mainly focused on the issue of authorship, whereas the efforts to assess this text as a translation have been limited both in their number and in their scope. This paper discusses Chaucer’s translation of the Roman de la Rose, and provides an evaluation of Fragment A from a modern traductological perspective, while taking account of contemporary theoretical positions. First, this article compares the Romaunt with Chaucer’s later translating practice. Second, taking into account that the immediate audience of the Romaunt would have been cognizant of French, this essay considers the pragmatic function of this translation. Finally, I reconstruct some of Chaucer’s decisions in the translation process, and then I present the translation strategies he adopted in order to create an English metapoem which replicated the spirit of the Roman, thus proving the adequacy of English for poetic expression.
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A film of Eric Serra's audio recording session of Doudou N'Diaye Rose and his drumming ensemble outdoors on the island of Gorée, off the coast of Dakar, Senegal. The film concentrates on two performances -- one shot in daytime, and one at night. Two performances are filmed, punctuated by images of the island.
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The state of consolidation of outer Bengal Fan deposits is closely related to their depositional history. Early Pleistocene sediments are underconsolidated, i.e., fabric strength is lower than under equilibrium with the present overburden stress, at depths greater than 60-80 mbsf. This may be due to rapid accumulation (>15-20 cm/k.y.) and overlying low-permeability (<10**-7 cm/s) deposits. The underlying Pliocene sediments are overconsolidated, i.e., fabric strength is higher than in equilibrium with the present overburden stress; at Sites 717 and 719 the sediments are slightly overconsolidated, whereas at Site 718 the overconsolidation is significant. Overconsolidation is explained by erosion that occurred during the early Pleistocene for which a stratigraphic gap was recorded in the drilled cores. The eroded section is estimated to be in the range of 10-40 m at Sites 717 and 719, respectively, and 130-150 m at Site 718. Below 250-300 mbsf the most sediments are normally consolidated. The amount of erosion seems to be related to block rotation and uplift due to intraplate deformation.
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Mode of access: Internet.
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