Traducción humanística (literaria y audiovisual)

Con la integración de las asignaturas de traducción literaria y traducción audiovisual de las tres especialidades (inglés, francés y alemán) dentro de una misma red docente de Traducción Humanística, sus profesores hemos conseguido, mediante una puesta en común, establecer una coherencia programática en nuestros respectivos sílabos que permite prever los conocimientos adquiridos por nuestro alumnado en los elementos comunes a ambas materias antes y durante la impartición de la docencia de una determinada asignatura. También hemos iniciado el proceso de elaboración de unos tutoriales audiovisuales que sirven para explicar la utilización de software para la elaboración de tareas vinculadas a dichas asignaturas, aplicables a cualquiera de los tres idiomas, algunos de los cuales ya están subidos a la página web del Departamento de Traducción e Interpretación para que los alumnos puedan consultarlos antes de empezar la docencia de las respectivas asignaturas. A los dedicados a la localización de traducciones literarias próximamente se incorporarán los de traducción para el doblaje, para el subtitulado convencional y los relacionados con la accesibilidad (audiodescripción y subtitulado para sordos). Con la consolidación de esta red tras el primer año de trabajo en común se seguirá progresando en esta conjunción de estrategias didácticas y cumplimiento de objetivos.

Rockingham County, New Hampshire, 1857 (Image 1 of 4) (Raster Image)

This layer is a georeferenced raster image of the historic paper map entitled: Map of Rockingham Co., New Hampshire, by actual surveys by J. Chace, Junr. It was published by Smith and Coffin in 1857. Scale [ca 1:15,840]. This layer is image 1 of 4 total images, representing the northeast portion of the four sheet source map. The image covers an inset of the City of Portsmouth but is not georeferenced for the city. The image inside the map neatline is georeferenced to the surface of the earth and fit to the New Hampshire State Plane coordinate system (NAD 1983 in Feet) (Fipszone 2800). All map collar and inset information is also available as part of the raster image, including any inset maps, profiles, statistical tables, directories, text, illustrations, index maps, legends, or other information associated with the principal map. This map shows features such as roads, railroads, drainage, public buildings, schools, churches, cemeteries, industry locations (e.g. mills, factories, mines, etc.), private buildings with names of property owners, town boundaries, and more. It includes many cadastral insets of individual county towns and villages. It also includes illustrations, business directories, and tables of statistics and distances.This layer is part of a selection of digitally scanned and georeferenced historic maps of New England from the Harvard Map Collection. These maps typically portray both natural and manmade features. The selection represents a range of regions, originators, ground condition dates, scales, and map purposes.

Aksa'l-ereb fî tercemeti Mukaddimeti'l-edeb

[Maḥmūd ibn ʻUmar Zamakhsharī].

Kitāb Muqaddimat al-adab

li-Abī al-Qāsim Maḥmūd ibn ʻUmar al-Zamakhsharī.

Hādhā kitāb al-Fīrūzaj: Sharḥ al-Unmūdhaj

li-Muḥammad ʻĪsá ʻAskar.

Rawḍ al-akhyār al-muntakhab min Rabīʻ al-abrār : manuscript, 1576

Title from f. 2r.

Geochemistry of ODP Hole 111-504B basalts (Table 2)

Fifty samples of basalt recovered during ODP Leg 111 from the dikes (Layer 2C) of Hole 504B (1350.0-1562.3 m below seafloor) were analyzed by X-ray-fluorescence techniques. All of the samples are highly depleted in magmaphile elements relative to other mid-ocean ridge basalts, with TiO2 = 0.75-1.24 wt%, Na2O = 1.59-2.22 wt%, Zr = 38-64 ppm, Nb = 0.3-1.5 ppm, and Y = 20-30 ppm (for samples containing 0%-2% phenocrysts), but have ratios of highly incompatible elements similar to normal Type I mid-ocean ridge basalts (e.g., Zr/Nb > 30). Abundances of compatible elements are similar to those of typical mid-ocean ridge basalts, with MgO = 7.2-9.2 wt%, Fe2O3* = 9.3-12.5 wt%, Ni = 55-164 ppm, and Cr = 26-388 ppm. Approximately 2% of the samples recovered from the top part of Hole 504B are similar to normal Type I or Type II ocean floor basalts. However, all of the analyzed Leg 111 samples from Hole 504B are depleted basalts. Aphyric dike rocks from Leg 111 are virtually identical to the depleted aphyric samples recovered from the pillow lavas and dikes in the upper 1075 m of Hole 504B during DSDP Legs 69, 70, and 83, with the exception of elements readily altered by seawater (Sr, Rb, and K). These elements reach a maximum in both abundance and variability in the pillow lavas of the upper 571.5 m of Hole 504B and decline to more constant values in the dike system sampled on Legs 83 and 111, apparently as a result of a decrease in porosity and increase in alteration temperatures relative to the pillow lavas. Based on compositional similarities to the vast majority of the pillows and flows, the dikes sampled on Leg 111 appear to be the feeder system for the pillow lavas in the upper part of Hole 504B. The incompatible-element-depleted compositions of the Costa Rica Rift Zone basalts are consistent with multistage melting of a normal mid-ocean ridge source.

(Table 2) Age determination of sediment core NIOP-C2_929

In this study we present a sea surface temperature (SST) record from the western Arabian Sea for the last 20,000 years. We produced centennial-scale d18O and Mg/Ca SST time series of core NIOP929 with focus on the glacial-interglacial transition. The western Arabian Sea is influenced by the seasonal NE and SW monsoon wind systems. Lowest SSTs occur during the SW monsoon season because of upwelling of cold water, and highest SSTs can be found in the low-productivity intermonsoon season. The Mg/Ca-based temperature record reflects the integrated SST of the SW and NE monsoon seasons. The results show a glacial-interglacial SST difference of ~2°C, which is corroborated by findings from other Arabian Sea cores. At 19 ka B.P. a yet undescribed warm event of several hundred years duration is found, which is also reflected in the d18O record. A second centennial-scale high SST/low d18O event is observed at 17 ka B.P. This event forms the onset of the stepwise yet persistent trend toward Holocene temperatures. Highest Mg/Ca-derived SSTs in the NIOP929 record occurred between 13 and 10 ka B.P. Interglacial SST is ~24°C, indicating influence of upwelling. The onset of Arabian Sea warming occurs when the North Atlantic is experiencing minimum temperatures. The rapid temperature variations at 19, 17, and 13 ka B.P. are difficult to explain with monsoon changes alone and are most likely also linked to regional hydrographic changes, such as trade wind induced variations in warm water advection.