762 resultados para 1480
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El Campus de la Universidad de Alicante es un espacio de una enorme calidad tanto por sus arquitecturas construidas, la mayoría notables y algunas de ellas magníficas, como por sus espacios libres, zonas verdes e hitos que lo dotan de identidad y llenan de significados varios. Pero, además, es el espacio de trabajo, de relación y encuentro, de vida en definitiva, de toda la comunidad universitaria, razón por la cual, el proyecto institucional Campus Accesible, Campus Igualitario, promovido por el Vicerrectorado de Campus y Sostenibilidad en colaboración con la Unidad de Igualdad y el Vicerrectorado de Estudiantes, se plantea como objetivo primordial alcanzar la misma excelencia como espacio modelo de integración de todas las personas, sea cual fuere su situación o condición. Para ello atiende a dos aspectos básicos: uno, la consecución de accesibilidad universal y, dos, la incorporación de la perspectiva de género a su construcción, mantenimiento y gestión como generadora de nuevas miradas que enriquecen los espacios y la vida desde la bienvenida a los mismos de la complejidad y la diversidad. El presente trabajo recoge tanto las reflexiones como las acciones que, en esta dirección y con carácter transversal y pionero, se han desarrollado.
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This layer is a georeferenced raster image of the historic paper map entitled: Melite vulgo Malta : cum vicinis Goza, quae olim Gaulos, et Comino insulis : sita est haec insula inter Barbariam et Siciliam ad 35. Grad 53 min. latitudinis et 32 Grad 30 min. long, uti exhibetur á Nic. de Fer ; nunc aeri incisa per Matth. Seutter, S. C. M. geogr. Augustanum. It was published by Matth. Seutter, ca. 1745. Scale [ca. 1:41,000]. Covers Malta. Map in Latin.The image inside the map neatline is georeferenced to the surface of the earth and fit to the Europe Lambert Conformal Conic coordinate system. 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 drainage, roads, cities and other human settlements, built-up areas, fortification, shoreline features, harbors, and more. Relief shown pictorially. Includes also inset map of Valletta, and "Nomina et insignia magistrorum equitum ordinis Melitensis ...".This layer is part of a selection of digitally scanned and georeferenced historic maps from the Harvard Map Collection. These maps typically portray both natural and manmade features. The selection represents a range of originators, ground condition dates, scales, and map purposes.
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li-Muḥammad ibn Aḥmad ibn Muḥammad al-Ṭarasūsī.
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Narsi Mehta, Pīr Ghauṣ, Miskīn, ... [et al.].
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Este estudo foi realizado com o propósito de desenvolver e validar o sistema de observação da comunicação cinésica do instrutor de fitness, assim como realizar uma aplicação piloto do mesmo. No processo de desenvolvimento e validação do novo sistema de observação foram consideradas cinco fases sequenciais. No final deste processo foi estabelecida a validade e fiabilidade de 5 dimensões e 21 categorias de comportamento cinésico dos instrutores, criando-se a versão final deste sistema de observação. Esta versão do sistema de observação foi aplicada num estudo piloto a uma amostra de 12 instrutores de quatro atividades de grupo distintas. Os resultados indicam que o comportamento proxémico dos instrutores pode ser codificado com recurso ao sistema de observação da comunicação cinésica do instrutor de fitness, tendo sido realizada uma análise comparativa acerca da sua intervenção nas diversas atividades, ainda que com uma amostra reduzida.
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Deep-sea sediments of two cores from the western (TY93-929/P) and the southeastern (MD900963) Arabian Sea were used to study the variations of the Indian monsoon during previous climatic cycles. Core TY93-929/P was located between the SW monsoon driven upwelling centres off Somalia and Oman, which are characterized by large seasonal sea surface temperature (SST) and particle flux changes. By contrast, core MD900963, was situated near the Maldives platform, an equatorial ocean site with a rather small SST seasonality (less than 2°C). For both cores we have reconstructed SST variations by means of the unsaturation ratio of C37 alkenones, which is compared with the delta18O records established on planktonic foraminifera. In general, the SST records follow the delta18O variations, with an SST maximum during oxygen isotope stage 5.5 (the Last Interglacial at about 120-130 kyr) and a broad SST minimum during isotope stage 4 and 3.3 (approximately 40-50 kyr). The SST difference between the Holocene and the Last Glacial Maximum (LGM) is of the order of 2°C. In both cores the SSTs during isotope stage 6 are distinctly higher by 1-2°C than the cold SST minima during the last glacial cycle (LGM and stage 3). To reconstruct qualitatively the past productivity variations for the two cores, we used the concentrations and fluxes of alkenones and organic carbon, together with a productivity index based on coccolith species (Florisphaera profunda relative abundance). Within each core, there is a general agreement between the different palaeoproductivity proxies. In the southeastern Arabian Sea (core MD900963), glacial stages correspond to relatively high productivity, whereas warm interstadials coincide with low productivity. All time series of productivity proxies are dominated by a cyclicity of about 21-23 kyr, which corresponds to the insolation precessional cycle. A hypothesis could be that the NE monsoon winds were stronger during the glacial stages, which induced deepening of the surface mixed layer and injection of nutrients to the euphotic zone. By contrast, the records are more complicated in the upwelling region of the western Arabian Sea (core TY93-929/P). This is partly due to large changes in the sedimentation rates, which were higher during specific periods (isotope stages 6, 5.4, 5.2, 3 and 2). Unlike core MD900963, no simple relationship emerges from the comparison between the delta18O stratigraphy and productivity records. The greater complexity observed for core TY93-929/P could be the result of the superimposition of different patterns of productivity fluctuations for the two monsoon seasons, the SW monsoon being enhanced during interglacial periods, whereas the NE monsoon was increased during glacial intervals. A similar line of reasoning also could help explain the SST records by the superimposition of variations of three components: global atmospheric temperature, and SW and NE monsoon dynamics.
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Cover title.
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Geertgen tot Sint Jans; 3 ft. 1/16 in.x 2 ft. 4 17/64 in.; oil on panel
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Master of the Prado "Adoration of the Magi"; 1 ft. 10 51/64 in.x 1 ft. 6 13/16 in.; oil on panel
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Portada a dos tintas con escudo y orla xilográficos.
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Contiene según consta en portada: Primeramente vn ... prologo y argumento ; Ite[m] vna decada d[e] Cesares ... ; Item vn libro de auiso de p[ri]uados y docrina d[e] cortesanos ... ; Yte vn libro del menosprecio de la corte y alabança de la aldea ... ; Ytem vn libro de los inue[n]tores del marear, y de sesenta trabajos q[ue] ay en las galeras ...
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Mode of access: Internet.
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Mode of access: Internet.
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Ruiz Fidalgo,