994 resultados para Grand Hotel-Dieu de Lyon
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Contenido: Octavio Nicolás Derisi / Mario Enrique Sacchi – L’inquiétude de Dieu chez saint Augustin / Rosa Muriel Zelasco – Opinar como actitud en San Agustín / Sergio Mancini – El comentario de Santo Tomás a la Física : la división del texto aristotélico / Celina A. Lértora Mendoza – La novedad como presencia según San Ireneo de Lyon / Juan Carlos Alby – The transcendental properties of being. Introduction: a concise history up to Thomas Aquinas / Leo J. Elders S. – Notas y comentarios -- Bibliografía
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This study owes its inception to the wisdom and experience of the staff of the Northeast Fisheries Science Center who, after several decades of surveys in the New York Bight, recognized a unique opportunity to capitalize on the decision to stop ocean dumping of sewage sludge and designed an innovative field study to evaluate effects on living marine resources and their habitats. For decades ocean dumping was viewed as a cheap and effective means for disposal of wastes generated by urbanized coastal areas. Even after the 12-mile site was closed, sewage sludge continued to be dumped at Deepwater Dumpsite 106. The 6-mile site off the NewJersey coast is still used as a dumpsite for dredged material from New York Harbor areas. Discussions continue on the propriety of using the deep ocean spaces for disposal of a variety of material including low level radioactive wastes. Consequently, managers are still faced with critical decisions in this area. It is to be hoped that the results from the 12-mile study will provide the necessary information on which these managers can evaluate future risks associated with ocean waste disposal. (PDF file contains 270 pages.)
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The FIDAWOG workshop held from 29 March to 1 April 1999 in Jinja was the third major stock assessment workshop attended by most of the participants during the project. It followed two workshops, each of which lasted three weeks, held in 1998.
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The Johnny Lyon Hills area is located in Cochise County in southeastern Arizona. The rocks of the area include a central core of Lower pre-Cambrian igneous and metamorphic rocks surrounded by a complexly faulted and tilted section of Upper pre-Cambrian and Paleozoic strata. Limited exposures of Mesozoic and Tertiary sedimentary and volcanic rocks are present at the north end of the map area. Late Tertiary and Quaternary alluvium almost completely surrounds and overlaps upon the older rocks.
The older pre-Cambrian rocks include a section of more than 9000 feet of generally moderately metamorphosed graywackes, slates and conglomerates of the Pinal schist injected in zones by somewhat younger rnyolite sheets. The original sediments were deposited in a geosyncline whose extent probably included large parts of Arizona, New Mexico and west Texas. During the Mazatzal Revolution the Pinal schist was deformed into northeast-trending, steeply dipping and plunging structures and the entire local section was overturned steeply toward the northwest. The pre-Cambrian Johnny Lyon granodiorite was emplaced as a large epi-tectonic pluton which modified the metamorphic character of part of the Pinal schist. Larsen method determinations indicate an age of about 715 million years for this rock, which is about the minimum age compatible with the geologic relations.
The Laramide orogeny produced numerous major thrust faults in the area involving all rocks older than and including the Lower Cretaceous Bisbee group. Major compression from the southwest and subsequent superimposed thrusting from the southeast and east are indicated. Minimum thrust displacements of more than a mile are clear and the probable displacements are of much greater magnitude. The crystalline core behaved as a single structural unit and probably caused important local divergences from the regional pattern of northeast-trending compressive forces. The massif was rotated as a unit 40 degrees or more about a northwest-trending axis overturning the pre-Cambrian fold axes in the Pinal schist.
Swarms of Late Cretaceous(?) or Early Tertiary(?) lamprophyric dikes cross the Laramide structures and are probably related to the large Texas Canyon stock several miles southeast of the map area. Intermittent high angle faulting, both older and younger than the dikes, has continued since the Laramide orogeny and has been superimposed on the older structures. This steep faulting combined with the fundamental northwesterly Laramide structural grain to produce the northwesterly trends characteristic of the mountain ridges and valleys of the area.
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Urteko kontuen analisia eta etorkizuneko urteko kontu probisionalak lantzea. Euskera.
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The Bassam artificial inlet was opened (in September 22, 1987) in order to revacuate offshore invasive aquatic plants. This has considerably modified the hydro-sedimentary environment of the lagoonal domain at Grand-Bassam. Tidal currents effect has confered the lagoonal waters an estuarine feature, the saline intrusion (25-35%o) increased beyond the Moossou bridges up to the confluence of the Comoe river. This has led to a cleaning of the river lower course and above all to the bottoms of the lagoon, which were previously confined. The remobilization of mud (from lagoonal bottoms around Bouet Island) evacuated offshore, has exposed lagoonal and oceanic sandy features. This new system remains fragile, with the seasonal (low river-flow) clogging.
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This paper presents the results of a comparative study of three series of samples collected in the area near the Bassam channel before, six and twenty months after its opening in September 1987. Observed effects are the decrease in the abundance and the modification of the benthic macrofauna composition. These effects appeared to be definitive, without recovery of the most abundant species Corbula trigona. Most differences noted in the population structure are due to the increase of the salinity and at a least degree to the modification of the nature of the sediment.
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El objeto del presente Trabajo Fin de Grado (TFG) es realizar un Plan de Marketing para el Hotel López de Haro de 5 estrellas, perteneciente a la cadena Ercilla y ubicado en Bilbao. Para ello, se ha analizado tanto el entorno interno como el externo, detectándose una serie de fortalezas entre las que destaca el excelente trato personal que ofrecen los empleados a sus huéspedes y que es un factor clave sobre el que cimentar su futuro. Asimismo, se han detectado debilidades, oportunidades y amenazas sobre las que hay que trabajar. Con ese diagnóstico y con una orientación al cliente se han definido objetivos de marketing alcanzables y que permitieran, mediante diferentes estrategias y acciones satisfacer las necesidades de la clientela. En este sentido, se han investigado también las tendencias del mercado y, teniendo en cuenta estas y la realidad del hotel, se ha aportado una visión externa que les permita mejorar el funcionamiento del hotel.
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The present paper deals with the variations of the dissolved oxygen content off Grand Bassam (11 miles east of Abidjan, Côte d'Ivoire), during nearly five years (March 1966 to September 1970). Although we find in general the low oxygen values near the bottom, the dissolved oxygen content is at its absolute minimum during the upwelling. There is a good correlation between the Secchi depth and the depth of the well ventilated layer. About 10% of surface irradiance is found at the layer where the dissolved oxygen content equals 80% of the oxygen content found at surface.
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En la actualidad, el éxito de los establecimientos hoteleros está influido por numerosos factores que hacen del hotel un negocio difícil de gestionar. Nos encontramos en un sector, el turístico, en el que la demanda aumenta año tras año en San Sebastián y el principal inconveniente es la competencia del sector. Una competencia feroz. Nos enfrentamos ante una estructura de empresa muy costosa y difícil de gestionar en la que el capital humano es el activo más importante. El valor añadido es una de las ventajas competitivas más destacadas de este negocio y la calidad de los servicios prestados es la clave del éxito. El objetivo del presente trabajo de fin de grado, se centra en analizar la situación por la que atraviesa el sector turístico en la capital guipuzcoana, y conocer y examinar la gestión diaria de un establecimiento hotelero para realizar una previsión fiable. Básicamente, se trata de estudiar la viabilidad de un nuevo hotel boutique en el casco histórico de San Sebastián.
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The effect of decreasing frost frequency on desert vegetation was documented in Grand Canyon by replication of historical photographs. Although views by numerous photographers of Grand Canyon have been examined, 400 Robert Brewster Stanton and Franklin A. Nims views taken in the winter of 1889-1890 provide the best information on recent plant distribution. In Grand Canyon, where grazing is limited by the rugged topography, vegetation dynamics are controlled by climate and by demographic processes such as seed productivity, recruitment, longevity and mortality. The replicated photographs show distribution and abundance of several species were limited by severe frost before 1889. Two of these, brittlebush (Encelia farinosa) and barrel cactus (Ferocactus cylindraceus), have clearly expanded their ranges up-canyon and have increased their densities at sites where they were present in 1890. In 1890, brittlebush was present in warm microhabitats that provided refugia from frost damage. Views showing desert vegetation in 1923 indicate that Encelia expanded rapidly to near its current distribution between 1890 and 1923, whereas the expansion of Ferocactus occurred more slowly. The higher frequency of frost was probably related to an anomalous increase in winter storms between 1878 (and possibly 1862) and 1891 in the southwestern United States.