696 resultados para 1619
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El Teatro Circo de Albacete constituye uno de los edificios emblemáticos del despertar de la ciudad hacia la modernidad decimonónica. El doble e interesante carácter de teatro y circo, originalmente se evidenciaba en la posibilidad de conversión del patio de butacas en pista. Generada una encendida polémica con su rehabilitación, este artículo pretende aportar unas opiniones más serenas y disciplinares a partir de la reflexión acerca de la historia del edificio y de la filosofía que ha animado la intervención.
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This layer is a georeferenced raster image of the historic paper map entitled: Carte de la province de Constantine, dressée au Dépôt général de la guerre ; gravé par J. Schwaerzle. It was published by Imp. de Kaeppelin et Cie. in 1844. Scale 1:400,000. Covers northeast Algeria and a portion of Tunisia. Map in French.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, cities and other human settlements, roads, camps, shoreline features, and more. Relief shown by hachures and spot heights.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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authore P. Duval Abbeviliense Regis Christianissimi geographo.
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[Gerardus Mercator].
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Title from ff. 1r and f. 2r.
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Planktonic foraminiferal test fragmentation in three cores along a depth transect from the western equatorial Pacific (ERDC-93P, 1619 m; RC17-177, 2600 m; V28-238, 3120 m [Thompson, 1976]) were examined for the last 500 kyr at sample intervals from 2.5 to 5 kyr to study the fluctuations of dissolution in the western equatorial Pacific. The age models were constructed by correlating the delta18O records with the SPECMAP stack [Imbrie et al., 1984]. Results showed that intermediate and deep waters experienced the same patterns of dissolution through climatic cycles. Fragmentation varied with a greater amplitude, and the carbonate ion concentration changed less, in the deep than in the intermediate water. Dissolution has significant variance distributions and coherencies with delta18O over the 100, 41, and 23 kyr periods of orbital variations; dissolution maxima lag ice volume minima by 6 to 20 kyr. The dissolution variability was consistent with recent geochemical models which seek to explain the reduction of atmospheric CO2 concentration at the last glacial maximum [Broecker, 1982; Boyle, 1988].
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"Primer año secundario."
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Includes index.
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Series title also at head of t.-p.
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This volume has been designated "sixième volume" in the Catalogue, for a collection known under the title of the repository, Cabinet du roi. The engravings were prepared between 1672 and 1689 by various engravers: Le Pautre, Le Clerc, Chauveau, Edelinck, Picart, Baudet, Silvestre, Simonneau and Chatillon. They were issued individually at the outset, collected, and in this instance issued in uniform format. The plates of the Labyrinthe, 15 x 8.5 cm., have been printed on 4 leaves of 9 and 1 leaf of 5.
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Engraved plan of Versailles and its surrounding park signed "Le Clerc;" key to the plan on facing leaf.
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The fountains, designed by Lebrun were placed at the path intersections of the labyrinth, which was destroyed in 1774 and replaced by the Bosquet de la Reine.