Luxembourg and Portions of Belgium, Germany, and France, 1705 (Image 4 of 4) (Raster Image)

This layer is a georeferenced raster image of the historic paper map entitled: Le Duché de Luxembourg divisé en Quartier Walon, et Allemand : dans chacun desquels sont diviséz, les Seigneuries, Prevostés et Comtés. Le Duché de Bouillon ; le Comté de Namur et le Pays entre Sambre et Meuse, Dedié au Roy par son tres-humble, tres-obeissant, tres-fidele sujet et serviteur Hubert Jaillot, Geographe du Roy. It was published by chez l'auteur, joignant les grands Augustins, aux deux Globes, avec privilége du roy in 1705. Scale [ca. 1:143,370]. Covers Luxembourg and portions of Belgium, Germany, and France. This layer is image 4 of 4 total images of the four sheet source map, representing the northwest portion of the map. 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, roads, cities and other human settlements, fortifications, territorial and administrative boundaries, ground cover, and more. Relief shown pictorially. 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.

Rotterdam, Netherlands, 1768 (Raster Image)

This layer is a georeferenced raster image of the historic paper map entitled: Nieuwe Platte Grond Vande Stad Rotterdam geleege aand Rivierea de Maase en de Rotte = Plan nouveau de la ville de Rotterdam située sur les Rivieres de la Meuse et de la Rotte, Henry de Leth, a l'enseigne du Pêcheur. It was published by J. Covens & Zoon in 1768. Scale [ca.1:3,923]. Covers Rotterdam, Netherlands. Map in Dutch and French. The image inside the map neatline is georeferenced to the surface of the earth and fit to the 'RD_New (Rijksdriehoekstelsel), GCS Amersfoort' 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 roads, drainage, built-up areas and selected buildings, fortification, ground cover, docks, wharves, canals, windmills, and more. Includes index. This layer is part of a selection of digitally scanned and georeferenced historic maps from The Harvard Map Collection as part of the Imaging the Urban Environment project. Maps selected for this project represent major urban areas and cities of the world, at various time periods. These maps typically portray both natural and manmade features at a large scale. The selection represents a range of regions, originators, ground condition dates, scales, and purposes.

The armies of the first French Republic and the rise of the marshals of Napoleon I ...

Preface signed: Charles F. Phipps.

History of the world war,

v.1. The attack on France. - v.2. The making of middle Europe - v.3. Verdun and the Somme. - v.4. America and Russia. - v.5. The victory of armistice.

Dictionnaire topographique de la France, comprenant les noms de lieu anciens et modernes, publié par ordre du ministre de l'instruction publique et sous la direction du comité des travaux historiques et des sociétés savantes.

Imprint varies.

The United States and the war : addresses /

Editorial note -- Introduction, by the editor -- Proceedings at the luncheon of th Pennsylvania Society: Address of Rear-Admiral R. E. Peary. Note from the Hon. Theodore Roosevelt [facsimile]. Address by the Hon. J. M. Beck. Verdun menu [facsimile] -- Proceedings at the luncheon of the Pilgrims in London: Address by Viscount Bryce. Address by the Hon. J. M. Beck -- An American advocate [editorial from "London daily telegraph"].

Vie des martyrs, 1914-1916.

A travers le territoire.--Histoire de Carré et de Lerondeau.--Mémorial de la vie des martyrs.--Mort de Mercier.--A Verdun.--Le sacrifice.--La troisième symphonie.--La grace.--Nuits en Artois.

The new book of martyrs, from the French of Georges Duhamel,

Translation of Vie des martyrs.

Sites et monuments ...

Introductory chapter of each volume signed: Onésime Reclus.

Catalogue général des manuscrits des bibliothèques publiques des départements.

No more published of this series. A new series, in octavo, was begun in 1886 under the direction of Ulysse Robert; still in progress (1924) (0412.358)

The story of the great war ...

Another issue in 8 vols. has title: The story of the great war, the complete historical records of events to date. Illustrated with drawings, maps and photographs by Francis J. Reynolds ... Allen L. Churchill ... Francis Trevelyan Miller ...

Mémoire à l'appui du projet d'un chemin à ornières de fer, à établir entre Anvers, Bruxelles, Liège et Verviers, destiné à former la 1er section de la nouvelle route d'Anvers à Cologne. Rédigé en exécution des ordres de M. le ministre de l'intérieur,

Half-title: Projet de route en fer d'Anvers à la Meuse et vers le Rhin.

Histoire écclésiastique de la province de Tréves.

Mode of access: Internet.

Revisiting the Late Jurassic-Early Cretaceous of the NW South Iberian Basin: new ages and sedimentary environments

The study of the Upper Jurassic-Lower Cretaceous deposits (Higueruelas, Villar del Arzobispo and Aldea de Cortés Formations) of the South Iberian Basin (NW Valencia, Spain) reveals new stratigraphic and sedimentological data, which have significant implications on the stratigraphic framework, depositional environments and age of these units. The Higueruelas Fm was deposited in a mid-inner carbonate platform where oncolitic bars migrated by the action of storms and where oncoid production progressively decreased towards the uppermost part of the unit. The overlying Villar del Arzobispo Fm has been traditionally interpreted as an inner platform-lagoon evolving into a tidal-flat. Here it is interpreted as an inner-carbonate platform affected by storms, where oolitic shoals protected a lagoon, which had siliciclastic inputs from the continent. The Aldea de Cortés Fm has been previously interpreted as a lagoon surrounded by tidal-flats and fluvial-deltaic plains. Here it is reinterpreted as a coastal wetland where siliciclastic muddy deposits interacted with shallow fresh to marine water bodies, aeolian dunes and continental siliciclastic inputs. The contact between the Higueruelas and Villar del Arzobispo Fms, classically defined as gradual, is also interpreted here as rapid. More importantly, the contact between the Villar del Arzobispo and Aldea de Cortés Fms, previously considered as unconformable, is here interpreted as gradual. The presence of Alveosepta in the Villar del Arzobispo Fm suggests that at least part of this unit is Kimmeridgian, unlike the previously assigned Late Tithonian-Middle Berriasian age. Consequently, the underlying Higueruelas Fm, previously considered Tithonian, should not be younger than Kimmeridgian. Accordingly, sedimentation of the Aldea de Cortés Fm, previously considered Valangian-Hauterivian, probably started during the Tithonian and it may be considered part of the regressive trend of the Late Jurassic-Early Cretaceous cycle. This is consistent with the dinosaur faunas, typically Jurassic, described in the Villar del Arzobispo and Aldea de Cortés Fms.

Incisión fluvial del río Darro durante el periodo 1890-2010 en el sector urbano de Granada (Alambra-Valparaíso, España) determinada a partir de fotografías históricas

En este trabajo se calcula la tasa media de incisión fluvial del río Darro (Granada, España) durante el periodo 1890-2010 en su tramo urbano (sector Alhambra-Valparaíso). Para ello se han utilizado fotografías históricas en las que aparece dicho río, a partir de las cuales se ha podido determinar la posición del cauce en el momento en el que se realizaron las fotografías. La comparación con los escenarios actuales de tales imágenes ha permitido determinar la diferencia de altura del cauce a través de medidas de cotas absolutas realizadas mediante teodolito. Esta metodología ha permitido estimar de modo cuantitativo un índice de encajamiento vertical medio del río de 1,05 cm/año para el periodo histórico considerado.