The Church historians of England.

Title varies.

Recueil des actes de Henri II : roi d'Angleterre et duc de Normandie, concernant les provinces françaises et les affaires de France /

Title-pages of Introduction, and of Atlas read: Recueil des actes de Henri II ... public sous la direction de M. H. d'Arbois du Jubainville par M. Léopold Delisle.

Le mystère de Robert le Diable /

Mode of access: Internet.

Coutumiers de Normandie:

Vol. 1 in 2 parts, each with separate title-page and pagination.

Eloges en vers latins des présidents et conseillers du parlement de Rouen, de 1499 à 1543,

Printed from an unpublished ms. entitled: Virorvm omnivm consvlarivm ab institvto Rothomagi senatv hactenvs ordine promotorvm libri qvatvor ...

Tableaux d'analyse chimique /

Mode of access: Internet.

The romance of history : England /

Vol. 2 imperfect: t.-p. wanting.

Miracle de Nostre Dame, de Robert le Dyable, filz du duc de Normendie, à qui il fu enjoint pour ses mefaiz aq'il féist le fol sans parler; et depuis ot Nosstre Seignor mercy de li, et espousa la fille de l'empereur.

"Note sur les divers imprimés relatifs à Robert-le-Diable": p. [xxxv]-xxxviii.

The dramatick works of Beaumont and Fletcher;

Cont. Fair maid of the inn. Cupid's revenge.--v. 10. Two noble kinsmen. Tragedy of Thierry and Theodorey. Woman-hater. Nice valour, or, the passionate madman. Honest man's fortune. Masque. Four plays, or moral representations, in one.

Lamp Post Motel

2424 E. Stadium (M-17) at Washtenaw (U.S. 23) Ann Arbor, Michigan NOrmandy 5-6123. The Lamp Post is a luxurious Motel of Colonial Design. Each of the 54 Rooms is furnished with Wall-To-Wall Carpeting, complementary TV, background music, bath, individually controlled message and morning wake-up system and Heated Pool. A Howard Johnson's Restaurant is adjoining. Located near University of Michigan Campus and Hospitals.

British Double Agents and Operation Fortitude: A New Perspective

On June 6th, 1944, Allied forces stormed the beaches of Normandy as a part of Operation Overlord, the Allied invasion of France. While they experienced pockets of stiff resistance, Allied troops sustained far fewer casualties than they had expected. The reason for this was due to Operation Fortitude, a deception mission that intended to fool Hitler about the time and location of the Allied invasion mission. The use of double agents by British Intelligence services was essential for the effective execution of Fortitude. The story of the double agents goes beyond their success during Fortitude. Double agents were initially recruited as German agents, but key agents immediately turned themselves in to British authorities upon reaching the nation. These agents decided to become involved with British Intelligence due to broader circumstances that were happening in Europe. The emergence of Fascist regimes disrupted the political landscape of Europe and led to widespread condemnation from political and social spheres. Their development as double agents became crucial to their effectiveness during Operation Fortitude. Their successful infiltration of German Intelligence allowed them to convince Hitler and German High Command that the main Allied invasion force would come at the Pas de Calais instead of Normandy. The result was that the Allies met an unprepared German defense force on D-Day and were able to advance past the beaches. The work of the double agents during Fortitude saved thousands of Allied lives and was vital to the success of Operation Overlord.

Fossil associations from the middle and upper Eocene strata of the Pamplona Basin and surrounding areas (Navarre, western Pyrenees)

Fossil associations from the middle and upper Eocene (Bartonian and Priabonian) sedimentary succession of the Pamplona Basin are described. This succession was accumulated in the western part of the South Pyrenean peripheral foreland basin and extends from deep-marine turbiditic (Ezkaba Sandstone Formation) to deltaic (Pamplona Marl, Ardanatz Sandstone and Ilundain Marl formations) and marginal marine deposits (Gendulain Formation). The micropalaeontological content is high. It is dominated by foraminifera, and common ostracods and other microfossils are also present. The fossil ichnoasssemblages include at least 23 ichnogenera and 28 ichnospecies indicative of Nereites, Cruziana, Glossifungites and ?Scoyenia-Mermia ichnofacies. Body macrofossils of 78 taxa corresponding to macroforaminifera, sponges, corals, bryozoans, brachiopods, annelids, molluscs, arthropods, echinoderms and vertebrates have been identified. Both the number of ichnotaxa and of species (e. g. bryozoans, molluscs and condrichthyans) may be considerably higher. Body fossil assemblages are comparable to those from the Eocene of the Nord Pyrenean area (Basque Coast), and also to those from the Eocene of the west-central and eastern part of South Pyrenean area (Aragon and Catalonia). At the European scale, the molluscs assemblages seem endemic from the Pyrenean area, although several Tethyan (Italy and Alps) and Northern elements (Paris basin and Normandy) have been recorded. Palaeontological data of studied sedimentary units fit well with the shallowing process that throughout the middle and late Eocene occurs in the area, according to the sedimentological and stratigraphical data.

Évolution pléistocène de la Seine fluviatile préservée en Baie de Seine

New high-resolution seismic data complemented with bedrock samples allowed us to propose a revised geological map of the Bay of Seine and to better define the control by the geological substrate on the morphogenesis and evolution of the Seine River during Pleistocene times. The new data confirm previous works. The Bay of Seine can be divided into two geological parts: a Mesozoic monocline domain occupying most of the bay and a syncline domain, mostly Tertiary, in the north, at the transition with the Central English Channel area. The highlighting of Eocene synsedimentary deformations, marked by sliding blocks in the syncline domain, is one of the most original inputs of this new study in the Bay of Seine that underlines the significant role of the substrate on the formation of the Seine paleo-valley. In the monocline domain, three terraces, pre-Saalian, Saalian and Weischelian in age respectively, constitute the infill of the paleovalley, preferentially incised into the middle to upper Jurassic marl-dominated formations, and bounded to the north by the seaward extension of the Oxfordian cuesta. The three terraces are preserved only along the northern bank of the paleovalley, evidencing a NE-to-SW migration of the successive valleys during the Pleistocene. We assume this displacement results from the tectonic tilt of the Paris Basin western margin. In the North, the paleo-Seine is incised into the axis of the tertiary syncline, and comprises three fill terraces that are assumed to have similar ages than those of the terraces. The fill terrace pattern is associated to the subsiding character of this northern domain of the Bay of Seine.

Prevalence and characterization of Salmonella spp. in three shellfish-harvesting areas in France

Shellfish farming is an important economic activity in the Brittany and Normandy regions. However, a part of the production sites corresponds to relatively sensitive areas where the presence of faecal microorganisms is a major concern for shellfish and constitutes a possible health risk. Indeed, shellfish bioaccumulates in their tissues pathogenic contaminants present in water and can cause food-borne diseases such as salmonellosis. During a two-year study, we evaluated the presence of faecal indicators, measured the prevalence of Salmonella spp., isolated and characterized Salmonella spp. from three French shellfish-harvesting areas (shellfish and sediment) and their watersheds (from river water samples).