 | | Journal (article/letter/editorial) | | of Auvers is built on the right side of the River Oise, on the declivity of a high terrace composed of...little dry valley on the south. On the level of th e Oise there are some glauconiferous sands somewhat difficult...(Reprinted by permission from Bull. Soc. Geol, de France, srd series, uol, xxuiii, 1900, p. '27.) and...higher up, the succeeding formation, the Calcaire de St. Ouen, can be seen. SANNOIS. The visit to the...marls we found the Sables d'Argen/euil or Sables de lIfarines, but in the north part of Paris they are |  | | Journal (article/letter/editorial) | | Collaborateur Principal it la Ca rte Geologi qu e d e France ; with the assistance of MM. G. RAIIIOND, G. COURTY...and Chatham R ailway and the Northern Railway of France, special accommodat ion being reserved in each...covered with alluvium, from beneath which the Calcaire de Brie (the uppermost beds of the local Lower Oligocene)...up a position at a higher level, with the Ca!caire de Beauce (Upper Oligocene) above them, whilst talus...about the junction of the sands with the Catcaire de Brie, at an exposure in the Fontainebleau sands, |  | | Journal (article/letter/editorial) | | Nummulites planulatus also exist , a nd it is highl y de sirable t hat their relative position should be carefully...current idea s is suggested. In a discussion of the En glish occurre nces of N ummulites laeu igatas (Wrigley...this was a species to be looked for in the London Clay, where indeed it neve r had been found, despite...frequen t and exas pera ting, while much of th e de te rmina ble material had to be supported on blocks...displacement, stand vertically , After the London Clay , the azoic Lower Ba gshot Sands, 138 feet thick |
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