EUROPE. 



6^ 



Gosselet, Prof. J. L'Etage eocene inferieur dans le Nord de la 

 France et en Belgique. [L. Eocene in Northern France and in 

 Belgium.] Bull. Soc. Geol. France^ 3 ser. t. ii. pp. 598-617 (6 figs, 

 in text). 



The correlation of the beds is thus tabulated (p. 616) : — 



Jf . part of Paris Basin, 

 Suessonian. 



D6pt. du Nord and Belgium. 

 Clay of Flanders. 



England. 



Sands of Bracheux, 1 

 lower part j 



Sands of Bracheux, 1 

 upper part J 



Plastic clay and Sois- 1 

 sonnais Lignites ... j 



Heersian sand & marls. Clay of Louvil. 1 

 " Tufeau " of Angres. Clay with flints? J 



r Clay of Clary. 1 



Sands of Ostricourt -I „ of Englefontaine > 



[ „ of Bourlon. J 



Clay of Orchies . , . 



Sands of Cuise Sands of Mons-en-P6vele. Clay of Roubaix 



Thanet Sands. 



LowerWoolwich 

 Sands. 



UpperWoolwich 



Sands. 

 Oldhaven Series. 

 London Clay. 



G. A. L. 



. Sur les calcaires deroniens du Nord de la France. [Devonian 



Limestones of N. France.] Bull. Soc. Geol. France, 3 ser. t. iii. 

 pp. 356-358. 

 Resume of the writer's work in filling up the lacunae in the Devo- 

 nian series, which it was thought existed on the northern side of the 

 Palaeczoic basin of Dinant or Avesnes, as compared with the develop- 

 ment of that series on its S. side. G. A. L. 



— . bondage a Marquette. 

 Geol. Nord, t. ii. p. 70. 



[Boring at Marquette.] Ann. Soc. 



Account of a boring reaching the tun at 62 metres. 



. Documents nouveaux sur Tallnre du Terrain houiller au sud 



du Bassin de Valenciennes. [Lie of the Coal Measures S. of the 



Valenciennes Basin,] Ann. Soc. Geol. Nord^ t. ii. pp. 113-121, 



one folding plate. 



Brings out the chief geological facts contained in two mining 



reports, one by M. Fusch on the Marly concession, and the other by 



M. Olry on that of Crespin. While accepting all the facts stated by these 



authors, the writer differs in the interpretation of some of them. Faults 



and reversals on a large scale render this district very complicated ; but by 



means of ideal and true sections the arrangement of the beds is rendered 



intelligible. [tSee Fusch and Olry, pp. 65, 87.] G. A. L. 



. Observations sur les sables d'Anvers. [The Antwerp Sands.] 



Ann. Soc. Geol Nord, t. ii. pp. 129-134. 

 The succession of these sands seen was as follows, in ascending order : — 

 Zones of 1, Panopea Menardi ; 2, Pectunculus jnlosus ; 3, Terehratula 

 grandis ; 4, Isocardia cor ; 5, Pecten pnsio ; 6, Fusus antiquus. 4 and 



f2 



