EUROPE* 97 



Beichs. pp. 238-241. Translated in Boll 11. Ctni, rjeoJ, Ital. t. vii. 



p. 490. 



The Naticella costata beds of S.E. Tyrol are wanting at Eecoaro ; and 



their place seems to be taken by the " Muschelkalk of Eecoaro," which 



in its turn is wanting in S.E. Tyrol. The other divisions of the latter 



district are present in the former. G. A. L. 



Mojsisovics, Dr. Edm. v. Yorlage der geoh gischen ^pccialkarte des 

 sUdostlichen Tyrols und der Provinz Belluno. [Notice of the Geo- 

 logical Map of S.E. Tyrol and the Province of Eelluno.] Vcrh. 

 7c.-l\ fjeol. lieichs. p. 347. 



An introductory note. 



Mortillet, G. de. La grotte de I'Herm. [Cave of I'Hcrtn.] Btdh 

 JSoc. Anthrop. Pai-is, 2 ser. t. xi. no. 6, p. 818. 



Superposition du Solutreen au Moustierien, a Thorigno 



(Mayenne). [The Solutrean above the Moustierian at Thorigno, 

 Mayenne.] ifat. Hist. Homme, 2 ser. t. vii. pp. 104-167. 



Mourlon, Michel. Sur les depots devoniens rapportes par Dumont 

 a I'etage quartzo-schisteux inferieur de son systeme eifelien, avec 

 quelques observations sUr les affleurements quartzo-schisteux de 

 Wiheries et de Montignics-sur-E,oc. [Devonian Deposits referred 

 by Dumont to the lower quartzo-schistose division of his Eifelian 

 system ; with Remarks on the quartzo-schistose Outcrops of Wi- 

 heries and Montignics-sur-Eoc] Bull. Ac. 11. Belg. ser. 2, t. xli. 

 pp. 323-345, plate (sections). 

 Discusses the views of various authors respecting the N. band of the 

 Din ant basin. Describes in detail sections in this region which confirm 

 Gosselet's results {Ann. Sd. Geol. 1873, t. iv.). Describes further sec- 

 tions near Wiheries and Montignies-sUr-Roc, with the object of sug- 

 gesting the probable L. Devonian age of rocks shown in them, before 

 looked upon as Silurian. Suggests that the presence of felspar in the 

 grit of these localities and of Ause is favourable to this view. Details 

 of sections form the bulk of the memoir. G. A. L. 



— . Sur les depots qui, aUx environs d'Anvers, separent les sables 



noirs miocenos des couches pliocenes scaldisicnnes. [Deposits near 



Antwerj) which separate the black Miocene sands from the Scal- 



disian Pliocene beds.] Bull. Ac. li. Bely. str. 2, t. xlii. pp. 760- 



790, coloured folding plate of sections. 



Considers as U. Miocene the black sands of Edeghem and Antwerp, 



which M. Vanden liroeck refers to the L. Pliocene. Gives details of 



many sections and lists of fossils. Many of these sections are only 



temporarily open. G. A. L. 



. Sur I'etage devonien des psammites du Condroz dans la vallce 



do la Meuse, cntre Lustin et Hermeton-sur-Meuse. [Tlio Condroz 

 sandstones in the Meuse Valley, between Lustin and Hermcton- 



1876. H 



