86 QEOLOGfT. 



Neumatr, Dr. M. Ueber den oberen Jura des Bas-Bugey (Siid- 

 Frankreich). [Upper Jura of Bas-Bugey (South France).] Verb, 

 k.-k. geol. Eeichs. pp. 37-40. 



Discusses some of the questions relating to the divisions of the Upper 

 Jura, as illustrated by a memoir by M. Falsan on this formation at 

 Bas-Bugey (BuU. Soc. Geol. France, 3 ser. i. p. 170). H. A. N. 



NoTH, Julius. Kleinere Mittheilungen. (1) Untersuchung auf 

 Braunkohle bei Kapi, W., bei Eperjes im Sarosen Comitate Un- 

 garns. (2) Kalkstein von Swiatkowa in der Herrschaft Miskowa 

 bei Zmigrod in Galizien mit Drusen, welche Bergol und Yerdun- 

 stungsriickstande enthalten. (3) Graphit mit Schwefelkies und 

 Brauneisenstein bei Dobschau, Gomoser Comitat, Ungarn. [Geo- 

 logical notes. (1) Investigation of the Brown Coal of Kapi, Hun- 

 gary. (2) Limestone of Swiatkowa in Galicia, with druses con- 

 taining petroleum and evaporation-residues. (3) Graphite, with 

 pyrites and brown iron-ore, near Dobschau, Hungary]. Yerh. 

 k.-k. geol. Eeichs. pp. 244-246. 



Olszewski, St. Poglad na geologija a w szczegolnosci na forma- 

 cyje mioceniczna wschodniej czesci Podola galicyjskiego." [Sketch 

 of the Geology, and especially of the Miocene formation, of Eastern 

 Podolia.] Akademija umiejetnosci w Krakowie [Ac. Sci. Cracow], 

 pp. 212-252. 

 ' Omalius d'Halloy, J. B. J. d'. Note sur le terrain devonien. Bull. 

 Ac. roy. Belg. 2 ser. t. xxxvii. pp. 191-196. 



Observations on Prof. Gosselet's paper on the Devonian rocks of the 

 country between the Sambre and the Meuse (see p. 68). 



Oetlieb, J. Falaise souterraine de la craie entre Eoubaix et Tour- 

 coing. [Underground Chalk-cliff between Roubaix and Tour- 

 coing.] Ann. Geol. Nord, 1870-74, pp. 4, 5. 



Note of an underground cliff 41 metres high, proved by borings 

 between these two places. 



. Forages a Croix et a Roubaix. [Borings at Croix and Rou- 

 baix.] Aun. Soc. Geol. Nord, 1870-74, pp. 14, 15. 



A section from the first place is given, 82*75 metres in depth, 

 through the foUowihg beds, in descending order : Quaternary, Tertiary 

 (Lower Landenian), White Chalk, Sandy Chalk, somewhat brecciated 

 Chalk, Chalk M arl, "Tourtia, Carboniferous Limestone. The Roubaix 

 boring is mentioned for comparison only. G. A. L. 



. Considerations generales sur les terrains tertiaires inferieurs 



du bassin flamand. [Lower Tertiaries of the Flemish basin.] 

 Ann. Soc. Geol. Word, 1870-74, pp. 23-27. 

 The divisions recognized by the author are as follows, in ascending 

 order : — Supercretaceous or Pretertiary Epoch, Epoch of the Clay of 

 Flanders, Epoch of the Cassel Sands ; Upper Eocene of Paris Basin 

 wanting. By this arrangement the physical causes of deposition are 

 shown. G. A. L. 



