EUROPE. 66 



strata ; the deepest well is about 360 feet. Fossils from the various 

 beds sunk through are named. E. B. T. 



Fuchs, Th. Die Tertiaerbildungen von Stein in Krain. [The Tertiary 

 formations of Stein, Illyria.] Verh. k.-Jc. geol. Reichs. pp. 48, 49. 



Rocks and fossils from Stein show that the following beds are there 

 developed : — below, Sotzka beds (Aquitanian) ; above, two divisions of 

 the Mediterranean stage, the lower (Horn beds) being much more nearly 

 allied to the upper than to the Sotzka beds below. E. B. T. 



. Zur Bildung der Terra Rossa. [On Terra Bossa.'] Verh. 



Ic.-k. geol. Reiclis. pp. 194-196. 

 Supplementary to Prof. Neumayr's paper : notices its large develop- 

 ment in Greece, where it is derived from freshwater limestones. Hence 

 it is always due to Glohiyerina remains, and the climate of the country 

 has more to do with its formation than the nature of the limestone. 



E. B. T. 



. Sulla Relazione di un Yiaggio geologico in Italia. Boll. B. 



Com. geol. Ital. pp. 237-240. 

 (From the German,) In reply to Prof. Seguenza (see p. 97). 



Fuchs, Th., and Al. Bittner. Die Pliocaenbildungen von SjTakus und 



Lentini. [Syracuse Pliocene.] Sitz. h. Ah. Wiss. Wien, matli.- 



nat. CI. Abth. i. Bd. Ixxi. pp. 179-188 (with woodcut); also 



Boll. B. Com. geol. Ital. pp. 288-293. 



Describes the Pliocene of several localities near Syracuse ; it lies 



unconformably on the Leitha limestone. That of Lentini corresponds 



with the beds at Tarento, consisting above of (1) Bryozoa sandstone ; 



below (2) blue plastic marls ; below which are (3) Bryozoa sands with^ 



corals. Lists of fossils in these divisions are given. E. B. T. 



Fusch, — . [Report on the Marly Concession (S. of the Valenciennes 

 coal-field.)]. Privately printed. 



Garnier, Jules. [Iron near Brest.] Bev. Geol. t. xi. pp. 76, 77. 

 The ironstone deposits are found in Devonian rocks, and consist of 

 geodic iron -ore. 



. [Iron-ores of Brittany.] Bev. Geol. t. xii. pp. 91, 92. 



Describes a deposit of white ironstone (analysis given), locally 

 called *' blandin," and associated with pockets of haematite worked in 

 an horizon of Silurian schists running from Glenac (Morbihan) to 

 Rcnac (Ille-et-Vilaine). G. A. L. 



Garrigou, Dr. — . Sur les causes geologiques de I'aflfaissement du 

 tunnel de Sarrouilhes. [Geological causes of the falling in of the 

 Sarrouilhes Tunnel.] Bull. Soc. Hist. Nat. Toulousej t. viii. pp. 

 377-379. 



Course a St. Beat. [Excursion to St. Beat.] Bull. Sac. 



Hist. Nat. Toulouse, t. viii. p. 418. 

 Geological notes with special reference to the St. Beat marbles, which 

 1875. F 



