EUROPE. 123 



* [Landslip at the Kahlenberg Slope along the Danube.] VerJi. 



h.-Tc. geol. lieichs. pp. 131-134 ; see also Woch. osterr. Ing. Ver. 



no. 9. 



Gives a detailed description of the occurrence, and classifies its 



causes under five heads, the first two of which, the pulpy nature of the 



beds and the deep-seated springs, are irremediable, whereas the. others 



could be neutralized by engineering. G. A. L. 



Wolf, H. Das Aufnahmsgebiet in Galizisch-Podoli.en im Jahre 1875. 



[District surveyed in Galician Podoiia in 1875.] Verh. h.-k. cjeoh 



Meichs. pp. 17G-183. 



Gives in a table the geological divisions recognized, compared with 



those made out by Alth in 1874 (see Geological Eecoed for 1874, 



p. 45) and by Stur in 1872. Admits 11 divisions. G. A. L. 



. lleisebericht aus Galizien. [Xotes of Travel in Galicia.] 



Verh. h.-Tc. cjeol. lieichs. pp. 318, 319. 

 Entirely geological. 



— '—. Die Bausteinsammlung dcs osterr. Ingenieur- und Archi- 

 tekten-Yereins. [Collection of Building-stones of the Austrian 

 Society of Engineers and Architects.] Woch, osterr. Ing. Ver, 

 no. 9. 



llefers chiefly to Austrian building-stones. 



Wurst ember ger, Arnold R. C. rebcr Lias Epsilon. [On the 



€ Lias.] Jahresh. Ver. Nat. Wilrtt. Jahrg. 32, pp. 193-233. 

 Describes the L. Lias of S. Germany, Switzerland, and E. Prance, 

 adding remarks on Ichthyosauri., with description of /. longipes, n. sp. 



Zezi, P. Cenno intorno ai lavori del Comitate geologico nel 1875. 



[Sketch of ^York of the Italian Geological Commission in 1875.] 



JBoU. B. Com. geol. Ital. vii. pj). 3-6. 



Mentions the progress of the map of the Monte Yiso district, scale 



1 : 50,000 ; that of the Messina and Eeggio (Calabria) districts, on 



same scale ; also one of the Monte Pisano, scale 1 : 80,000, and another 



of Massa Marittima district, &c. &c. E. B. T. 



. Osservazioni geologiche fatte nei dintomi di Fcrentino e di 



Prosinoue nella provincia di Horn a. [Geology of Prosiuone, &c.J 

 Boll. E. Com. gcol. Jtal. vii. pp. 360-388 ; 3 woodcuts. 

 The hills consist chiefly of Eocene limestone or Miocene (?) sand- 

 stone, the Pliocene being absent. In depressions among these lies the 

 Quaternary travertin. Several Quaternary volcanoes are noted; the 

 lavas all augitic ; some show cones or orators, some only peperino and 

 ashes, others lava-streams. E. B. T, 



Ziegler, Prof. M. Ueber das Yerhiiltniss der Topographic zur Geo- 

 logic. Text zur topographischcn Karte vom Engadin und Bernina. 



