ETJROPE. Ill 



Farm. Stocl-holm Forh. Bd. iii. pp. 219-226, plate (plan and sec- 

 tion to the scale of 1 : 200,000). 

 Gives a sketch of the situation and the geology of the mountain, calls 

 attention to its minerals, describes its rocks (quartzite, hyperite, and a 

 porphyritic rock). E. E. 



Soler, D, M. Las Minas de Oro de la Nava de Jadraque, en la pro- 

 vincia de Guadalajara. [The Gold Mines of la Nava de Jadraque, 

 in Guadalajara.] Hev. Min. t. ii. pp. 245. 



Stache, Dr. Guido. Gcologische Notizen iiber die Insel Pelagosa. 

 [Geology of the Island of Pelagosa.] Verh. Tc.-Tc. geol. Reiclis. pp. 

 123-127. 

 llefers particularly to the statements of M. Stossich. Regards Pela- 

 gosa as a part of the sunken sea- coast of the Adriatic Neogene main- 

 land which joined Dalraatia to Apulia. G. A. L. 



. Geologische Karte des oberen Yintschgau. [Note on the Geo- 

 logical Map of U. Yintschgau.] Verh. k.-k. geol. Reichs. p. 176. 



Aus dem Ortler Gebiet. [The Ortler District.] Verh. Tc.-Tc, 



geol. Reichs. pp. 314-317. 



Ueber die altcn andesitischen Eruptivgesteine des Ortlerge- 



bietes. [Ancient Andesite eruptive Rocks of the Ortler District.] 

 Verh. Tc.-Tc. geol. Reichs. pp. 346-348. 



Stefani, C. de. Geologia del Monte Pisano. Mem. R. Com. geoh 

 Ital. i. iii. part 1, pp. 47-169, plate (sections) and 4 woodcuts. 

 [8ee also Geological Record for 1874, p. 99, and for 1875, p. 99.] 



A detailed description of Mte. Pisano, S. of Lucca, and of the Pisa 

 district. The older schists often cited as Palaeozoic are here referred to 

 the Trias ; above these come grey limestones and shales (Infra-Lias). 

 Chapter 3 deals with the " calcaire ceroide " (L. Lias) and the red 

 limestone (upper part of L. Lias) ; among the fossils cited from L. Lias 

 the following are new : — Rissoina obliquecostata, Chemnitzia 2^seudotu- 

 mida, C. phasianelloideSj C. clava, C. Saviana, Neritopsis Meneghiniana^ 

 N. Passerinii (Men.), Straparollus ornattis (Men.), Sto7natia Meneghini 

 (Men.), Pleurotomaria Pisana, P. candliculata, MytUns disputabilis. 

 Limestone with chert is referred to the M. Lias ; variegated sliales, with 

 Posidonomya Bronnii as sole fossil, represent the U. Lias. Chap. 4 treats 

 of Tithonian and Neocomian beds. 5 of the " argille scagliose " (M. Cre- 

 taceous). 6. " Albereso" (U. Cretaceous). 7. " Macigno " (M. Eocene). 

 8. Pliocene. 9. Postpliocene. 10. Mentions the gain of land, removing 

 the coast-line from Pisa for a distance of several thousand metres, since 

 the time of the Romans ; the distribution of different river-sediments 

 is tracked along the coast. A disquisition on the orography and 

 elevation of the " metalliferous chain " and of the Apennines (pp. 132- 

 167) ends the memoir. E. 13. T. 



