EFEOPE. 103 



and green Eurite, &c., containing ores and limestone in its lower 

 parts. E. E. 



ToRNQTJiST, S. L. Om Siljanstraktens palaeozoiska formationsted. 

 [PalsBozoic formations in the neighbourhood of Lake Siljan, Dale- 

 carHa.] Ofver. K. S. Vet. Akad. Forhandl. no. 4. 



ToucAs, A. Note sur la geologic des environs de Toulon. [Geology 



of the neighbourhood of Toulon.] Bull. Soc. Geol. Prance, 3 ser. 



t. ii. pp. 457-403, 1 fig. 



Gives the relations existing between the Jurassic and Cretaceous 



deposits to the north of Toulon, a detailed section of the Caoume hill, 



and short lists of fossils. G. A. L. 



ToFLA, Franz. Die Congerienschichten an Eichkogel bei Modling. 

 [" Congeria-beds " at Eichkogel.] Verb. k.-k. geoL Reichs. 

 p. 383. 



TouENoufiR, E-. Note sur les coquilles des tnfe quatemaires de la 

 Celle, pres Moret (Seine-et-Mame). [Shells of the Quaternary 

 tuffs of the Celle, near Moret.] Bull. Soc. Gcol. France, 3 ser. 

 t. ii. pp. 443-452. 

 Gives a list of the species found. Of these, 21 are still living in the 

 district ; 5 are stiU living in France, but not in this district ; 3 are still 

 living in Europe, but not in France ; 4 (or perhaps 8) are extinct. The 

 age of these tufaceous deposits the writer considers to be that of 

 Elephas primigeniiis and lUiinoceros tichorliinus. G. A. L. 



Trautschold, — . Ueber die Naphtaquellen von Baku. [Naphtha- 

 springs of Baku.] Zeits. deutsch. geol. Gesell. Bd. xxvi. pp. 257- 

 274, pi. iv. 

 Describes part of the peninsula of Apscheron. A map (not geological) 

 is given, showing the distribution of the springs of inflammable gas, 

 the mud-volcanos, and the naphtha-springs. Four kinds of springs are " 

 recognized — those of naphtha, of gaseous hydrocarbons, of salt water, 

 and of fresh water. The naphtha generally occurs in sands and sand- 

 stones of younger Tertiary age. During the excavation of a reservoir 

 in the naphtha-bearing sand the author found shells of Cardiicm tngo- 

 noides and Mytilus polymorphus. A peculiarly limpid naphtha occurs 

 on the margin of a salt-lake near Ssurachany ; and a clay in this locality 

 has yielded the following fossils : — Monodacna caspiaj M. intermedia, 

 Didacna trigonoides, and Congeria rostriformis. The paper contains 

 statistics of the production of naphtha, and a description of the chemical 

 operations of the petroleum- works. F. W. R. 



Tribolet, M. F. de. Notes geologiques et paleontologiques sur le 

 Jura Neuchatelois. [Geological and Palseontological Notes on the 

 Neuchatelese Jura.] Pp. 32, plate (section and fossils). Pub- 

 lished with Bull. Soc. Sci. Nat. Neuchatel, t. x. 1 cahier. 

 1. On the presence of hydraulic limestones in the " Lower Astartian " 

 (pp. 5-8). 2. On a supposed bed of " Upper Corallian " at Joux- 

 dorrieres (pp. 9-14), with section and list of fossils. 3. On the fossilifcrous 



