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dislocated and folded, following the core 

 of the two chief anticlines. (Fig. 4.) 



Some faults at Bujoreni-Fedelesoaia 

 bring the upper formations (Sarmatian) 

 in contact with the banded salt forma- 

 tion. In the southern region, at Ocnele 

 Mari-Govora, this horizon is constituted 

 almost exclusively of sand with shingle 

 and small banks of sandstone or con- 

 glomerates; the deposits present here 

 the character of a delta with violently 

 rushing arms. 



A very interesting point of this hori- 

 zon is at Casa Arendasului (Govora), 

 where we find an intercalation of marls 

 and more or less dissolved gypsum beds 

 between the uniform sand and shingle 

 strata. This horizon occurs in the mid- 

 dle of an eroded anticline, and has often 

 a lenticular form; it is limited here and 

 there by faults. Northward from 

 Govora Spa it touches and passes into 

 the banded facies; at Aninoasa, south 

 of Slatiora, it reappears with the delta 

 or torrential facies. 



In the ravines of Ocnele Mari quan- 

 tities of fossil debris may be seen, and 

 I have found very many small Num- 

 mulites and Orbitoides, all somewhat 

 eroded. 



Nummulites was collected also from 

 a conglomerate bank north of Govora 

 Spa, also in secondary beds. In the 

 ravines below Titireciu I found in the 

 same torrential strata fossil debris in 

 quantity, where Cerithium plicatum 

 Brug., Cerithium lignitarum Eichw., and 

 Corbula sp., could be determined. 



