712 CM. MURGOCI 



which stream can be seen on the eroded hills in the Subcarpathian 

 depression. After this, there occurred in this region small disloca- 

 tions only, which changed the hydrographic lines, 1 and from this time 

 we have the rivers of Oltenia and the south Carpathian region as we 

 know them at present. This last phenomenon is very important for 

 the orography and hydrography of Oltenia; to this question of paleo- 

 geography I intend soon to return. 



1 E. de Martonne has studied this depression exhaustively, and has brought out 

 clearly the last movements of this region and of the whole of Oltenia (C. R. Ac. Paris, 

 1904, etc.)- 



