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WILLIAM T. M. FORBES 



steeply dipping strata of the Eocene series. At one place Num- 

 mulites lavigata (Lutetien period of the Eocene) was picked up, 

 but not in situ. 



Fig. 8. — Kara Burun and immediate vicinity. The trap is indicated by hori- 

 zontal lines, the granite by coarse cross-hatching. Gardens have been shown in 

 stipple, indicating the position of springs. 



There are also some smaller igneous outcrops in the neighbor- 

 hood of Medjidie, which do not seem to belong to the Getchi 

 Kalesi range, in particular a neck of very coarse porphyry some 

 five miles northeast of that town and on the other side of the river. 



