184 TRAP-ROCKS OF TCHANDEER. 



at the head of the district of Karditch, where 

 the beds of shale are thrown up vertically, and 

 the serpentine is burst through by protruding 

 masses of amygdaloid. The shales at the point 

 of contact are of a deep red colour, and very 

 crumbling. The same occurs near Geordenna. 

 At Tchandeer there is a good section, showing 

 the disturbance of the limestone by the trap 

 which bursts up between the beds of the former, 

 and includes large masses of it. 



«, Amygdaloid, including beds of limestone (b) at Tchandeer. 



In the west of Lycia there are few traces of 

 such recent irruptions ; but near Capac, in the 

 Seven Capes, there are dikes of igneous rock, 

 which disturb the limestone, and convert it into 

 a white and semicrystalline marble. 



Reviewing the geological features of Lycia, the 

 following considerations occur to us respecting 

 their history in time. 



