112 Scientific Intelligence. 
lower half is very much expanded in the plane of cleavage, and has 
lost thereby its radiations. In figure 6 there is the same angle between 
cer rT 7 Tae ee 
North Wales, there are several anticlinal and synclinal axes of the 
stratification, yet, as shown in figure 10, only one axis of cleavage: 
The several anticlinal and synclinal axes, excepting the central one, 
influenc he ich fe 
have not influenced t 
