734 



ME. P, H. C. EEED ON THE LOWER PALEOZOIC [NoV. I 899, 



Kilfarrasy Strand, similar slates occur in the bend of the cliffs 

 and extend 



Pig. 10. — Cliff-section, Kilfarrasy Strand, on the 

 luest side of the road to the beach. 



westward to 

 the west side 

 of the road 

 down to the 

 Strand. Avol- 

 canicneck[96] 

 [802] pierces 

 them near the 

 Black Door ; 

 they are every- 

 where highly 

 cleaved and 

 much faulted 

 and folded. A 

 greenish felsite 

 [560] [801], 

 resting on, and 

 containing nu- 

 merous frag- 

 ments of them, 



extends for 50 yards west of the road (see fig. 10), and then 

 a block of limestones similar to those in Tramore Bay is found 

 faulted into it (see fig. 11), with many signs of crushing in the 



A = Black shales, finely fissile, and crushed at the junction. 

 B=: Intrusive felsite [801] with numerous lai'ge xenoliths of 



the shales. 

 0=Eotten breceiated rock at the junction. 



Pig» 11. — Cliff-section, Kilfarrasy Strand, 100 yards west of 

 the road to the beach. 







S 

 ( 



> 



l.-O- 



k^ 



^^^S^P^^ii-~=-" 





A= Intrusive greyish felsite [54]. 



E= Impure limestones (Tramore Limestone Series), with black shaly crush- 

 zones at the margins. 

 C=Intrusive greenish felsite [36] [40], with included strips of shale. 

 D = Pale greenish intrusive felsite [25] free from inclusions. 

 E=Intrusive vein of pale greyish felsite [67]. 



