Vol. 58.] THE FOSSILIFEROUS SILURIAN BEDS OF KERRY. 237 
neighbourhood of the thrust and traversed by a rude cleavage (see 
fig. 7, below). . 7 | i 
Fig. 6.—Section along the eastern side of the inlet. of Coosmore. 
S (6.1) 
[Horizontal scale: 1 inch=50 feet ; vertical scale exaggerated. | 
O.R.8,= Old Red Conglomerate. S (B 1)=Silurian gritty slates, 
D = Fault-débris. F =Faults. 
Fig. 7.—Section through the northern slope of Clogher Head. © 
N. 
EF E-ZZOH 
— SAA S& 
9) Sas’; RWW 
is i) YI NWN 
js YY Gf) NN WY 
OK by Wi if d)X~> a= RRO 
EE SS elas Saar 3 Wi ‘ 
4 F 
O B (1) 
{Horizontal scale: 3 inches=100 yards. | 
T=Thrust. O =Old Red Conglomerate. B (2)=Green ash. 
F= Fault. B (1)= Fossiliferous hard green B(3)=Asbky red sandstone. 
grits. 
We obtained the following fossils from these beds :— 
Lindstremia sp. | <Atrypa hemispherica, Sow. 
Heliolites sp. Orbiculoidea rugata, Sow. 
Worm-tracks. _ Whitfieldella sp. 
Orthis elegantula, Dalm. Encrinurus Stokesi, M‘Coy. 
Spirifer bijugosus, M‘Coy. | Lichas anglicus, Beyrich. 
Plectambonites transversalis, Wahl. Phacops caudatus, Brinn. 
Leptena rhomboidalis, Wilck. _ Proetus sp. 
Atrypa reticularis (Linn.). | Crinoidal ossicles. 
The foregoing list of fossils leads us to regard these beds as of Upper 
Wenlock age, and to correlate them with the Drom-Point Beds. 
