Vol. 58.! TH& FOSSILIFEROUS SILURIAN BEDS OF KERRY. 239 
forms the Minnaunmore Rock, and is here slightly nodular in 
arts. 
: The coarser ash (B 5) is very well exposed north of the Minnaun- 
more Rock, and many blocks of the red sandstone and fine ash (B 3) 
are strewn about over the tract of country farther north again, 
though the rock is not seen there 2a situ. South-east of the 
Minnaunmore Rock is a mass of the same banded rhyolite, dipping, 
however, east-south-eastward, which has been probably faulted into 
its present position. 
Fig. 9.— Croaghmarhin Hill (to the left), formed of Ludlow flags 
aul grits; the Minnaunmore Rock (to the right), formed of 
rhyolite. ; 
The mutual relations of the bands (B6), (B45), and (B4) are very 
weil seen in the little inlet opposite the rock called Carrignahogha, 
at Clogher Head. Here the rhyolite (B6) is seen overlying the 
coarse ash (B5), which in its turn overlies the greenstone (B 4). 
The peninsula to the south of the little inlet is chiefly composed of 
the rhyolite. 
B(7). Ashes with rhyolite-bands form the southern border of 
the little peninsula just referred to, aud occupy the coast as tar as 
the head of the bay north of Carrigard. Judging from observations 
in the field, (B7) would appear throughout to be clearly an ash. 
Sections, however, show that part of the matrix is crystalline, and 
it is probable that a considerable part of the apparent ash is a 
rhyolite containing many xenoliths. 
B(8). This band of sandy limestone, ashy in parts, forms the rock 
of Carrigard and the shores of the little bay at the mouth of which 
