42 
JOURNAL OF THE GEOLOGICAL SOCIETY OF DUBLIN. 
sion of the usual fossils of that division of these lower beds. 
Axinus nuculoides is got in whole masses; Modiola Macadami , 
and Modiola subparallela , abundant; seven species of Cytheras 
have been got, and scales of Holoptychius Portlocldi. A band of 
gray shale crosses the Moyola from this to the White river; this 
band is supposed to have the Old Red Sandstone under and 
over it. See Moyheeland. 
Farmacaffly, or Redbarn, in Armagh, is one mile S.W. of Armagh, 
Fish remains are got in the limestone here,—palates, teeth, and 
spines. 
Fasglassagh, in Tyrone, is four miles N.E. of Ballygawley. The 
lower black shales abound here, and contain the usual fossils. 
Fellow’s-hall, in Armagh, is seven miles west of Armagh— a lime¬ 
stone locality, and fossiliferous. 
Finner, in Donegal, is three miles S.W. of Ballyshannon, on the 
south side of the mouth of the river Erne. The rocks are so 
well exposed by the action of the waves that it is an excellent 
locality for the fossils of this part of the series. 
Flemingstown, in Meath, is six miles west of Balbriggan, and one 
mileN.W. of the village of Naul. About the chapel of Clonalvy 
the limestone is light gray, and the fossils come out well. 
Fort-william, in Cork, is one mile and a half S.W. of Doneraile, on 
the Mallow road. A good limestone locality for fossils. 
Glenbane.— See Lackagh. 
Granard, in Longford, is a small town, situated on the lower shales 
and sandstones of the carboniferous rocks. Numerous fossils 
occur here. 
Grangemore, in Roscommon, is three miles S.W. of Boyle, and two 
north of Frenchpark; an extensive field of limestone spreads 
over this part of the country, but does not contain a great va¬ 
riety of fossils. Orthis filiaria is common. 
Greaghs, in Donegal, is three miles S.E. of the town of Donegal, 
and half a mile east of the village of Laghy. The fossils of the 
lower black shales are abundant here. 
Gubbaroe, in Fermanagh, is two miles S.W. of Kesh, on the east 
shore of Lough Erne. This is a good locality for fossils. 
Gurteenroe, in Cork, is two miles north of Bantry. The rock here 
is calcareous slate. No good excavation is exposed, but hum¬ 
mocks of slate on the road side afford crinoid stems and fenestellge. 
