LOCALITIES OF IRISH CARBONIFEROUS FOSSILS. 
41 
Drumowen, in Tyrone, is two miles west of Drumquin. The same 
band of limestone, containing the same fossils, crosses this town- 
land, which is found in Drumscraw and Cavansallagh, the ad¬ 
joining townlands. 
Drumreagh Etra, in Tyrone, is four miles N.E. of Dungannon, on 
the Stewartstown road. The limestone here is supposed to be 
of the upper part, from its immediate proximity to the Coal 
Island coal district. 
Drumreask, in Fermanagh, on the west shore of Lough Erne, is 
one mile north of the village of Church-hill. It is a good loca¬ 
lity for black shale fossils. 
Drumscraw, in Tyrone, is one mile S.W. of Drumquin. The band 
of gray limestone which crosses this townland contains a great 
variety of the usual fossils of the limestone. 
Dundonagh, in Monaghan, is six miles north of Monaghan, and two 
miles S.E. of Emyvale. 
Dunkineely, in Donegal, is a smalltown, ten miles west of Donegal. 
This is a sandstone locality, and has the usual alternations of 
sandstone, limestone, and shale, found at the base of the Carbo¬ 
niferous limestone in the N.W. parts of Ireland. The rocks 
mostly dip S.E. about 10°. The locality abounds in fossils. 
Dunkit, in Kilkenny, is three miles north of the city of Water¬ 
ford. Large excavations have been made here in limestone; but 
the rock is not fertile in fossils. The calcareous slate which 
underlies it, and is exposed about the entrance to the quarry, 
yields fossils plentifully, and in a good state. 
Edenacrannon, in Tyrone, is four miles S.W. of Dungannon. The 
rock is the lower part of the limestone, with its interlaminated 
slate. 
Edenasop, in Tyrone, is five miles S.W. of Castlederg. 
Ederny, in Fermanagh, is two miles east of Kesh. 
Enagh, in Armagh, is seven miles west of Armagh; about a quarter 
of a mile S.E. of the village of Tynan. Teeth and spines of 
fishes are found in the light reddish-gray limestone, as at the 
Downs, near Armagh. 
Fallagloon, in Londonderry, is two miles west of Maghera. The 
mountain stream which forms the east boundary of this town- 
land exposes a good section of the Old Red Sandstone; and the 
black shales, about a mile up from the chapel, contains a profu- 
