LOCALITIES OF IRISH CARBONIFEROUS FOSSILS. 
39 
The roaH here is cut through, and shows some sections of shale, 
which afford specimens of the fossils usually found in those lower 
beds. 
Curraghmore, in Fermanagh, is four miles west of Kesh, on the 
north shore of Lough Erne. 
Currens, in Kerry, is six miles S.E. of Tralee, on the Killarney 
road, and about three miles S.W. of Castle Island. This is a 
very fine locality for the fossils of the calcareous slate, and they 
are got in a state of good preservation. 
Cusackstown, in Meath, is six miles S.E. of Navan, and is in the 
lower part of the limestone. The rocks here contain the usual 
fossils. 
Deerpark, in Fermanagh, is two miles S.E. of Kesh; it is a loca¬ 
lity of the lower part of the limestone. 
Derrygonelly is in Fermanagh, is eleven miles N.W. from Ennis¬ 
killen, on the west side of Lough Erne. Casts of fossils are 
found here in a quarry, in a soft yellow sandstone. 
Derryloran, in Tyrone, is at the south end of the town of Cooks- 
town. Alternate beds of limestown and sandstone occur here. 
The sandstone is generally red; but a thick bed, near the church, 
is of a greenish-gray colour. The limestone, like all hereabouts, 
is fossiliferous, some of it takes a high polish. 
Derrynacapple, or Derrynacapplekeagh, in Fermanagh, is four 
miles N.E. of Kesh. This is a locality of limestone, shale and 
sandstone alternating, with the usual fossils. 
Desertmartin, in Londonderry, is a small town, four miles south 
of Maghera. The limestone quarries here are not very fossilife¬ 
rous. Fish palates have been got in them. 
Donaghrisk, in Tyrone, is two miles S.E. of Cookstown, and im¬ 
mediately west of the village of Tullyhog. Like Derryloran, 
limestone and sandstone are found here alternating. Some fos¬ 
sils are got in the limestone. 
Doneraile is in the county of Cork. The limestone in this locality 
is fossiliferous. 
Doonfeeny, in Mayo, is eight miles N.W. from Killalla, and two 
N.W. of Ballycastle. This is a locality of the arenaceous rocks. 
Black shales predominate; but there are also thin beds of im¬ 
pure limestone. Some beds of the shale are very fossiliferous. 
Doorin, in Donegal, is seven miles west of the town of Donegal, and 
