LOCALITIES OF IRISH CARBONIFEROUS FOSSILS. 
45 
here, and affords some of the finest specimens of Siphonophyllia 
cylindrica. There are several whin dykes here, running in an 
east and west direction, cutting through the limestone rock. 
Killaghtee, in Donegal, is situated on the sea-shore, eleven miles 
west of Donegal, and one mile S.W. of the village of Dunkineely. 
This locality is in the lower shales and limestones, and the sec¬ 
tions are well exposed by the action of the water, and contain 
much fossils. 
Ivilleshandra, in Cavan, is a small town. It stands on yellow sand¬ 
stone, but over this lies limestone with shale, which is partially 
quarried, about two furlongs west of the church. This limestone 
contains a great variety of fossils. 
Killinamack, in Waterford, is three miles S.W. of Clonmel, near 
Knocklofty bridge. Calcareous slate occurs here at the road-side, 
which contains a profusion of fossils. 
Killingly or Ballea, in Cork, is five miles S.E. of Cork, and two 
miles N.W. of Carrigaline. The calcareous slate here contains 
only one group of slaty beds between the yellow or upper part 
of the sandstone and the overlying limestone. 
Killogunra, in Mayo, is two miles S.W. of Killalla. The lower 
shales and limestones occur here, and are fossiliferous. 
Killukin, in Roscommon, is about one mile S.W. of Carrick-on- 
Shannon. The rock is limestone, and very fossiliferous. 
Killybrone, in Mayo, is one mile N.W. of Killala. The fossilife¬ 
rous rock here is an oolitic limestone, nearly black, and appears 
covered by yellow sandstone. 
Killycloghy is in Fermanagh. It is about a mile and a half S.E. 
of Lisbellaw. A river flows down into the valley southwards, 
in which yellow sandstone and the accompanying shales and 
limestones are exposed, in which are found the usual Modiolse, 
NucuIeb, &c. of the lower shales. 
Killygrean Upper, in Monaghan, is about two miles N.E. of the 
little town of Emyvale, a locality of limestone, shale, and sand¬ 
stone, the two former having fossils. 
Killymeal, in Tyrone, is half a mile east of Dungannon. On ac¬ 
count of the vicinity to the coal district of Coal Island, the rock 
here is supposed to be the upper limestone, but there is no 
visible junction to verify this supposition. The quarries, which 
are extensive, afford a good variety of fossils, and there are some 
vertical cracks, which admit water from the surface, and which 
