44 
JOURNAL OF THE GEOLOGICAL SOCIETY OF DUBLIN. 
Howth, in Dublin, is nine miles east of Dublin. A fine quarry of 
limestone occurs here, the rock being also well exposed on the 
shore, a little to the north of the village, and contains the usual 
fossils. 
Inver, in Donegal, is situated on the sea-coast, seven miles west 
of Donegal. This locality is all in black calcareous slate and 
shale, of the lower part of the limestone division. 
Kesh, in Fermanagh, is thirteen miles N.E. of Enniskillen, near the 
N.E. angle of Lough Erne. The development of the sandstone, 
to the north of this place, with its alternations of limestones 
and shales, is remarkable. 
Kilbride, in Mayo, is seven miles N.W. of Ballina, and two miles 
N.E. of the village of Ballycastle. The rock is limestone, with its 
shales, and this place shows it well, being surmounted by sand¬ 
stone. The place is rich in fossils. Atrypci gregaria occurs in 
masses; it has been only found here, at Ballinglen, which maybe 
said to be part of the same series of beds, and in the White river, 
near Draperstown, in Londonderry. 
Kilcar, in Cavan, is two miles S.W. of Belturbet. The rock here 
is limestone, and fossiliferous. 
Kilcommock, in Longford, is three miles N.W. of Ballymahon, a 
lower limestone locality, and fertile in fossils. 
Kilcummin, in Mayo, is on the sea-coast, five miles N.W. of Killala. 
This is a locality of alternations of limestone, shale, and yellow 
sandstone, and contains many varieties of the fossils usually found 
in this position. 
Kilcurry, in Louth, is four miles N.W. of Dundalk. In this loca¬ 
lity is found red sandstone, some black shales, and some lime¬ 
stone, as also yellow sandstone. The shales especially have fos¬ 
sils. 
Kildress, in Tyrone, is two miles west of Cookstown. In the river 
here is found a section of red shale, which contains the usual fos¬ 
sils of the black and gray calcareous shales, especially trilobites 
and corals, and this is the only locality where such fossils have 
been got in red shale. A little higher up, or westwards in the 
river, is found a red sandstone also, which contains abundance of 
casts of fossils. Atrypci canalis and Atrypa laticosta are got in 
this sandstone. 
Kilglass in Sligo, is eight miles north of Ballina, on the sea-shore, 
on the east side of Killalla Bay. The limestone is well exposed 
