32 
JOURNAL OF THE GEOLOGICAL SOCIETY" OF DUBLIN. 
series, and afford fossils in the limestones, the shales, and even 
here in red sandstone—a thing unusual. 
Bundoran, in Donegal, is a bathing village, three miles S.W. of 
Ballyshannon; the rock here is calcareous slate, with beds of im¬ 
pure limestone, the strata lie nearly level, and are very well 
exposed. The black shales and impure limestone beds contain 
a profusion of fossils. In one place in the bay some beds of the 
rock are covered with Orthis resupinata , studded so closely that 
they resemble a pavement of stones about two inches diameter. 
In the west side of the bay, near low-water mark, in black fine 
slates, some beautifully marked Pectens are got; and near the same 
place, where there are rude steps made in the precipice as a pas¬ 
sage to descend to the water, one of the upper beds of the cliff, 
about three feet thick, is composed almost wholly of a mass of 
Orthis crenistria. 
Bunowna, in Sligo, is at the east side of the river at Easky, about 
fifteen miles N.E. of Ballina. The rock is a dark, impure limestone, 
and is well exposed in the river near the village, and on the shore. 
Siphonophyllia cylindrica is very abundant, and the specimens 
very large. Large bunches of Lithodendrons occur on the shore. 
Burris, in the Queen’s County, is two miles N.E. of Maryborough. 
The rock is light gray limestone, which abounds with the fossils 
usually found in this rock. 
Caheratrim, in Galway, is three miles S.W. from Loughrea, on the 
north brow of the Derrybrian mountains. Slate occurs here at 
thejfoot of the hill, in a stream that runs northward, a few chains 
south of its junction with a larger stream running westwards. 
This slate is calcareous, and contains a profusion of the ordinary 
fossils found lowest in the series, as Leptagonia analogs Spirifer 
attenuata, Orthis crenistria , &c. &c. 
Calragh, in Armagh, is five miles N.W. of the town of Armagh. 
The rock is limestone, and dips N.W. about 10°. Indeed, the 
general dip of the rock for a few miles northward of Armagh is 
to the N.W. Products and Spirifera are found here. 
Cappaghmoyle, in Galway, lies four miles N.E. of Athenry. A 
light gray limestone occurs here, full of beautiful fossils, a thing 
unusual for miles in the limestone of the surrounding country. 
The rock has not been quarried, except a little used for fences; 
but the beds are bare at the only farmhouse on the townland, 
