56 
JOURNAL OF THE GEOLOGICAL SOCIETY OF DUBLIN. 
pears to be wanting. In the Termon quarry the beds of gray 
limestone are seen resting on yellow sandstone directly. These 
lowest beds of limestone contain a profusion of Orttiis papilliona- 
cea and Orthis crenistria , with but few other fossils. 
Tinnekill, in the Queen’s County, is three miles N.E. of Mountmel- 
lick, on the Grand Canal banks. This is a fossiliferous limestone 
locality. 
Tinnycahill, in Donegal, is two miles east of the town of Donegal, 
on the south side of the Londonderry road. The rock here is 
composed of limestone beds, with black shale interstratified. The 
limestone beds contain a variety of the fossils usually found in 
the lower divisions of the carboniferous limestone, as Orthis cre¬ 
nistria , Leptagonia analog a, &c. 
Tirlicken, in Longford, is three miles N. W. of Ballymahon, on the 
banks of the Royal Canal. The limestone here is fossiliferous, 
and yields good specimens of Nautilus, Temnocheilus, &c. &c. 
Toberory, in Roscommon, is two miles N. W. of the village of Tulsk 
on the French parkroad. The limestone here is oolitic, and con¬ 
tains a good variety of fossils. 
Tonyelida, in Monaghan, is three miles north of Carrickmacross, 
on the mail-coach road-side. Good specimens of Producta hemi¬ 
spherical and other fossils, are got here in the limestone. 
Tonyshandenny, in Monaghan, is two miles N.E. of Emyvale. 
This locality is on the lower part of the limestone, and yields 
fossils. 
Tornaroan, in Antrim, is on the sea-shore, one mile and a half east 
of Ballycastle. There are two beds of limestone here, under 
high-water mark, which dip south 8°, and contain fossils. The 
coal district of Ballycastle lies immediately over those beds, 
which, if that be millstone grit, would put them in the position 
of the upper part of the limestone; but they are indeed very 
unlike the appearance of this rock in other localities in Ireland. 
From the description given of the Scotch coal rocks about Bur- 
diehouse, they appear to be almost identical with the Ballycastle 
coal district, and the fossils, both shells and fish remains, got 
lately in the Scotch coal rock, are the same as those found in the 
lower shales in the Irish carboniferous rocks, as at Cultra, Dra- 
perstown, Drumlish, Kesh, &c. 
Tuberelathan.— See Cregganore. 
