In stratigraphic order, its constituent formations are:
Dartry Limestone Formation
Traditionally known as the Upper Limestone, the Dartry Limestone is a significant landscape-forming rock unit dating from the Asbian substage. It is dark grey and argillaceous in nature and includes some fossils and chert nodules or beds. The type area is in the Benbulben Range and Dartry Mountains of County Sligo. Up to 350m thick, it is subdivided with several distinct ‘rock units’ or ‘members’ recognised. In stratigraphic order, these are:
Carn Limestone
Cloghany Limestone
Carrickmacsparrow Limestone
Cloghan Hill Limestone
Knockmore Limestone
In the Irish Republic, this rock sequence is known as the Bricklieve Limestone Formation.
Known previously as the lower part of the Middle or Calp Limestone and of the Upper Calp Shale, this 60-120m thickness of mudstones with fossil-rich grey limestones and thin calciturbidites and sandstones make up the formation. The outcrop runs from north of Monaghan towards Upper Lough Erne then north to Maguiresbridge. West of the lough, a broad outcrop runs north to the Derrygonnelly area. From beneath the Cliffs of Magho, the outcrop wraps around the south of Lough Melvin generally west to Glencar Lough. There are further outcrops north of Ederney and running NE-SW through Manorhamilton.
Variously known in the past as the Middle or Calp Sandstone, Upper Calp Sandstone and Clonelly Sandstone Group, about 200m thickness of brown to grey sandstones interbedded with mudstones and siltstones make up this formation. A thin band extends southwest and northeast from Scotstown in County Monaghan whilst a broader band is found east of Lough Macnean Lower, running north to Derrygonnelly. A narrow outcrop runs northeast-southwest through Manorhamilton. The most extensive area is around Lough Melvin west to Mullaghmore Head and including Inishmurray. A further band wraps south towards Sligo. There are other outcrops west of Ballyshannon, around Mountcharles from Lough Bradan Forest to the shores of Lower Lough Erne.
Known variously in the past as the Middle or Calp Limestone, or Lower and Middle Calp Shales, this 80-450m thickness of dark grey mudstones with layers of bioclastic limestone includes at its base, the Skea Sandstone Member. Its outcrop extends from northeast of Monaghan southwest to Upper Lough Erne, though is largely covered by more recent deposits. A band of these shales extends west of Enniskillen to north of Derrygonnelly. There are broken outcrops around the northern shore of Lower Lough Erne and from the west end of the lough to the coast at Bundoran and further outcrops around the northeast of Donegal Bay. There are more further west between Kinlough and Drumcliff whilst another band runs southwest from Manorhamilton. Occurrences of this rock further south in the Republic of Ireland are known as the Lisgorman Shale Formation.
Ballyshannon Limestone Formation
Formerly known as the Pettigo Limestone Group or the Lower Limestone, this 120-450m thickness of blue-grey limestones with interbeds of silty shale, includes the Gortnaree Sandstone Member at its base. It outcrops in the country between Clabby and Brookeborough and in a small area east of Aughnacloy. A further outcrop extends from north of Monaghan west then along the border from Rosslea to Upper Lough Erne and then through Enniskillen and the western edge of the lough as far as Church Hill. It also occurs in the Kesh and Ederney areas and in a broken curved outcrop towards Drumquin then northwest to Slieve Glass then west and southwest to Pettigoe and the north shore of Lower Lough Erne to Belleek. It is widespread east of Donegal Bay in the country around Ballintra and east of Donegal. There are further outcrops around Sligo Bay and southwest from Manorhamilton. In the Irish Republic, this rock sequence is known as the Oakport Limestone Formation.
Clogher Valley Formation
The formation which comprises peritidal limestones and shales is evident in the Castlecaulfield area and extends from Ballygawley through Clogher to the Fivemiletown area. The outcrop also extends southwest from the Tempo area to south of Lisbellaw and along the northeast edge of Enniskillen to the eastern shores of Lower Lough Erne.
Ballyness Formation
Formerly known by various names including the Lower Carboniferous Sandstone, Basal Clastics and Calciferous Sandstone, the formation comprises about 300m thickness of red sandstones and quartz conglomerates. Though much obscured by superficial deposits, its outcrop extends from the countryside north of Donamore southwestwards towards Clogher and in the area between Fivemiletown and Fintona. A further outcrop extends northwest from Lisbellaw to Ballycassidy and the eastern shores of Lower Lough Erne.
