The BGS Lexicon of Named Rock Units — Result Details

Ballyshannon Limestone Formation

Computer Code: BAL Preferred Map Code: BAL
Status Code: Full
Age range: Chadian Substage (CI) — Arundian Substage (CJ)
Lithological Description: Limestone, dark blue-grey, bioclastic, argillaceous packstones, interbedded with dark grey, silty shale; rarely with chert nodules in upper part; named members include sandstones.
Definition of Lower Boundary: Lowest member of the formation, the Gortnaree Sandstone Member, conformably succeeds the Termon River Limestone Formation.
Definition of Upper Boundary: Highest member of the formation, the Ederny Limestone Member, is overlain disconformably by the normal Bundoran Shale Formation or the sandstone basal member in the Kesh-Omagh area and southwest County Fermanagh.
Thickness: 120 - 450 metres.
Geographical Limits: Northwest Carboniferous basin of Ireland.
Parent Unit: Tyrone Group (TYRO)
Previous Name(s): Pettigo Limestone Group [Obsolete Name And Code: Use BAL] (PELG)
Lower Limestone (GLRB)
Lower Limestone (GLRB)
Alternative Name(s): none recorded or not applicable
Stratotypes:
Type Area  The area around Ballyshannon, County Sligo. In a road cutting, 1.6 km east of the town and south of Knader Lough, basal dolomitic conglomeratic limestones rest unconformably on 'Moine' quartzites. Centred on 10 km Grid Square C 18 36. 
Reference Section  Corn Quarry, 2.1 km south east of Ederny, County Fermanagh. This quarry and other abandoned sites on Corn Ridge expose completely the top 50 m of the formation including some new members. 
Reference(s):
Oswald, D H, 1955. The Carboniferous rocks between the Ox Mountains and Donegal Bay. Quarterly Journal of the Geological Society of London, Vol.111, Part 2, 167-186. 
Brunton, C H C, and Mason, T R. 1979. Palaeoenvironments and correlation of the Carboniferous rocks in west Fermanagh, Northern Ireland. Bulletin of the British Museum of Natural History (Geology), Vol. 32, 91-108. 
Simpson, I M, 1954. The Lower Carboniferous stratigraphy of the Omagh Syncline, Northern Ireland. Quarterly Journal of the Geological Society of London, Vol.110, 391-408. 
1:50K maps on which the lithostratigraphical unit is found, and map code used:
N32