Notes:
Local sandstone with red brick dressings. Kinahan, p. 236 links Ballyconnell sandstone, along with Latt Sandstone, to St Patrick's College, Cavan. However, there is no sandstone present in the Ballyconnell area; the town is surrounded by the Dartry Limestone Formation. It is likely that the source of the yellow-grey sandstone in this building was only the Latt quarry.References
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Kinahan, G. H. (1889). Economic Geology of Ireland: VIII. Williams & Norgate.
