This region is situated
along the north-eastern edge of the Namurian outlier of the Lough Allen Basin.
The region can be divided into 2 distinct areas.
The first is the Belmore
/ Tullybrack area, north of Lough MacNean, with the limestone outcropping
roughly north-south from Belcoo to Lough Navar, and the second is the Cuilcagh
Mountain area, where the limestone outcrops in a roughly east-west line
from Swanlinbar to beyond Blacklion.
The caves in the Tullybrack
/ Knockmore upland area are mostly vertical pot systems which enter extensive
horizontal systems. Classic caves in the area include Pollaraftara,
Noons-Archand Reyfad Pot, ( at -179m the deepest cave system
in Ireland ). Some rising caves can be entered at resurgence level.
In the Cuilcagh Mountain
area, deep, choked shafts in loose, chert-rich, limestones typify the eastern
part of the limestone outcrop. Moving west, extensive active river systems
such as Tullyhona, Prods-Cascades and Marble Arch are
formed in pure carbonate mudbank-type limestones. In the western part of the
limestone outcrop there are many systems where active exploration continues
such as Pollnagossan, Ture Rising and Shannon Cave. |