N9-N10 Kilcullen to Waterford Road Scheme
N9-N10 Kilcullen to Waterford Road Scheme
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Constraints Report > North > 7 Geology and Hydrogeology > 7.2 Bedrock

7 Geology and Hydrogeology

7.2. Bedrock

The northern and central sections of the area of study are underlain by sedimentary Carboniferous limestone with Silurian slates and shales at the east (Kilcullen to Castledermot). Granites (igneous rocks) and surrounding metamorphic deposits (Leinster batholith) occurs along the eastern part of the study area. The central Castlecomer plateau area is composed of sedimentary Carboniferous sandstones, siltstones and shales.

Sedimentary rocks

The main geological formations occurring in the study area are described, starting with the oldest sequence, in Table 7.1.

Some of the Carboniferous limestone formations identified may be associated with Karst features (Ballyadams and Clogrenan Formations, designated Rck-3 on the geotechnical constraints mapping). The dolomitised Limestone rocks may also prove hard to excavate (the boundary of dolomitisation which runs from Carlow to Thomastown can be identified on the geological bedrock maps). The Quartzitic sandstone occurring in the Castlecomer plateau could also prove hard to excavate.

Granite Complex

A granite complex known as the Tullow granite extends in a broad zone to the east of Gorebridge-Carlow (Rck-5). The granites are igneous rocks and the resulting heat and deformation during their formation has created the surrounding metamorphic rocks. The Tullow granite is the largest granite pluton igneous body in the Leinster Batholith and is mostly of medium-grained texture but some coarse and fine veins cut the mass. Outcrops of granite were observed to the east and south-east of Carlow Town: Kernanstown, Chapelstown and Tinryland (Reference 8), see Rck-5 on the geotechnical constraints maps.

The granites can be very hard and difficult to excavate, although along the joints, the granite is often deeply weathered to sand with solid blocks in-between. This deep weathering can also result in a highly or completely decomposed granite structure. To the east and north-east of Carlow, geophysics surveys (Reference 8) indicated the presence of weathered granite in some locations ranging in thickness from 3.5m to 7.8m.

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