Waterford City: Position & Structure

Latitude:        52º  16' North

Longitude        7º   7' West

The rocks which form the base of the City all belong to the Palaeozoic Group: principally Ordovician Shales, underlying some Sandstone on the North West, and crossed - East of the centre of the City - by an Alluvial bank running N.E./S.W.

At the cliffs on the North and South banks of the River Suir, above Rice Bridge, inter-stratification of sharply-folded Ordovician Slates and Sandstone conglomerates may be clearly observed.