On a gently sloping hillside in Ballyhussa, a single upright stone rises about one and a half metres from the ground, quietly occupying a south-easterly facing slope as it has done for thousands of years. It is not a large monument by any measure, but there is something quietly deliberate about it: the careful orientation running north-north-east to south-south-west, the rounded point tapering at the top, the sense that its position was chosen rather than accidental.

The stone is a monolith of Old Red Sandstone, a sedimentary rock common across County Waterford and much of Munster, formed from ancient river and desert deposits laid down roughly 400 million years ago. It measures roughly 90 centimetres wide and 40 centimetres deep at its base, and stands 1.6 metres tall. Standing stones of this kind are a widespread but still poorly understood feature of the Irish prehistoric landscape. They were erected, most likely, during the Bronze Age, though their precise purposes remain open to interpretation: territorial markers, ritual monuments, burial indicators, or some combination of functions that no longer maps neatly onto modern categories. The orientation of this particular example, aligned on a north-north-east to south-south-west axis, invites speculation about whether astronomical or seasonal considerations played any part in its placement, though nothing in the surviving record confirms this one way or the other.