They lean against one another in places, inclining from the vertical as though caught mid-collapse, and their arrangement stretches just under seven metres along a north-east to south-west axis. It is a quietly odd sight: prehistoric architecture succumbing to scrub, the scale modest enough that a casual walker might pass close without realising what they were looking at.

Stone rows of this kind are a feature of the prehistoric landscape across Munster, typically attributed to the Bronze Age, though their precise function remains genuinely uncertain. Theories range from ceremonial processional routes to astronomical alignments, and the Cork examples tend to be small, four-stone rows being among the shorter varieties recorded. At Piercetown, the four stones vary considerably in size. The north-easternmost is the smallest, standing roughly 1.1 metres if fully erect, while the south-westernmost is the tallest at around two metres. The two southerly stones are notably close together, almost touching, with the tallest leaning against its neighbour. The arrangement was catalogued by Seán Ó Nualláin in 1988, as part of his broader survey of Irish stone rows, and the measurements he recorded give a sense of monuments that are present but not dominant, embedded in a hillside rather than commanding it.

The gorse covering the site is dense enough to make close inspection difficult, and the stones' tilted, partially recumbent state means the row does not announce itself easily from a distance. Visitors approaching the south-east slope of Doolieve Hill should expect to work for the view, and late winter or early spring, before the gorse is in full growth, would give the clearest sight of the stones and the best sense of how the alignment sits within the slope.