What makes it worth attention is not its size alone, though at just over two metres tall it commands the hillside, but the way it has been shaped by time and position. The stone leans noticeably to the northwest, and that same face is far more heavily weathered than the others, a record of wind and rain accumulating over centuries, perhaps millennia, written into the rock itself.

The stone is trapezoidal at its base and irregular as it rises, with the southwest side climbing almost vertically while the opposite face tapers gradually up to a flat top. It measures roughly 2.05 metres in height, 1.2 metres wide, and 0.35 metres thick, oriented on a northeast to southwest axis. Beside it, just to the northwest, lie two thick stone slabs arranged at right angles to one another, each averaging around 1.15 metres in length and 0.55 metres thick. Their tops barely clear the ground surface, which may mean they have sunk with time, or that they were always intended to be low, perhaps as kerbing or markers associated with the main upright. Standing stones of this kind are a familiar feature of the Irish prehistoric landscape, raised during the Bronze Age in most cases, though their precise purposes remain debated; some appear to have had ceremonial or funerary functions, others may have served as waymarkers or territorial indicators. The low slabs beside this one add a further element that does not resolve neatly into any single interpretation, which is part of what makes the site quietly compelling. The survey of the Iveragh Peninsula compiled by A. O'Sullivan and J. Sheehan, published by Cork University Press in 1996, catalogued the stone as part of a broader effort to document the extraordinary density of prehistoric remains across South Kerry.