Ringed by a dense growth of hawthorn, blackthorn and hazel, and worn down by generations of farm stock, the site belongs to a category of monument once extraordinarily common across Ireland: the rath, or ringfort, a roughly circular enclosure defined by an earthen bank and ditch that served as a farmstead during the early medieval period, broadly from around the fifth to the twelfth century. Tens of thousands survive in various states of preservation, yet each one occupied a specific, considered position in its landscape, and this one is no exception.

The enclosure measures approximately 27 metres northwest to southeast and 25 metres northeast to southwest, a modest but legible circle on a low ridge above the Trimoge River, roughly 40 metres to the northeast. The earthen bank, which incorporates internal stone facing, stands to an external height of about 1.3 metres at its southeast arc. Outside it runs a fosse, the wide ditch that would once have reinforced the barrier effect of the bank, and beyond that a fragmentary counterscarp bank survives on the eastern arc. The fosse, a shallow depression for most of its circuit, shifts character on the downslope northeastern side, where it becomes something closer to a stony terrace as the ground falls away towards the river. Where the original entrance was is no longer clear; the most likely candidates are the northeast or east, where the interior slopes down towards lower sections of the inner bank. Inside, a slightly raised stony area near the northern bank lies obscured under vegetation, and a loose pile of large stones sits against the inner face of the southern sector, suggesting collapsed structural remains of some kind.

The position of the site, on a gentle ridge with open views along the river valley and across to the rising ground on the far bank, reflects the practical logic typical of ringfort placement: defensible enough, well-drained, with good sightlines. What survives today is fragmentary, eroded by livestock and softened by centuries of weather, but the underlying geometry of the enclosure remains readable in the field, particularly where the fosse is most pronounced on the southwestern to northwestern arc.