Ringforts, which served as enclosed farmsteads during the early medieval period in Ireland, were typically circular enclosures defined by banks and ditches. Here, the enclosure is defined by a stone-faced earth-and-stone bank, and what makes this particular example quietly compelling is the construction method still visible in places: large limestone slabs laid edge to edge along the circumference, a technique that speaks to considerable local effort and an intimate knowledge of the crag beneath.

The enclosure measures roughly 33 metres north to south and 31 metres east to west, giving it a near-perfectly circular footprint. The bank survives best along the arc running from north-north-west to south-south-east, where its internal height reaches about a metre. Elsewhere, particularly along the western to north-north-western stretch, cattle movement has done considerable damage, softening and spreading what was once a more defined structure. The entrance, 2.3 metres wide, opens to the south-east and is flanked on either side by standing stones, a detail that would have given the original threshold a deliberately formal quality. Inside, the ground is littered with loose stone and punctuated by natural limestone outcrops, and the interior surface dips noticeably down towards the centre rather than lying flat. Running eastward from the enclosure, a linear earth-and-stone field bank, about 4.5 metres wide and 0.6 metres high, extends some 45 metres downslope, suggesting that the cashel was once part of a broader pattern of land organisation on this hillside. The site was compiled and recorded by Denis Power, with notes uploaded in August 2011.

The cashel sits in working pasture, so the landscape around it remains actively farmed. A haybarn and cattle crush have been erected immediately outside the enclosure to the west-north-west, which gives some indication of how closely the site is integrated into daily agricultural use. The south-eastern entrance is the clearest point of reference when approaching on foot, and the flanking stones on either side of the gap are among the more legible features remaining. The limestone crag on which the cashel stands means the footing can be uneven, and the interior scatter of loose stone requires some care. The section of bank running from north-north-west around to south-east offers the best sense of the original scale and facing method, and it is worth following that arc slowly to catch the places where the flat limestone slabs are still visible at the base of the bank.