The site is a univallate rath, meaning a ringfort defined by a single enclosing bank rather than the multiple concentric rings found at more elaborate examples, and it sits on a level coastal strip where early medieval farmers once organised their lives inside a boundary that was as much a social statement as a defensive one. What survives today is fragmentary enough that the overall shape of the place is difficult to read from ground level, with dense overgrowth making any clear impression hard to come by.

Where the bank is best preserved, it stands 1.2 metres high and runs about 4 metres wide at its base, though much of the stone visible on its surface likely arrived there not as original construction material but as debris cleared from nearby fields over the centuries. A 14-metre stretch of the western bank was at some point removed entirely, and the confused scatter of earth and stones at the south-western edge is probably what remains of that demolition. The northern portion of the bank has been absorbed into the local field boundary system, as has a short stretch of walling at the south-east, a pattern common to Irish ringforts whose structural bones proved useful to later generations of farmers. At the centre of the interior, a probable house-site survives as a 7.25-metre length of east wall, now just a low stony bank about 40 centimetres high, with the rest of the structure reduced to an irregular scatter of stones. The site was recorded by J. Cuppage in the 1986 Dingle Peninsula archaeological survey, which catalogued the dense concentration of early monuments across the Corca Dhuibhne region.