A cashel is a stone-walled ringfort, the drystone equivalent of the earthen raths found elsewhere in Ireland, and this one measures approximately 32 metres north to south and 28 metres east to west. What makes it quietly unusual is the way the land itself has absorbed it: the interior sits around two metres above the external ground level on the downslope side, giving the enclosed area an elevated, platform-like quality that was almost certainly deliberate, offering both drainage and a degree of natural defence.

The most legible remnant of the original structure survives in the south-west quadrant, where the cashel wall persists as a one-metre-wide drystone revetment, a retaining face of stacked stone holding the edge of the scarp in place. It does not rise above the level of the interior and its inner face has been lost entirely, suggesting centuries of collapse or robbing for building material elsewhere. Around the south-east arc, the wall is reduced to a low stony bank, and much of the remaining circuit is traceable only as a faint undulation in the ground. Two low stone uprights at the east-south-east, roughly 0.9 metres apart, may preserve the position of the original entrance, a detail recorded in J. Cuppage's 1986 archaeological survey of the Dingle Peninsula, Corca Dhuibhne.

The site rewards a careful eye rather than a casual glance. The elevated interior and the surviving revetment in the south-west are the clearest points of reference on the ground, and the probable entrance uprights at the east-south-east are easy to miss without knowing to look for them. The slope's south-east orientation means that the light falls across the low earthworks at an angle that can make the underlying structure more legible in the morning hours, when shadows define what the eye would otherwise flatten into grass.