The site never announced itself at ground level; the enclosing ditch is only around twenty centimetres deep at its most visible, and the external bank rises barely above the surrounding land. It is precisely the kind of place that generations of walkers could have crossed without registering anything more than a slight unevenness underfoot.

The enclosure was identified through an aerial photograph taken as part of the Bruff Survey, catalogued as Map 23, Bruff 120, AP 3719. Doody's 2008 description records an oval platform measuring roughly 33 metres on its north-south axis, sitting approximately 0.7 metres above the base of its enclosing ditch, which is around 2.5 metres wide. An external bank, about 3 metres wide and 0.2 metres high, runs around the outside. By the time this description was made, the site was already quite denuded, meaning eroded and reduced from its original form, with the enclosing elements surviving only on the southern, western, and north-western sides. The morphology, that is, the overall shape and arrangement of the earthwork, is consistent with Bronze Age construction, placing its likely origins somewhere in the period between roughly 2500 and 500 BC, though no excavation appears to have confirmed this.

Because so little of the monument projects above ground, a visit requires some patience and a reasonable eye for subtle landform. The site sits in ordinary agricultural land, so access would depend on landowner permission, as is standard for unexcavated earthworks of this kind in Ireland. The southern and western arcs of the ditch and bank are the portions most likely to reward careful observation, particularly in low winter or early morning light, when raking shadows can pick out very slight changes in ground level. A comparison with aerial imagery before visiting can help orientate what the eye is looking for, since the feature reads far more clearly from above than from within the field itself.