It is not a dramatic landmark; the whole feature measures only around three metres north to south and four metres east to west. What makes it quietly interesting is precisely this compression of detail into a modest patch of ground, where a scarped edge, an external fosse, and a counter-scarp bank have survived together in a landscape that has otherwise moved on without much ceremony.

The site was recorded by Denis Power and uploaded to the archaeological record in November 2013. It sits within the north-east quadrant of a larger embanked enclosure, catalogued separately as LI023-058, and abuts the inner face of that enclosure's scarped edge at its north-north-east point. A barrow, in Irish archaeological terms, is a burial mound or funerary earthwork, typically dating from the Bronze Age or earlier, though the form persisted across several periods. This particular example is defined by a low scarped edge roughly a metre wide and between ten and fifteen centimetres high, with an external fosse, a shallow ditch running around the outside, measuring just over three and a half metres wide and about ten centimetres deep. Beyond that sits a counter-scarp bank, the low ridge thrown up on the outer side of the ditch, nearly seven metres wide with an external height of around thirty centimetres. These are subtle dimensions, the kind of earthwork that rewards careful looking rather than a glance from a field gate.

The site lies on private farmland, and there is no formal public access or visitor infrastructure associated with it. Anyone with a serious interest in finding it would do well to consult the National Monuments Service mapping portal, which carries the full record, before making any approach. The surrounding landscape is typical of lowland Limerick, and the enclosure within which the barrow sits provides its own layer of context; the relationship between the smaller funerary feature and the larger earthwork that contains it is itself worth considering. The features are low and easily missed in summer when vegetation is full, so earlier or later in the year, when the ground is barer, gives a better chance of reading the earthwork's form on the surface.