It is, in fact, a prehistoric burial monument, and its survival, however faint, is partly down to an infrastructure project rather than any deliberate act of heritage protection. Ring-barrows are circular earthworks associated with burial, typically consisting of a low bank enclosing a central area; they are found across Ireland and Britain and generally date to the Bronze Age, though precise dating of individual examples is rarely straightforward without excavation.

This particular site came to light not through an archaeological survey but through aerial photographs taken on 3 November 1984, as part of work associated with the Bord Gáis Éireann Cork-to-Dublin gas pipeline. The photographs, filed under BGE No. 3224 and Site No. 022197, caught the faint cropmark signature of the monument from above. When the Archaeological Survey of Ireland visited in 2000, they recorded a near-circular earthwork measuring 7.40 metres north to south and 7.35 metres east to west, defined by a bank roughly 3.2 metres wide and no more than 0.2 metres high on the outside. The interior sits slightly lower than the surrounding ground, which suggests the bank material was scraped inward from that same interior, a construction method that helps explain the monument's squat, unassuming profile. A gap of 1.8 metres in the bank at the north-north-west to north-north-east indicates an original entrance or break. The site does not sit in isolation; two further ring-barrows lie within 160 metres, one just 15 metres to the east, and a possible ringfort sits approximately 150 metres to the north-east, hinting at a landscape that was once meaningfully organised around these features.

The site lies 118 metres north of the townland boundary with Shanaclogh, in what remains working agricultural land. There is no formal access or signage, and the earthwork itself is subtle enough that even knowing its location, a visitor might need to look carefully for the slight depression and encircling rise. A dry day with low, raking light, particularly in winter or early spring when vegetation is short, gives the best chance of reading the ground. The 2006 Google Earth orthoimage still shows a faint outline, which offers a useful reference before any visit. The bank measures are small, so expectations should be calibrated accordingly; the interest here lies less in spectacle than in the quiet fact of survival.