It is not signposted, not fenced off, and not particularly dramatic in appearance. But its proportions, an oval flat-topped form with a basal diameter of nine metres, a summit measuring roughly three metres east to west and just over two metres north to south, and a height of two and a half metres, suggest something deliberate rather than natural. Mounds of this kind in the Irish landscape are often the result of human activity across many centuries, sometimes serving as burial monuments, sometimes as markers of territory or assembly, and sometimes as remnants of later earthworks whose original purpose has been obscured by time and vegetation.

The site was recorded and compiled by archaeologist Geraldine Stout, with a later update by Christine Baker, and uploaded to the national record in October 2014. Beyond these details, the written record is sparse, which is itself telling. Many such earthen mounds in the Dublin coastal zone have never been formally excavated, leaving open questions about whether they date to the prehistoric period, the early medieval era, or somewhere in between. The flat-topped form is worth noting; in some cases this profile is associated with mottes, the raised earthen platforms used by Norman lords as bases for timber towers following the invasion of the late twelfth century, though a basal diameter of nine metres would be modest even by motte standards. Without excavation, the question of origin stays open.

The mound sits between a pedestrian path that runs to the north, giving access down to the beach, and a drainage ditch to the south, so it is effectively framed by the movement of both water and people. Reaching it means following the coastal path at Bremore, keeping an eye on the riverbank as it approaches the cliff edge. The vegetation that covers the mound tends to make it blend into the surrounding slope, so it rewards a slower pace and some attention to changes in ground level. Low winter light, when the grass is shorter and shadows sharpen the contours of the land, is generally the best condition for reading earthworks of this kind.