The only evidence that these earthworks exist at all comes from a single aerial photograph, catalogue reference BDT 47, which reveals the faint geometry of banks that have long since sunk below the threshold of ordinary sight. There are no surface traces. A walker crossing this field today would have no reason to pause.

The earthworks were recorded as part of a 1994 archaeological survey covering Ballinrobe and the districts around Lough Mask and Lough Carra, compiled by D. Lavelle for the Lough Mask and Lough Carra Tourist Development Association. The survey entry is spare, noting little more than the landform and the aerial evidence, which leaves the question of date and function open. Earthen banks of this kind could belong to almost any period of Irish prehistory or early history; enclosures, field boundaries, and ceremonial monuments all leave broadly similar traces once centuries of ploughing, grazing, and drainage work have had their effect. The Ballinrobe and Lough Carra region is archaeologically dense, with the limestone landscape around Lough Mask particularly well studied, which makes the near-total disappearance of this site all the more striking.

For anyone curious enough to visit the general area, the land around Skealoghan is typical south Mayo pasture, gently rolling and largely unremarkable from ground level. The earthworks, such as they are, would require specialist equipment to locate precisely. What the site really illustrates is how much of the Irish archaeological record exists only in archive photographs and survey entries, rather than as anything a person could walk up to and read.