What appears at a distance to be a tidily tree-ringed field boundary is, in fact, a prehistoric stepped barrow, a type of burial mound distinguished by its layered, terraced profile rather than a simple earthen dome. The stepped arrangement here is created by a sequence of features working outward from the centre: a slightly domed interior, then a scarp, then a level berm, and finally the remains of a low outer earthen bank. That combination of elements, carefully graduated from the inside out, gives the monument its classification and sets it apart from more familiar, plainer mound types.

The barrow sits at roughly 343 feet above sea level, on the crest of a gentle rise that opens up broad views across the landscape to the south-west, west, and north-west. It was already being recorded by cartographers in the nineteenth century: the 1840 edition of the Ordnance Survey six-inch map depicts a raised circular area enclosed by a wide berm, and a later Cassini edition of the same map shows an OS trigonometric station, used for land surveying, standing on the northern side of the enclosure. The Archaeological Survey of Ireland carried out a formal survey of the monument in 1999. Their measurements place the raised area at approximately 33 metres east to west and 31 metres north to south. Entrance gaps were recorded on the eastern side, one five metres wide through the outer bank, another two metres wide further in, suggesting deliberate, structured access points rather than later damage or erosion. The berm between the inner and outer elements is level across much of the northern and eastern arc, while a steep natural slope drops away from the monument's outer edge on the south-western and western sides.

The monument sits in working pasture, so access would depend on land ownership and the usual courtesies of the Irish countryside. It is most legible from above: aerial orthophotos taken between 2011 and 2013, and Google Earth imagery from November 2018, both show the enclosure clearly as a circular, tree-planted feature. On the ground, visitors should look for the graduated earthworks, the subtle step from berm to inner rise, and the eastern entrance gaps, which remain the clearest physical indicators of how this structure was originally organised. The trees that now ring the site, while not original, help to mark its outline against the surrounding fields.