A rath, as this type of ringfort is known, was the standard farmstead of Gaelic Ireland, typically dating from roughly the fifth to the twelfth century. Farmers enclosed their households and livestock within a raised earthen bank and a surrounding ditch, or fosse, choosing elevated ground wherever possible, even if that elevation amounted to no more than a gentle hummock above waterlogged fields. Here, that subtle topography still does its quiet work, lifting the circular enclosure just enough above the surrounding pasture to make its purpose legible.

The earthwork itself is a circle of approximately thirty-five metres in diameter, a typical scale for a single-family rath. Its construction is layered with some care: a main earthen bank rises around 1.8 metres on its outer face, a scarped edge reinforces the perimeter on the north-northwest to southeast arc, and a fosse roughly 0.8 metres deep and 2.2 metres wide runs all around the outside. Beyond that again sits a counterscarp bank, the smaller outer ridge that would have made the whole defensive arrangement still more formidable to anyone approaching from the fields. The survey record, compiled by Denis Power and uploaded in August 2011, notes that the banks and fosse are now heavily overgrown, with mature trees established on both earthworks, and that the interior is largely consumed by dense vegetation apart from the eastern third, which remains under rough pasture.

There is one small detail that brings the site's continued use into focus: a narrow gap in the western bank, most likely worn through by cattle rather than by any human intention, which have been accessing the interior as part of the surrounding farmland. This is pasture country, and the rath sits within it on working agricultural ground, so anyone visiting should come prepared for uneven, potentially wet terrain and expect to work around livestock. The heavy undergrowth across most of the interior means the earthworks themselves, viewed from the outside, give the clearest sense of the structure's original form, particularly the pronounced height difference between the inner and outer faces of the main bank on the southern and southeastern sides.