The earthen bank enclosing it rises only about 0.3 metres on its interior face and 0.8 metres on the outside, low enough to be easily missed, and the shallow ditch that once ran around it has been partially filled in or redirected for agricultural use over the centuries. What remains is a rath, the Irish term for a ringfort, a type of enclosed farmstead built throughout Ireland during the early medieval period, roughly between 500 and 1000 AD. Thousands survive across the country in varying states of preservation, and this one in Co. Limerick sits quietly in level pasture, its circular outline measuring 37 metres in diameter, still legible in the landscape if you know how to read it.

The details recorded by surveyor Denis Power give a clear picture of a site that has been quietly worked against by farming practice over time. On the south-west to west-northwest arc, the bank has been levelled and the external fosse, the encircling ditch that originally measured 1.6 metres wide and 0.2 metres deep, has been filled in entirely. On the north to west-northwest section, that same fosse has been re-cut and repurposed as a field drain, which is a common fate for such features; a ready-made channel is a practical thing, and its original function as a boundary marker becomes secondary. The interior of the enclosure is grassed over and level, as one would expect of a site that has been incorporated into working farmland, though the perimeter and the surviving sections of the enclosing bank are obscured in places by overgrowth.

The site sits in ordinary pasture, which means access depends on the landowner's permission, as is standard with most ringforts in private fields across Ireland. There are no visitor facilities and no formal path to it. The best time to look for earthworks like this is in late autumn or winter, when low-angle light throws subtle ground features into relief and vegetation has died back enough to reveal the overgrown bank and the line of the fosse. If you do get close, look along the perimeter rather than into the interior; it is at the edges, where the bank meets the old ditch line, that the original shape of the enclosure becomes most apparent. The south-western section, where the bank has been levelled, will show the least, while the northern arc, reshaped as a drain, offers an inadvertent record of where the fosse once ran.