This one does not. Sitting a short distance upslope from a neighbouring recorded site in the townland of Feaghmaan, this small ringfort went unregistered on the maps entirely, which means it belongs to that quiet category of places that exist in the landscape without any official cartographic acknowledgement.

A rath, as the site type is also known, is a roughly circular enclosure defined by an earthen bank, used as a farmstead during the early medieval period, roughly between the fifth and twelfth centuries. This particular example is univallate, meaning it has a single enclosing bank rather than the double or triple rings sometimes seen at higher-status sites. The bank here is composed of earth and stone and is revetted along its inner face with slabs set on edge, a detail that suggests some care in the original construction even if the overall state of preservation is now poor. The enclosure measures about 16 metres north to south and nearly 20 metres east to west. The bank itself stands only half a metre high on the interior and under a metre on the exterior, and a modern field boundary cuts across the north-western sector, further disturbing what remains. The entrance was positioned to the north-east, where an arrangement of upright slabs still defines its northern side; the southern side of the opening has eroded away. Inside, centrally placed within the enclosure, are the remains of a subrectangular hut. Its stony bank survives to about 0.6 metres, and its sunken floor area measures roughly 4.2 metres by 1.5 metres, a very narrow space that points to a simple, functional structure rather than anything elaborate.

The combination of the absent map marking, the damaged bank, the bisecting field boundary, and the modest dimensions all make this a site that rewards patience rather than spectacle. It is the kind of place where the archaeology is legible mainly to someone already looking for it, and where the upright entrance slabs still holding their position after more than a thousand years are quietly more interesting than the surrounding erosion might suggest.