The northeast face of the stone has split, and the upper portion, roughly half a metre tall, has broken away and now leans against the lower section like a discarded fragment, as though the monument is slowly returning itself to rubble. It has not fallen outright; it persists, just not quite as it once stood.

The stone itself is a conglomerate of sandstone and quartz, rising to about one metre in height, with a roughly rectangular cross-section measuring just over a metre wide at its broadest. It is aligned northwest to southeast, a orientation commonly observed in prehistoric standing stones across Ireland, though whether that alignment here carries astronomical, territorial, or ritual significance is not recorded. It sits on a slight break in a northeast-facing slope of undulating upland terrain, the surrounding land under pasture. The field contains numerous old river channels, traces of watercourses that have long since shifted or dried, suggesting the landscape around the stone has changed considerably over whatever span of time the stone has occupied it.