Neither survives in any visible form today. The promontory is now covered by a fir plantation, and whatever relationship once existed between the boulder, the enclosure, and the dramatic coastal geography around them can only be guessed at from the outside.

The granite boulder was described by Redington in 1914 as standing approximately 1.5 metres high and roughly 0.85 metres in length and width. An erratic is a boulder transported far from its origin by glacial movement and deposited when the ice retreated, which explains why a large piece of white granite might sit prominently atop a coastal headland. The small enclosure to its east was also noted by Redington, suggesting the two features were recognised together as part of the same site, though the nature of that relationship was not recorded in detail. Neither feature has left any trace on the ground. Elsewhere on the same hill, a stone pair, a form of prehistoric monument consisting of two upright stones set in deliberate alignment, lies roughly 250 metres to the south-southwest, and a pre-bog wall runs along the southeastern slopes, pointing to a wider landscape of early human activity that predates the spread of blanket bog across this part of Connacht.

The site, such as it is, offers nothing to see in the conventional sense. What it does offer is a particular kind of historical layering: a place where a distinctive glacial boulder apparently attracted prehistoric attention, later human construction, and early twentieth-century documentation, before the plantation closed over everything.