The pair are aligned along a northeast-southwest axis, a orientation seen repeatedly across prehistoric standing stone settings in the south of Ireland, and which some researchers associate with solar or lunar events. What makes this particular pair quietly compelling is the contrast between the two stones: one leans noticeably to the northwest, tilted by time or ground movement, while the other still stands upright at 1.6 metres. If the leaning stone were restored to vertical, it would reach only about 1.05 metres, making it considerably the shorter of the two.

The stones sit on the western bank of the Clashduff River, in a valley that opens southward toward Bantry Bay. The taller, northeastern stone measures 0.65 metres by 0.37 metres in section; the southwestern stone is slightly broader at 0.8 metres by 0.4 metres. The gap between them is 0.9 metres, and their combined length along the alignment is 2.35 metres. Standing stone pairs of this kind are a recognised monument type in Cork and Kerry, generally assigned to the Bronze Age, though precise dating is rarely possible without associated finds or excavation. They are sometimes interpreted as route markers, territorial indicators, or as having had some ceremonial function, but their exact purpose remains genuinely unresolved. The rough pasture and river setting here are typical of a landscape that has changed relatively little in its broad character, even if the original context of the stones themselves has long been lost.