In Farrantooleen on the Dingle Peninsula, a standing stone that had occupied a level field at the foot of a low hill, looking out northward over Brandon Bay, fell at some point around the early 2000s and was subsequently removed. No ruin remains, no stump, no visible trace. The stone had stood roughly seven feet tall, or just over two metres, which puts it in the mid-range for Irish standing stones, those solitary upright megaliths erected across Ireland from the Neolithic through to the early medieval period, their precise purposes still debated but their presence in the landscape usually deliberate and considered.

The stone had been recorded on both the first and second editions of the Ordnance Survey maps of the area, which gives some sense of its continuity through the nineteenth and twentieth centuries. It was documented more formally in J. Cuppage's 1986 archaeological survey of the Corca Dhuibhne region, the Dingle Peninsula, a survey that catalogued a landscape extraordinarily dense with prehistoric and early Christian monuments. The townland of Farrantooleen sits within that same landscape, and the stone's position overlooking Brandon Bay would have placed it in sight of the water and the slopes of the Brandon massif, one of the most significant early Christian pilgrimage routes in Ireland. Whether the stone predates that Christian association or was once part of it is not known.

What makes this site worth noting is precisely that there is no site left to visit. The stone appears on historical maps, it has a survey number, and it has local memory attached to it, but the object itself no longer exists in the field. It is a reminder that the archaeological record is not fixed; monuments that survived for millennia can disappear quietly, within a human lifetime, and leave almost nothing behind.