When turf is removed from a bogland slope in West Cork, it can expose walls that have not seen daylight in centuries, and that is precisely what happened at Cloontreem, on a west-facing hillside overlooking a stream valley running towards Eagle Hill. What emerged was a collapsed stone wall, roughly sixty centimetres high and a generous one-point-seven metres wide, running on a north-north-east to south-south-west alignment before disappearing back into an uncut turf bank nearly a metre deep. A handful of stones remain upright, hinting at the wall's original form, while the bog simply swallows the rest.

The wall itself is only part of a larger, quietly complex picture on this slope. Lower down, shallow peat, only about twenty centimetres deep in places, has allowed rough lines of stones to remain partially visible, the remnants of numerous disused field boundaries that once divided this ground into worked land. Bog preservation of this kind is not unusual in Ireland; the waterlogged, oxygen-poor conditions that make peat such good fuel also happen to be excellent at protecting organic and structural remains beneath the surface. Alongside one of these lower boundaries, on its eastern side, sits a small circular enclosure just four metres in diameter, the kind of modest feature that might have served any number of agricultural or domestic purposes. Forty metres further east sits a cairn of small boulders, measuring roughly three-point-seven metres in both directions, with its western edge notably well defined. Cairns like this can mark burials, boundaries, or simply the cleared stones of former cultivation, and without excavation this one keeps its purpose to itself.