In a marshy corner of a tillage field on a WSW-facing slope in Ballymot, County Cork, there once lay a spread of heat-shattered stones and charcoal-enriched soil roughly twenty metres across. No visible trace of it remains today, yet the spot is recorded as a burnt mound, a class of prehistoric site found in great numbers across Ireland and Britain.

Burnt mounds are the accumulated debris of a repeatedly used cooking or heating process. The typical method involved heating stones in a fire, dropping them into a water-filled trough to bring it to the boil, and then discarding the cracked, spent stones to one side. Over time these discarded stones built up into a mound, usually crescentic in shape and almost always found beside a water source, which explains why so many, including this one, occupy low-lying or marshy ground. They date most commonly to the Bronze Age. At Ballymot, the marshy field setting fits this pattern precisely. What survives is not the mound itself but the local knowledge that it once existed, a spread of shattered stone and darkened soil that has since been ploughed or otherwise disturbed back into the land. Adding a further layer of interest, a standing stone sits in the same field roughly a hundred metres to the north-east, and another possible burnt mound lies approximately eighty metres to the north, suggesting this small patch of Cork countryside was, at some point in prehistory, a place of some repeated activity.