Yet the black soil visible through the grass is a reliable signal of something far older beneath: a fulacht fia, the term used for a class of prehistoric cooking site found in great numbers across Ireland. The name refers broadly to a burnt mound, typically consisting of fire-cracked stones discarded after repeated use in heating water, usually in a timber- or stone-lined trough. They are most commonly associated with the Bronze Age, though the tradition of use may span several periods.

This particular example, in pasture roughly 160 metres west of the townland boundary with Spittle, had a curious route into the documentary record. It does not appear on the Ordnance Survey six-inch map of 1840, nor on the more detailed twenty-five-inch survey of 1897, suggesting it was either overlooked or not considered significant enough to mark at the time. It surfaces later on the Cassini edition of the OS six-inch map, annotated with the Irish form "Folaí Fiadh" and a note recording that stone and bronze implements were found at the site around 1894. That find, modest as it sounds in a single annotation, is the closest thing the site has to a documented history. The Archaeological Survey of Ireland recorded a grass-covered mound standing 1.5 metres high with black soil showing at the surface, which is characteristic of the charcoal-rich, organically dense deposits left behind by repeated burning and water-heating activity over many seasons or generations.

By the time aerial and satellite imagery was consulted, between roughly 2011 and 2013, no surface remains were clearly visible on either Digital Globe or Google Earth orthoimages, which suggests the mound may have been reduced or disturbed in the intervening years. The site sits in working farmland, and access would depend on landowner permission. Anyone hoping to locate it should note that there is little to see at ground level now; the significance lies in what the annotations and soil record point to rather than in any visible monument. The black soil, if still exposed at the surface, remains the most telling indicator of what lies below.