A togher, as these bog roads are known, was essentially a causeway of timber laid across wet or unstable peatland to allow passage where none would otherwise be safe. This particular example came to light not through deliberate excavation but through the slow industrial scalping of the bog itself, which left a scatter of birch, hazel, and willow brushwood exposed on the field surface, oriented east to west and traceable across the full width of the field.

The site was recorded during a 2013 peatland reassessment and later excavated the following year. When archaeologists cleared away loose milled peat by hand, they found roundwood and brushwood timbers ranging from just a few centimetres to over a metre in length, all confined to an area of roughly 3.2 by 1.8 metres. The structural logic of the original road had been lost; what remained gave no clear sense of how it had been laid or how substantial it once was, suggesting these fragments may be the base layer of something more elaborate now largely destroyed. A fragment of willow was selected for AMS radiocarbon dating, a technique that measures the decay of carbon isotopes to establish age, and the result placed the timber's felling or use somewhere between approximately 1294 and 1403, squarely in the later medieval period. By that time the bog would already have been a familiar obstacle to local movement, and toghers of this kind were a practical and well-established solution across the Irish midlands.

The timbers themselves were machine damaged, dried out, and in poor condition by the time they were examined, casualties of the same industrial peat extraction that had exposed them. The surrounding peat was a moderately humified Sphagnum mix with heather, cottongrass, and sedge, the kind of deposit that preserves organic material over centuries but surrenders it quickly once the surface is broken. What survives is less a road than a trace of one, a compressed record of a journey someone made across this bog more than six hundred years ago.