The earthen bank and filled-in fosse, a fosse being a defensive ditch cut to reinforce a rampart, that once separated this headland from the mainland have been so thoroughly flattened by time and agriculture that the enclosing elements are only eight metres wide and a matter of ten centimetres high. Most ancient earthworks assert themselves. This one hardly admits to existing.

A survey carried out in 2003 by Casey recorded the site carefully, noting the headland's southwest-facing aspect toward Doulus Bay, the signs of earlier cultivation within the interior, and a dried stream that once ran through the centre of the enclosed area. Just outside the site, close to the southern cliff edge, there is a low earthen platform of uncertain purpose that may or may not be connected to whatever the original builders intended here. The flanking cliffs are described as low, and the sea is accessible from within the enclosure, a practical detail that distinguishes promontory forts from purely defensive structures; they were frequently associated with fishing, trade, or seasonal occupation as much as with military use. On a nearby subsidiary headland, two further earthen banks appear to cut across the ground, though these turn out to be Land Commission boundaries, the remnants of administrative divisions drawn along the coast in a much later era, rather than prehistoric features.

The site is genuinely difficult to read at ground level. Old field boundaries visible in the surrounding land add to the layered quality of the landscape, where prehistoric, agricultural, and administrative traces have settled into one another over centuries. The levelled bank is best understood not as a monument to look at but as a faint pressure beneath the grass, an almost erased argument that people once thought this particular headland worth the effort of enclosing.