What makes this particular example quietly interesting is how much it conceals behind an apparently featureless surface. The grassy interior offers almost nothing to the casual eye, yet beneath that ordinariness lies a layered history of human effort and coastal erosion working in slow opposition.

When the site was recorded in 2002 by Casey, the promontory was described as subcircular, facing north-west, and cut off from the land behind it by a combination of a modern earthen bank and the much older remains of a fosse and inner bank. A fosse is simply a defensive ditch, and here the original one survives only as a low scarp no more than a metre high. The inner edge of the bank is barely visible, rising just twenty centimetres at its most pronounced, and no stone revetment, the facing material that would once have reinforced and retained the earthwork, remains detectable. Access to the enclosure was through a causewayed entrance from the south, meaning a raised pathway crossed the fosse rather than a gap being cut through it. Inside, the ground shows faint undulations and traces of a perimeter bank along the shoreline, but little else. Perhaps the most telling detail is geological rather than archaeological: sea rocks extending northwards from the headland become exposed at low tide, suggesting the promontory itself was once considerably larger. The coastline has retreated, taking whatever originally stood near the edge with it.

The surrounding land is open pasture, gently rolling and fertile, which means the site sits without drama in an agricultural landscape rather than looming above dramatic cliffs. The sea is reachable from within the enclosure, though with difficulty, a detail that hints at the practical relationship between the fort's occupants and the water, whether for fishing, communication, or simply as a last means of escape.