The ground around it is swampy enough to make access effectively impossible, so the mound sits in its wet field, unclassified and uninvestigated, its purpose and origins genuinely unknown.

What little is recorded comes from two sources separated by four decades. A 1936 Ordnance Survey six-inch map marks it with hachures, the small radiating lines cartographers used to indicate raised or mounded ground, and notes an arc of bank running immediately to the north-west of the main feature. Then, in May 1977, an aerial photograph captured what surveyors describe as differential growth patterns, meaning the vegetation above the mound was behaving differently from the surrounding marsh, suggesting something beneath the surface was influencing drainage or soil composition. The mound lies approximately forty metres north-east of a bend in a nearby stream. Beyond that, the record offers nothing further. No excavation has been attempted, no artefacts are documented, and no confident assignment to any period or function has been made. It could be a natural glacial feature, a burial mound, the remnant of a ringfort, or something else entirely.