Seal Howe stands on a limestone plateau overlooking the Lyvennet Valley, where traces of prehistoric activity remain scattered across the surrounding fell. Nearby are the remains of ancient field systems, settlements and ceremonial monuments, suggesting that this exposed upland landscape supported communities for thousands of years. Together with the neighbouring stone circles and standing stones, the cairn forms part of one of Cumbria’s most remarkable Bronze Age landscapes.

Seal Howe is formed from a circular mound of loose limestone stones, standing prominently on the plateau above Oddendale. The curving line of stones leading towards the cairn adds to the sense of antiquity. Excavations revealed the uncremated remains of an adult male within the cairn, while a secondary burial to the south contained an urn holding the cremated remains of a woman and child.

From Seal Howe, a gap between the shelter belts creates a natural window towards the Shap and Hardendale fells. The elevated position of the Potrigg plateau provides extensive views across the surrounding countryside and helps explain why this landscape became home to such a concentration of prehistoric monuments, including cairns, stone circles and standing stones.