Cliffs and scree below Roundton Hill

A named place photographed at this map point in Powys.

Roughly 250–300 metres in elevation, the cliffs and scree below Roundton Hill are composed of Carboniferous limestone, typical of the surrounding Welsh uplands. The area is part of the broader geological and landscape character of the Clwydian Range and Dee Valley, contributing to regional biodiversity and upland habitat continuity.