What is recorded here

The Wall Right of the Paddy Cave is shown as a cliff on the public map of Westmorland and Furness. The saved point is the map point or the centre of its mapped shape.

The Wall Right of the Paddy Cave is a sea cliff composed of Carboniferous limestone, formed around 340–320 million years ago through the accumulation of marine sediments. It is notable for its association with the nearby Paddy Cave, a coastal karst feature indicative of the region's extensive limestone geology.

This does not grant access. Check current paths, opening conditions and ownership before entering.