What is recorded here

Ewe Crag 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.

Ewe Crag is a sea cliff composed primarily of Ordovician greywacke and slate, formed around 470 to 450 million years ago through deep-marine sedimentation and subsequent regional metamorphism. It is notable for its resistant rock formations that have withstood coastal erosion, contributing to the rugged character of the Cumbrian coastline.

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