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 of Ordovician-age volcanic and sedimentary rocks, formed through ancient volcanic activity and subsequent erosion by marine processes. It is notable for its exposure of early Paleozoic geological formations along the northwest coast of England.

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