Why this matters
Gosforth Crag is a sea cliff composed primarily of Carboniferous limestone, formed around 340 to 320 million years ago through the accumulation of marine sediments. It is notable for its exposure of ancient rock layers and its role in illustrating the geological history of the Cumberland coast.
What is recorded here
Gosforth Crag is shown as a cliff on the public map of Cumberland. The saved point is the map point or the centre of its mapped shape.
The public map does not by itself grant access. Check current paths, opening conditions and ownership before entering.