Why this matters
Hare Crags is a sea cliff composed primarily of Carboniferous sandstone, formed around 300 to 340 million years ago through sedimentary deposition in ancient river and delta systems. The cliff is notable for its resistant rock layers and coastal erosion features, typical of the Northumberland coastline.
What is recorded here
Hare Crags is shown as a cliff on the public map of Northumberland. 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.