Why this matters
Stag Rocks is a sea cliff or coastal rock feature composed primarily of Old Red Sandstone, formed during the Devonian period around 400 to 360 million years ago through sedimentary deposition. It is notable for its exposure of ancient terrestrial and shallow marine sediments, typical of the geological formations found in northern Scotland.
What is recorded here
Stag Rocks is shown as a cliff on the public map of Moray. 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.