Why this matters
Craigencat Craigs is a sea cliff composed of Silurian greywacke and mudstone, formed around 440–420 million years ago during sedimentary deposition in a deep marine environment. The site is notable for its exposure of ancient volcanic and sedimentary rock layers, which are part of the Dalradian Supergroup and provide insight into Scotland’s early geological history.
What is recorded here
Craigencat Craigs is shown as a cliff on the public map of Fife. 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.