
Why this matters
Backways Cove in Cornwall consists of sedimentary rocks, primarily Devonian-age slates and shales, formed from accumulated marine sediments under pressure over 380 million years ago. The cove is notable for its well-preserved coastal erosion features and the exposure of folded rock layers, which provide insights into the tectonic history of the region.
What is recorded here
Backways Cove is shown as a bay on the public map of Cornwall. 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.