Why this matters
The Whites is a sea cliff composed primarily of chalk, formed during the Cretaceous period around 80 to 100 million years ago. It is notable as part of the extensive South Downs chalk formation, which is significant for its role in the geological and landscape character of southern England.
What is recorded here
The Whites is shown as a cliff on the public map of Mole Valley. 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.