Why this matters
Hooken Cliffs are composed primarily of Devonian-age sedimentary rocks, including sandstone and shale, formed around 380 million years ago through the deposition of river and delta sediments. The cliffs are notable for their exposure of ancient terrestrial and coastal environments, offering insights into Devonian geological history in the region.
What is recorded here
Hooken Cliffs is shown as a cliff on the public map of East Devon. 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.