Cave with overhanging chalk strata near Birling Gap, East Sussex

Cave with overhanging chalk strata near Birling Gap, East Sussex is shown and named in a reusable Geograph picture. The saved point is the picture's recorded map point.

The cave is formed in Cretaceous chalk, typical of the South Downs, and likely developed through coastal erosion and solution processes. No significant archaeological or folklore history is recorded for this specific site.