Ladder stile on Cockington Cliff

A named place photographed at this map point in Torridge.

Ladder stile on Cockington Cliff is a coastal rock feature formed from Devonian-age sedimentary rocks, primarily mudstones and sandstones, deposited around 380 million years ago in a shallow marine environment. The feature is notable as part of the broader geological exposure along the North Devon coast, which provides important insights into the region's ancient geological history.