At the back of the car park are old cliffs dating from the 18th century. They are rather degraded but still quite recognisable as cliffs. They are not yet undergoing erosion again, except to the east, as mentioned above. That eastern part is going to provide good geological exposures sooner or later, and it may be helpful in interpreting the Pleistocene Interglacial deposits, discussed elsewhere in this webpage.

Shoot, who would have thhgout that it was that easy?