They include ones on the Isle of Wight; on the Dorset-Devon border near Lyme Regis; on cliffs near Branscombe in East Devon; and at White Nothe, Dorset.
All arose from slump of harder strata over softer clay, giving rise to irregular landscapes of peaks, gullies and slipped blocks, that have become densely vegetated due to their isolation and change of land use.
The microclimate of warm sunshine, moist air and few winter chills was recognised by leading physicians in Victorian times as a beneficial environment for sufferers of respiratory diseases.
[2][3][4][5][6] The west Dorset coast around Charmouth and Lyme Regis includes unstable cliffs which have given rise to undercliff areas with varied topography.
[12] A large tract of land below Bindon Manor and Dowlands Farm slipped, creating the features now called Goat Island and the Chasm.
[13][14] The Undercliff was formerly open rough pasture, grazed by sheep and rabbits, including features such as Donkey Green (an area of turf used for picnics and sports), Landslip Cottage (which used to sell teas to visitors),[15] and Chapel Rock (where, according to tradition, Tudor religious dissenters met).
[16] Folkestone Warren, since stabilised by sea defences to protect the Dover-Folkestone railway that runs at its foot, is designated a Site of Special Scientific Interest and a nature reserve.
Coastal soft cliffs and slopes support a specialised assemblage of species reliant on a historical continuity of bare ground, pioneer vegetation habitats, and freshwater seepages.