Chines

A chine ( /ˈtʃaɪn/) is a steep-sided coastal river valley where the river flows to the sea through, typically, soft eroding cliffs of sandstone or clays. The word is still in use in central Southern England—notably in East Devon, Dorset, Hampshire and the Isle of Wight—to describe such topographical features. However, 'bunny' is also used to describe a chine in Hampshire.

Chines appear at the outlet of small river valleys when a particular combination of geology, stream volume and coastal recession rate creates a knickpoint, usually starting at a waterfall at the cliff edge, that initiates rapid erosion and deepening of the stream bed into a gully leading down to the sea.

All chines are in a state of constant change due to erosion. The Blackgang Chine on the Isle of Wight, for example, has been destroyed by landslides and coastal erosion during the 20th century. As the walls of the chines and cliffs are so unstable and erode continually, particularly those of the south coast of the Isle of Wight, the strata are clearly visible. Chines are, therefore, very important for their fossil records, their archaeology and the unique flora and fauna, such as invertebrates and rare insects, for which they provide shelter.

In Devon, Sherbrooke Chine is west of Budleigh Salterton, and Seaton Chine is at the western end of the West Walk esplanade, Seaton. In Dorset, west of Bournemouth are found Flaghead Chine, Branksome Chine, Alum Chine, Middle Chine and Durley Chine, and east towards Boscombe, Boscombe Chine and Honeycombe Chine. Bournemouth town centre itself is built in the former Bourne Chine, although urban development since the late 19th century has altered the topography. Becton Bunny and Chewton Bunny are other examples of chines near Barton on Sea, Hampshire ("Bunny" being the New Forest equivalent to "Chine").

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