In geological terms, the Clyne River is a ‘misfit stream’. It gently meanders through the steep sided valley, and although the Clyne is classed as a main river, and it’s very pretty, it’s hardly the roaring torrent associated with deep rock erosion. Really, the river is an opportunist – it runs along a course carved out by the torrents of melt water containing ice and debris from the retreating glaciers as they drained at the end of the ice-age.
The Clyne River rises around Fairwood Common and continues down the Valley to the sea at Blackpill. The former LMS railway line, which is now a cycle way and footpath, broadly followed the same route, and these two features form the spine of the Valley.
Useful Links
All information and images are copyright of CVCP, unless otherwise stated.