Campden Tunnel Gravel Pit | |
Aos: | Gloucestershire |
Interest: | Geological |
Coordinates: | 52.0658°N -1.7658°W |
Area: | 0.2 hectare |
Notifydate: | 1988 |
Enref: | 1004120 |
Campden Tunnel Gravel Pit is a 0.2ha geological Site of Special Scientific Interest in Gloucestershire, notified in 1988.[1] [2] The site is listed in the 'Cotswold District' Local Plan 2001-2011 (on line).[3] [4]
The site exposes a mixture of gravels, sands and silts which make up the Campden Tunnel Drift (Pleistocene period). These are glacial sediments which fill a deep channel. The melt water is considered to have run from the ice-filled valley of the River Avon (north) to the drainage system of the River Evenlode (south east).[1]
This links with the sequence of glacial deposits in the Midlands and the Upper Thames terraces (Evenlode Valley). The site also links with others in the Moreton-in-Marsh area, for example Stretton-on-Fosse.[1]
The site is considered precious so it must only be used for research purposes.[5]