The Stockbridge Anticline is one of a series of parallel east-west trending folds in the Cretaceous chalk of Hampshire. It lies at the western end of the South Downs, immediately to the north of the Winchester-King's Somborne Syncline and east of Salisbury Plain.

Structure

The anticline axis runs for around 35 kilometres (22 mi) from around the Wallops, swinging south-south-east through Stockbridge and Crawley, between Micheldever and Kings Worthy, towards Medstead in the east.[1][2]

Hills include Danebury and Chattis Hill to the west, Stockbridge Down, Woolbury, Chilbolton Down, Windmill Hill (Crawley) and Abbotstone Down.

Parallel folds to the south include the Winchester-East Meon Anticline and the Winchester-King's Somborne Syncline. To the north is the Micheldever Syncline. As with other nearby folds, the structure is controlled by movement of fault blocks within the Jurassic strata below.[3]

See also

List of geological folds in Great Britain

References

  1. ↑ Winchester (Map). 1:50000. British Geological Survey England and Wales. British Geological Survey. 2002. ISBN 0-7518-3340-1.
  2. ↑ Alresford (Map). 1:50000. British Geological Survey England and Wales. British Geological Survey. 1999. ISBN 0-7518-3250-2.
  3. ↑ Booth, K.A. (2002). Geology of the Winchester district - a brief explanation of the geological map. British Geological Survey. ISBN 0-85272-429-2.


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