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Geology in South Downs


Geology in South Downs

An iconic image, The Seven Sisters
An iconic image, The Seven Sisters
The south Downs are the remnants of the former Wealden Anticline, which stretched across Sussex, The chalk was laided down between 100 and 65 million years ago, on top of the weaker Greensand and Sandstone which makes up much of the Weald, the beds were then folded from 30 to 1 million years ago, the top of the chalk was then eroded, leaving two nearly parallel ridges, which is why 'The Downs' form a long ridge. They are mirrored in the north by the North Downs.

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South Downs Travel Guide from Wikitravel. Many thanks to all Wikitravel contributors. Text is available under Creative Commons Attribution-ShareAlike 3.0, images are available under various licenses, see each image for details.

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