Jurassic Coast

Chesil Beach - Finest barrier beach in Europe

2chesil_beach_from_abbotsburLocation: Chesil Bank (West Bay - Portland) Best viewed from Abbotsbury Hill.

Rock Type: Large shingle bank made largely of chert pebbles.

Age: approximately 20,000 years

Look out for: Chesil bank supports its own unique plant and animal communities. Some areas are protected and under restricted access to protect nesting birds.

The geology in Detail

Chesil Bank was formed from the debris of ancient landslides along what would become the West Dorset coast. Before 125,000 years ago sea levels were at a similar level to those of today and the cliff line of West Dorset would have been in almost the same position as it is now. During that time the familiar processes of landslides and mudflows that characterise that part of the Jurassic Coast would have been operating, carrying thousands of tonnes of debris on to the beach to be slowly removed by the sea. However, at about 125,000 years ago sea levels dropped due to the formation of ice sheets and the actively eroding coastline was abandoned. The landslides continued to occur along the cliffs but without the sea to remove the fallen material it built up into massive debris fans. Eventually the slopes formed a stable angle, stopped moving and became vegetated. After 100,000 years sea levels rose again to their previous height and encountered these huge accumulations of mud and rock. As these debris fans were eroded the material was carried east by long shore drift and formed an enormous shingle bank. Today the landslides around Lyme Regis that haven't moved for thousands of years have been exposed again and are slowly re-activating.
Geo highlights

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