Flixton Quarry is a 0.7 hectare geological Site of Special Scientific Interest south-west of Bungay in Suffolk. It is a Geological Conservation Review site.
This site has sands and gravels which are thought to be a glacial outwash dating to the most extreme ice age of the Pleistocene epoch, the Anglian glaciation around 450,000 years ago. It is described by Natural England as important because of its relationship with deposits of the succeeding Hoxnian Stage.
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