Between Osmington Mills and Ringstead Bay is this distinct ledge at the base of the cliff at Bran Point .
Crowded with the trace fossil - 'Arenicolites Variabilis' , also traces of the ‘U-shaped’ burrows of the invertebrate - 'Diplocraterion Parallelum'.
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Osmington Mills and Ringstead Bay are to the East of Weymouth
Ref: 8780
Date: 30/04/2021
Location: SY 7423 8134