The section of coast, east of Ringstead Bay, between Bran Point and Osmington Mills, expose a superb succession of Corallian (Middle Jurassic) rocks, which reveal the entire sequence of the Osmington Oolite Formation and other beds, which are rich in fossils. A good variety of fossils are found in broken rocks from rockfalls and along the foreshore, which may be collected. Ammonites, bivalves and gastropods and trace fossils are common finds.Jurassic, Cliffs and Foreshore, Rating: ♦♦♦
Bowleaze Cove exposes both the famous Oxford Clay Formation and the overlying Corallian Group, making it one of the most geologically interesting locations around Weymouth. While the historic Oxford Clay exposures that once produced abundant marine reptile remains are now much reduced, the foreshore east of the main beach continues to yield a wide variety of fossils, including ammonites, belemnites, bivalves and trace fossils. The best collecting is generally found beyond the sandy beach beneath Ham Cliff, where fallen Corallian blocks and material washed from the cliffs can provide rewarding finds. The terrain is rough and uneven, consisting of boulders, shingle and fallen rock, so sturdy footwear is essential.Jurassic, Cliffs and Foreshore, Rating: ♦♦♦
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