The Beacon Limestone Formation, historically known as the Junction Bed, is a formation of the early Jurassic age (Pliensbachian–Toarcian).
It lies above the Dyrham Formation and below the Bridport Sand Formation.
It forms part of the Lias Group.
It is found within the Wessex Basin and parts of Somerset,[1] in England.
It is well known for the Strawberry Bank Lagerstätte, which contains the 3-dimensionally preserved remains of vertebrates, including marine crocodyliformes, ichthyosaurs and fish, as well as insect compression fossils.