Beacon Limestone Formation
http://dbpedia.org/resource/Beacon_Limestone_Formation an entity of type: SpatialThing
The Beacon Limestone Formation, historically known as the Junction Bed, is a formation of 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, 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.
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Beacon Limestone Formation
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Beacon Limestone Formation
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Marlstone Rock, Barrington & Eype Mouth Limestone Members
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~
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Upper Pliensbachian–Toarcian Spinatum-lowermost Thouarsense
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Cliff exposure at Thorncombe Beacon
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Toarcian
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Up to
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Averaging <
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50.9 -2.8
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The Beacon Limestone Formation, historically known as the Junction Bed, is a formation of 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, 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.
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Cliff exposure beneath Thorncombe Beacon
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