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Corallian Limestone is a coralliferous sedimentary rock, laid down in Jurassic times. It is also called Coral Rag and is very hard. Building stones from this geological structure tend to be irregular in shape. It is often found close to seams of Portland Limestone (e.g. Abbotsbury in Dorset, England). It is a younger limestone than its near-neighbour, the Oolitic, as found in the Cotswolds, in Gloucestershire.
Additional recommended knowledge
A ridge of Corallian Limestone rises above the Vale of Avon and the Thames Valley in its Oxfordshire stretch. The Oxfordshire Corallian ridge is an escarpment holding back the hanging valley that is the Vale of White Horse and its hardness forced the River Thames to take a wide Northern detour, to cut through the low ridge at Oxford. High points along the ridge are Cumnor Hill and Wytham Hill.
Hilly outcrops above this corallian ridge, composed of Lower Greensand, occur at Badbury Hill, Faringdon (Folly Hill) and Boars Hill.
Softer sandy deposits occur within the Corallian, found for example at Faringdon, Shellingford and Hatford in Oxfordshire, where the sands and gravels are extensively quarried.
In England, Corallian Limestone is to be found in Dorset, Wiltshire, Oxfordshire, Buckinghamshire, Cambridgeshire, Lincolnshire and Yorkshire.
|This article is licensed under the GNU Free Documentation License. It uses material from the Wikipedia article "Corallian_Limestone". A list of authors is available in Wikipedia.|