Oxford Clay

Oxford Clay is a Jurassic marine sedimentary rock underlying much of South East England, from as far west as Dorset and as far north as Yorkshire. The Oxford Clay is argillaceous (consists of clay) and is of Callovian to lower Oxfordian age.

Oxford Clay appears at the surface around Oxford, Peterborough and Weymouth and is exposed in many quarries around these areas. The top of the Lower Oxford Clay shows a lithological change, where fissile shale changes to grey mudstone. The Middle and Upper Oxford Clays differ slightly, as they are separated by an argillaceous limestone in the South Midlands.

The Callovo-Oxfordian Clay also occurs in the Paris basin (France) and it is a potential host formation to dispose high-level radioactive waste in France.

Palaeontology

The Oxford Clay is well know for its rich fossil record of fish and invertebrates. [Cite book
last = Martill
first = D.M.
coauthors = Hudson J.D.
date = 1991
year = 1991
title = Fossils of the Oxford Clay
publisher = Palaeontological Association] Many of the fossils are well preserved, occasionally some are found exceptionally well preserved. Animals which lived in the Oxford Clay Sea include ichthyosaurs, cephalopods (such as belemnites), bivalves (such as "Gryphaea"), and a variety of gastropods.

Uses

Oxford Clay has a porous consistency and is soft and is often used in the making of roads. It is also the source of the Fletton stock brick of which much of London is built. For brick making, the Oxford Clay has the advantage of containing carbon which provides part of the fuel required in firing it so reducing the requirement for an external fuel source.

ee also

* Clay
* London Clay
* Weald Clay
* Cheltenham Clay
* List of fossil sites "(with link directory)"
* List of dinosaur-bearing rock formations

References