Brickearth

Description

Brickearth is a superficial deposit of homogeneous loam or silt deposited during the Pleistocene geological period. Brickearth typically occurs in discontinuous spreads, across southern England and South Wales, south of a line from Pembroke in the west to Essex in the east in depths of up to a metre. Commercially useful deposits of about 2m to 4m thick are present in Kent, Hertfordshire and Hampshire, overlying chalk, Thanet Beds or London Clay. The original deposition of the sediments occurred under cold climates where fluvial out-wash sediments from glaciers were subject to windy dry periods. The exposed finer-grained sediments were picked up and transported by the wind and were deposited wherever the wind strength decreased.

There are extensive brickearth deposits in Kent, particularly on the North Downs dip slope and on the Hoo peninsula, sections of the Medway and Stour valleys. Its mineral content is critical to its applicability in brickmaking and requires precise proportions of chalk, clay, and iron.

Brickearth requires little or no admixture of other materials to render it suitable for the manufacture of 'stock bricks'. When used for brick making, it was often dug from small temporary holes and baked into bricks on the spot in brick clamps, and used for building nearby. The hole often remained and became a pond. In 1986, four active stock brick works were in Kent: at Otterham Quay, Funton, Murston and Ospringe.

The brickearth gives rise to rich and fertile soils which have been exploited for agriculture. It is prone to rapid 'collapse' settlement when saturated with water and does not provide a firm foundation for buildings.

In Chichester, the brickearth is a flint-rich brown silty clay up to five metres thick, which occurs on the coastal plain. The brickearth is unfossiliferous but occasionally yields man-made flint implements.

References

• The engineering properties and behaviour of the brickearth of south Essex K. J. Northmore, F. G. Bell and M. G. Culshaw, doi: 10.1144/GSL.QJEGH.1996.029.P2.04 May 1996 Quarterly Journal of Engineering Geology and Hydrogeology, 29, 147-161.

References

1. BGS solid and drift edition 1:50,000 Maps
2. Gibbard, P. L., 1985 Pleistocene History of the Middle Thames Valley
3. [https://shareweb.kent.gov.uk/Documents/Environment-and-planning/planning-and-land-use/kent-minerals-subject-plan-brickearth-extraction/kent-minerals-subject-plan-brickearth-1986.pdf Kent Minerals Subject Plan, BrickEarth Written Statement], May 1986, Kent County Council Planning Department. Accessed April 2012
4. [http://www.geo-east.org.uk/pp/essex/cgreport_pdf/GCA%201%20-%20Tendring%20Plateau.pdf Geodiversity Character Area Descriptions GCA 1 Tendring Plateau] {{Webarchive. link. (2016-03-04 Geo-East Partnership Accessed April 2012)
5. [http://www.bgs.ac.uk/science/landUseAndDevelopment/engineering_geology/formation_engineering.html Loessic Brickearth Map] at Physical Properties and Behaviour of UK Rocks and Soils. British Geological Survey, National Environmental Research Council. Accessed April 2012
6. [http://qra.org.uk/uploads/downloads/files/22/original/Tendring_Essex_Geodiversity_poster.pdf Tendring Essex Geodiversity poster] {{webarchive. link. (May 7, 2013 Peter Allen, Gerald Lucy, Teresa O’Connor, David Bridgland, William George, Adrian Gascoyne, Adrian Knowles, Tom White. Quaternary Research Association, Geo Essex . Accessed April 2012)
7. link. (October 16, 2007 Chichester Museum website. Accessed April 2012)