Essex Field Club on Facebook

Visit Our Centre

EFC Centre at Wat Tyler Country ParkOur centre is available for visits on a pre-booked basis on Wednesdays between 10am - 4pm. The Club’s activities and displays are also usually open to the public on the first Saturday of the month 11am - 4pm.

Video about the Club Essex Field Club video

About the Essex Field Club
Essex Field Club
registered charity
no 1113963
HLF Logo A-Z Page Index

Geology Site Account

A-Z Geological Site Index

Oozes Wood Puddingstone, FARNHAM, Uttlesford District, TL48642565, General geological site

show OS map  show polygon    

Site category: Boulders - puddingstone

Site name: Oozes Wood Puddingstone

Grid reference: TL 4864 2565

Brief description of site:

A small boulder of Hertfordshire Puddingstone (70 centimetre diameter) on the north side of a bridleway on the edge of the wood.

----------------------------------------

Hertfordshire puddingstone

Hertfordshire Puddingstone was formed around 55 million years ago when the climate of Britain was hot and a layer of pebbles beneath the surface of the ground became cemented with quartz. They are thus very resistant to erosion and have survived the rigours of the Ice Age. They originated in Hertfordshire, hence the name, and were probably carried to Essex by the River Thames when it flowed north of its present course. However, the distribution and abundance of Hertfordshire puddingstone in parts of Essex suggests that some occurrences may have a local Essex source.

The formation of silcretes (which includes sarsens and puddingstones) has been the subject of recent scientific debate. Research has compared the conditions under which sarsens and puddingstones may have been formed with the present day climate in the Kalahari Desert and parts of Australia.



The Oozes Wood Puddingstone in 2009 (Photo: Simon Taylor)

 

if you have an image please upload it


Reference: Simon Taylor (personal communication)

Geology Site Map
A-Z Geological Site Index