The well measures water levels in the Chalk aquifer. The well lies to the south of a north-west–south-east trending fault.
Our enquiries service can help you to access groundwater level data for this well.
Our groundwater level records for Ashton Farm start in 1974.
|Datum||72.16 m AOD|
|Monitored by||EA South West|
It is dug into the Lewes Nodular Chalk Formation. The site lies on the south side of the west-north-west–east-south-east trending Winterbourne Abbas Fault with a downthrow to the north-north-east of 20 m.
It is a brick lined well, 1.4 metres in diameter. It was originally sunk for a farm water supply.
The hydrograph has an annual sinusoidal appearance, with some response to intense winter rainfall events. Its response is rapid for a chalk well, presumably because of its shallow depth. It appears to have an unconstrained response, although levels tend to peak close to 71 m AOD, and have only been lower than 64 metres on rare occasions.
Contact Andrew McKenzie for further information