West Woodyates Manor

Although once called the 'Roman Well' there is no real evidence that it is that old, but it has been used to measure groundwater levels in the Chalk since 1942.

Our enquiries service can help you to access groundwater level data for this well.

Hydrograph


hydrograph

Show data from :-
1942 to 2013 1970s 1980s 1990s 2000s 2010s


Information about the well

West Woodyates Manor
Wellmaster ID SU01/5B
NGR 4016 1194
Datum 110.88 m AOD
Monitoring details
Type Groundwater Level
Aquifer Chalk
Confinement Unconfined
Depth 45.1 m
Record
Monitored by EA South West
Records commence 1942
Records end active

Map of West Woodyates Manor showing geology and water level contours.

Hydrogeological setting

This well measures water levels in the Wessex Chalk aquifer between Blandford Forum and Salisbury. It is dug into Seaford Chalk. It is close to the head of a Bourne stream.

Well or borehole construction

The well consists of a 45.1 metre deep oval shaft, with a diameter of 3 metres by 1.37 metres. It is recorded in some records as the 'Roman' well - but there is no evidence in the record of whether this is anything other than a name.

Hydrograph response

The well has a relatively rapid and flashy response for a Chalk well, with typical annual fluctuations of 25 metres, and evidence of rapid recharge at high levels.

A file note suggests that the well responds to changes in wind direction - possibly barometric effects or the venturi effect.

At the highest levels groundwater flooding has been recorded in the cellars of the adjacent Manor House.

Data issues

Levels were noted in 1930, 1936, 1937 and 1938 prior to the commencement of regular monitoring in 1942.

Contact

Contact Andrew McKenzie for further information